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description Publicationkeyboard_double_arrow_right Article , Research , Conference object , Preprint 2021 Sweden, Belgium, Italy, Germany, Denmark, Belgium, United KingdomPublisher:IOP Publishing Funded by:UKRI | RootDetect: Remote Detect..., UKRI | Improved Loss Modelling o...UKRI| RootDetect: Remote Detection and Precision Management of Root Health ,UKRI| Improved Loss Modelling of SMC ComponentsAbbasi, R.; Ackermann, M.; Andeen, K.; Fox, D.; Franckowiak, A.; Friedman, E.; Fritz, A.; Fürst, Philipp; Gaisser, T. K.; Gallagher, J.; Ganster, Erik; Garcia, Alfonso; Garrappa, S.; Anderson, T.; Gerhardt, L.; Ghadimi, A.; Glaser, C.; Glauch, T.; Glüsenkamp, T.; Goldschmidt, A.; Gonzalez, J. G.; Goswami, S.; Grant, D.; Grégoire, T.; Anton, G.; Griswold, S.; Gündüz, M.; Günther, C.; Haack, Christian; Hallgren, A.; Halliday, R.; Halve, Lasse Yannik; Halzen, F.; Minh, M. Ha; Hanson, K.; Argüelles, C.; Hardin, J.; Harnisch, A. A.; Haungs, A.; Hauser, Simon; Hebecker, D.; Helbing, K.; Henningsen, F.; Hettinger, E. C.; Hickford, S.; Hignight, J.; Ashida, Y.; Hill, C.; Hill, G. C.; Hoffman, K. D.; Hoffmann, R.; Hoinka, T.; Hokanson-Fasig, B.; Hoshina, K.; Huang, F.; Huber, M.; Huber, T.; Axani, S.; Hultqvist, K.; Hünnefeld, M.; Hussain, R.; In, S.; Iovine, N.; Ishihara, A.; Jansson, M.; Japaridze, G. S.; Jeong, M.; Jones, B. J. P.; Bai, X.; Kang, D.; Kang, W.; Kang, X.; Kappes, A.; Kappesser, D.; Karg, T.; Karl, M.; Karle, A.; Katz, U.; Kauer, M.; V., A. Balagopal; Kellermann, Moritz; Kelley, J. L.; Kheirandish, A.; Kin, K.; Kintscher, T.; Kiryluk, J.; Klein, S. R.; Koirala, R.; Kolanoski, H.; Kontrimas, T.; Barbano, A.; Köpke, L.; Kopper, C.; Kopper, S.; Koskinen, D. J.; Koundal, P.; Kovacevich, M.; Kowalski, M.; Kozynets, T.; Kun, E.; Kurahashi, N.; Barwick, S. W.; Lad, N.; Gualda, C. Lagunas; Lanfranchi, J. L.; Larson, M. J.; Lauber, F.; Lazar, J. P.; Lee, J. W.; Leonard, K.; Leszczyńska, A.; Li, Y.; Adams, J.; Bastian, B.; Lincetto, M.; Liu, Q. R.; Liubarska, M.; Lohfink, E.; Mariscal, C. J. Lozano; Lu, L.; Lucarelli, F.; Ludwig, A.; Luszczak, W.; Lyu, Y.; Basu, V.; Ma, W. Y.; Madsen, J.; Mahn, K. B. M.; Makino, Y.; Mancina, S.; Maris, I. C.; Maruyama, R.; Mase, K.; McElroy, T.; McNally, F.; Baur, S.; Mead, J. V.; Meagher, K.; Medina, A.; Meier, M.; Meighen-Berger, S.; Micallef, J.; Mockler, D.; Montaruli, T.; Moore, R. W.; Morse, R.; Bay, R.; Moulai, M.; Naab, R.; Nagai, R.; Naumann, U.; Necker, J.; Nguyễn, L. V.; Niederhausen, H.; Nisa, M. U.; Nowicki, S. C.; Nygren, D. R.; Beatty, J. J.; Pollmann, A. Obertacke; Oehler, M.; Olivas, A.; O'Sullivan, E.; Pandya, H.; Pankova, D. V.; Park, N.; Parker, G. K.; Paudel, E. N.; Paul, Larissa; Becker, K.-H.; Heros, C. Pérez de los; Peters, L.; Peterson, J.; Philippen, Saskia; Pieloth, D.; Pieper, S.; Pittermann, M.; Pizzuto, A.; Plum, M.; Popovych, Y.; Tjus, J. Becker; Porcelli, A.; Rodriguez, M. Prado; Price, P. B.; Pries, B.; Przybylski, G. T.; Raab, C.; Raissi, A.; Rameez, M.; Rawlins, K.; Rea, I. C.; Bellenghi, C.; Rehman, A.; Reichherzer, P.; Reimann, René; Renzi, G.; Resconi, E.; Reusch, S.; Rhode, W.; Richman, M.; Riedel, B.; BenZvi, S.; Robertson, S.; Rongen, Martin; Rott, C.; Ryckbosch, D.; Cantu, D. Rysewyk; Safa, I.; Sandrock, A.; Sandroos, J.; Santander, M.; Sarkar, S.; Satalecka, K.; Aguilar, J. A.; Bernardini, E.; Schneider, A.; Schneider, J.; Schröder, F. G.; Schumacher, Lisa Johanna; Schwefer, Georg; Sclafani, S.; Silva, M.; Smithers, B.; Soedingrekso, J.; Soldin, D.; Spiczak, G. M.; Spiering, C.; Stachurska, J.; Stein, R.; Stettner, Jöran Benjamin; Stezelberger, T.; Stuttard, T.; Sullivan, G. W.; Taboada, I.; Tenholt, F.; Ter-Antonyan, S.; Tollefson, K.; Tomankova, L.; Toscano, S.; Blaufuss, E.; Trettin, A.; Tung, C. F.; Turcati, A.; Turley, C. F.; Elorrieta, M. A. Unland; Blot, S.; Vandenbroucke, J.; van Eijndhoven, N.; van Santen, J.; Verpoest, S.; Walck, C.; Watson, T. B.; Weaver, C.; Weldert, J.; Wendt, C.; Whitehorn, N.; Wiebusch, Christopher; Wolf, M.; Yoshida, S.; Yuan, T.; Böser, S.; Ahlers, M.; Botner, O.; Bradascio, F.; Bron, S.; Burgman, A.; Campana, M. A.; Chen, C.; Chirkin, D.; Clark, B. A.; Clark, K.; Coleman, A.; Collin, G. H.; Conrad, J. M.; Coppin, P.; Correa, P.; Cowen, D. F.; Cross, R.; Dave, P.; De Clercq, C.; DeLaunay, J. J.; Dembinski, H.; Desai, A.; Desiati, P.; de Vries, K. D.; de Wasseige, G.; de With, M.; DeYoung, T.; Diaz, A.; Díaz-Vélez, J. C.; Dujmovic, H.; Eller, P.; Evenson, P. A.; Fazely, A. R.; Fienberg, A. T.; Finley, C.;Ultraluminous infrared galaxies (ULIRGs) have infrared luminosities L $_{IR}$ ��� 10$^{12}$ L $_{���}$, making them the most luminous objects in the infrared sky. These dusty objects are generally powered by starbursts with star formation rates that exceed 100 M $_{���}$ yr$^{���1}$, possibly combined with a contribution from an active galactic nucleus. Such environments make ULIRGs plausible sources of astrophysical high-energy neutrinos, which can be observed by the IceCube Neutrino Observatory at the South Pole. We present a stacking search for high-energy neutrinos from a representative sample of 75 ULIRGs with redshift z ��� 0.13 using 7.5 yr of IceCube data. The results are consistent with a background-only observation, yielding upper limits on the neutrino flux from these 75 ULIRGs. For an unbroken E $^{���2.5}$ power-law spectrum, we report an upper limit on the stacked flux at 90% confidence level. In addition, we constrain the contribution of the ULIRG source population to the observed diffuse astrophysical neutrino flux as well as model predictions. The astrophysical journal 926(1), 59 (2022). doi:10.3847/1538-4357/ac3cb6 Published by Univ., Chicago, Ill. [u.a.]
arXiv.org e-Print Ar... arrow_drop_down arXiv.org e-Print ArchiveOther literature type . Preprint . 2021Data sources: arXiv.org e-Print ArchiveVrije Universiteit Brussel Research Portal; Journal of Physics : Conference SeriesArticle . Conference object . 2021 . 2022 . Peer-reviewedLicense: CC BYPublikationsserver der RWTH Aachen UniversityArticle . 2022Data sources: Publikationsserver der RWTH Aachen UniversityGhent University Academic BibliographyArticle . 2022Data sources: Ghent University Academic BibliographyOxford University Research Archive; The Astrophysical JournalArticle . 2022 . Peer-reviewedLicense: CC BYedoc-Server. Open-Access-Publikationsserver der Humboldt-Universität zu BerlinArticle . 2022 . Peer-reviewedCopenhagen University Research Information SystemArticle . 2022Data sources: Copenhagen University Research Information SystemVrije Universiteit Brussel Research PortalArticle . 2022Data sources: Vrije Universiteit Brussel Research PortalVrije Universiteit Brussel Research PortalConference object . 2022Data sources: Vrije Universiteit Brussel Research PortalPublikationsserver der RWTH Aachen UniversityPreprint . 2021Data sources: Publikationsserver der RWTH Aachen UniversityGhent University Academic BibliographyArticle . 2022Data sources: Ghent University Academic Bibliographyedoc-Server. Open-Access-Publikationsserver der Humboldt-Universität zu BerlinArticle . 2022 . Peer-reviewedLicense: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1088/1742-6596/2156/1/012087&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 7 citations 7 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert arXiv.org e-Print Ar... arrow_drop_down arXiv.org e-Print ArchiveOther literature type . Preprint . 2021Data sources: arXiv.org e-Print ArchiveVrije Universiteit Brussel Research Portal; Journal of Physics : Conference SeriesArticle . Conference object . 2021 . 2022 . Peer-reviewedLicense: CC BYPublikationsserver der RWTH Aachen UniversityArticle . 2022Data sources: Publikationsserver der RWTH Aachen UniversityGhent University Academic BibliographyArticle . 2022Data sources: Ghent University Academic BibliographyOxford University Research Archive; The Astrophysical JournalArticle . 2022 . Peer-reviewedLicense: CC BYedoc-Server. Open-Access-Publikationsserver der Humboldt-Universität zu BerlinArticle . 2022 . Peer-reviewedCopenhagen University Research Information SystemArticle . 2022Data sources: Copenhagen University Research Information SystemVrije Universiteit Brussel Research PortalArticle . 2022Data sources: Vrije Universiteit Brussel Research PortalVrije Universiteit Brussel Research PortalConference object . 2022Data sources: Vrije Universiteit Brussel Research PortalPublikationsserver der RWTH Aachen UniversityPreprint . 2021Data sources: Publikationsserver der RWTH Aachen UniversityGhent University Academic BibliographyArticle . 2022Data sources: Ghent University Academic Bibliographyedoc-Server. Open-Access-Publikationsserver der Humboldt-Universität zu BerlinArticle . 2022 . Peer-reviewedLicense: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2021 Switzerland, Germany, ItalyPublisher:American Association for the Advancement of Science (AAAS) Funded by:EC | RESOLUTION, EC | SUCCESSEC| RESOLUTION ,EC| SUCCESSAlan Cooper; Chris S. M. Turney; Jonathan G. Palmer; Alan G. Hogg; Matt S. McGlone; Janet M. Wilmshurst; Andrew Lorrey; Timothy J Heaton; James M. Russell; Ken McCracken; Julien Anet; Eugene Rozanov; Marina Friedel; Ivo Suter; Thomas Peter; Raimund Muscheler; Florian Adolphi; Anthony Dosseto; J. Tyler Faith; Pavla Fenwick; Christopher J. Fogwill; Konrad A Hughen; Matthew Lipson; Jiabo Liu; Norbert R. Nowaczyk; Eleanor Rainsley; Christopher Bronk Ramsey; Paolo Sebastianelli; Yassine Souilmi; Janelle Stevenson; Zoë Thomas; Raymond Tobler; Roland Zech;pmc: PMC7612203
handle: 11585/839023
Cooper et al . (Research Articles, 19 February 2021, p. 811) propose that the Laschamps geomagnetic inversion ~42,000 years ago drove global climatic shifts, causing major behavioral changes within prehistoric groups, as well as events of human and megafaunal extinction. Other scientific studies indicate that this proposition is unproven from the current archaeological, paleoanthropological, and genetic records.
Archivio istituziona... arrow_drop_down Europe PubMed CentralArticle . 2021Full-Text: http://europepmc.org/articles/PMC7612203Data sources: PubMed CentralGFZ German Research Centre for GeosciencesArticle . 2021Data sources: GFZ German Research Centre for GeosciencesGFZ German Research Centre for GeosciencesArticle . 2021Data sources: GFZ German Research Centre for GeosciencesScienceOther literature type . Article . 2021 . Peer-reviewedZHAW digitalcollection; ScienceOther literature type . Article . 2022 . 2021 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1126/science.abh3655&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesbronze 4 citations 4 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert Archivio istituziona... arrow_drop_down Europe PubMed CentralArticle . 2021Full-Text: http://europepmc.org/articles/PMC7612203Data sources: PubMed CentralGFZ German Research Centre for GeosciencesArticle . 2021Data sources: GFZ German Research Centre for GeosciencesGFZ German Research Centre for GeosciencesArticle . 2021Data sources: GFZ German Research Centre for GeosciencesScienceOther literature type . Article . 2021 . Peer-reviewedZHAW digitalcollection; ScienceOther literature type . Article . 2022 . 2021 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1126/science.abh3655&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Preprint , Article , Other literature type 2021 DenmarkPublisher:Copernicus GmbH Funded by:SNSF | EGRIP: The Swiss Contribu..., UKRI | Developing and testing a ...SNSF| EGRIP: The Swiss Contribution ,UKRI| Developing and testing a new Energy from Waste gasification feedstockGiulia Sinnl; Mai Winstrup; Tobias Erhardt; Eliza Cook; Camilla Marie Jensen; Anders Svensson; Bo Møllesøe Vinther; Raimund Muscheler; Sune Olander Rasmussen;Abstract. Ice-core timescales are vital for the understanding of past climate; hence they should be updated whenever significant amounts of new data can contribute to improvements. Here, the Greenland ice-core chronology was revised for the last 3835 years by synchronizing six deep ice-cores and three shallow ice-cores from the central Greenland ice sheet. A layer-counting bias was found in all ice cores because of site-specific signal disturbances, and a manual comparison of all ice cores was deemed necessary to increase timescale accuracy. A new method was applied by combining automated counting of annual layers on multiple parallel proxies and manual fine-tuning. After examining sources of error and their correlation lengths, the uncertainty rate was quantified to be one year per century. The new timescale is younger than the previous Greenland chronology by about 13 years at 3800 years ago. The most recent 800 years are largely unaffected by the revision, while the slope of the offset between timescales is steepest between 800 and 1000 years ago. Moreover, offset-oscillations of about 5 years around the average are observed between 2500 and 3800 years ago. The non-linear offset behavior is attributed to previous mismatches of volcanic eruptions, to the much more extensive data set available to this study, and to the finer resolution of the new ice-core matching. In response to volcanic eruptions, averaged water isotopes and layer thicknesses from Greenland ice cores provide evidence of notable cooling lasting for up to a decade, longer than reported in previous studies of volcanic forcing. By analysis of the common variations of cosmogenic radionuclides, the new ice-core timescale is found to be in alignment with the IntCal20 curve. Radiocarbon dated evidence found in the proximity of eruption sites such as Vesuvius or Thera was compared to the ice-core dataset; no conclusive evidence was found regarding if these two eruptions can be matched to acidity spikes in the ice cores. A hitherto unidentified cooling event in the ice cores is observed at about 3600 years ago (1600 BCE), which could have been caused by a large eruption which is, however, not clearly recorded in the acidity signal. The hunt for clear signs of the Thera eruption in Greenland ice-cores thus remains elusive.
https://doi.org/10.5... arrow_drop_down https://doi.org/10.5194/cp-202...Preprint . 2021 . Peer-reviewedLicense: CC BYData sources: CrossrefCopenhagen University Research Information SystemArticle . 2022Data sources: Copenhagen University Research Information SystemOnline Research Database In TechnologyArticle . 2022Data sources: Online Research Database In TechnologyCopernicus Publications; Climate of the Past (CP)Other literature type . 2022Data sources: Copernicus Publicationsadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/cp-2021-155&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesgold 9 citations 9 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert https://doi.org/10.5... arrow_drop_down https://doi.org/10.5194/cp-202...Preprint . 2021 . Peer-reviewedLicense: CC BYData sources: CrossrefCopenhagen University Research Information SystemArticle . 2022Data sources: Copenhagen University Research Information SystemOnline Research Database In TechnologyArticle . 2022Data sources: Online Research Database In TechnologyCopernicus Publications; Climate of the Past (CP)Other literature type . 2022Data sources: Copernicus Publicationsadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/cp-2021-155&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2021 France, Netherlands, FrancePublisher:Elsevier BV Frank, Anja,; Frei, Robert; Moutafi, Ioanna; Voutsaki, Sofia; Orgeolet, Raphaël; Kristiansen, Kristian; Frei, Karin,;Sr isotopes are a powerful tool used to reconstruct human mobility in archaeology. This requires extensive bioavailable 87Sr/86Sr baselines used as reference for deciphering potential areas of origin. We define the first extensive bioavailable Sr isotope baselines for the different geographical regions and surface lithologies of Greece by combining new Sr data with previously published bioavailable 87Sr/86Sr data. We present 82 new Sr concentrations and 87Sr/86Sr signatures of plants, soil leachates, surface waters and spring waters from Central Greece and combine these with published baseline values from all over Greece. We define individual baselines for ten of the thirteen geographical regions of Greece. We also provide soil leachate 87Sr/86Sr ratios from the two archaeological Bronze Age sites of Kirrha and Ayios Vasileios in Central and Southern Greece and demonstrate the validity and applicability of the new baselines for these sites. The bioavailable 87Sr/86Sr compositions of Central Greece define a narrow range of 87Sr/86Sr values between 0.70768 — 0.71021, with the widest range observed for the soil leachates. Sr derived from carbonate weathering appears to be the most important Sr source sampled by the proxies. There is an overall larger variability in baseline ranges of the different geographical regions, the narrowest is that for West Greece and the widest that for West Macedonia. In addition, we computed statistical Sr isotope ranges for the five main surface lithological groups characterising the sampling sites of the various proxies. Narrowly ranged, unradiogenic bioavailable Sr isotope signatures are typical of areas characterised by igneous outcrops as well as by Cenozoic and Mesozoic sediments. Areas, where Palaeozoic and Precambrian bedrock outcrops dominate, produce significantly wider ranges. Our study promotes the usefulness of multi-proxy baselines for geographical reference purposes and thus their promising applicability for future human mobility studies.
NARCIS; The Science ... arrow_drop_down NARCIS; The Science of The Total EnvironmentArticle . 2021The Science of The Total EnvironmentArticle . 2021 . Peer-reviewedLicense: Elsevier TDMData sources: CrossrefHyper Article en Ligne - Sciences de l'Homme et de la Société; Hal-DiderotArticle . 2021License: CC BY NC NDHAL AMU; Mémoires en Sciences de l'Information et de la CommunicationArticle . 2021License: CC BY NC NDadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.scitotenv.2021.148156&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen bronze 13 citations 13 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert NARCIS; The Science ... arrow_drop_down NARCIS; The Science of The Total EnvironmentArticle . 2021The Science of The Total EnvironmentArticle . 2021 . Peer-reviewedLicense: Elsevier TDMData sources: CrossrefHyper Article en Ligne - Sciences de l'Homme et de la Société; Hal-DiderotArticle . 2021License: CC BY NC NDHAL AMU; Mémoires en Sciences de l'Information et de la CommunicationArticle . 2021License: CC BY NC NDadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.scitotenv.2021.148156&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2021Funded by:NSERC, NSF | Collaborative Research: P..., NSF | Collaborative Research: A... +1 projectsNSERC ,NSF| Collaborative Research: Paleoclimate perspective on the response of Southwest North American rainfall to elevated greenhouse gases ,NSF| Collaborative Research: Arctic Temperature Amplification during the Middle Pliocene (ArcAMP): Assessing the interaction among feedback mechanisms ,NSF| The Management and Operation of the National Center for Atmoshperic Research (NCAR)Zhongshi Zhang; Daniel Lunt; Ellen Berntell; Stephen Hunter; Wing-Le Chan; Qiang Li; Charles Williams; Linda Sohl; Christian Stepanek; Xiangyu Li;Abstract. The mid-Pliocene warm period (mPWP; ∼3.2 million years ago) is seen as the most recent time period characterized by a warm climate state, with similar to modern geography and ∼400 ppmv atmospheric CO2 concentration, and is therefore often considered an interesting analogue for near-future climate projections. Paleoenvironmental reconstructions indicate higher surface temperatures, decreasing tropical deserts, and a more humid climate in West Africa characterized by a strengthened West African Monsoon (WAM). Using model results from the second phase of the Pliocene Modelling Intercomparison Project (PlioMIP2) ensemble, we analyse changes of the WAM rainfall during the mPWP by comparing them with the control simulations for the pre-industrial period. The ensemble shows a robust increase in the summer rainfall over West Africa and the Sahara region, with an average increase of 2.5 mm/d, contrasted by a rainfall decrease over the equatorial Atlantic. An anomalous warming of the Sahara and deepening of the Saharan Heat Low, seen in >90 % of the models, leads to a strengthening of the WAM and an increased monsoonal flow into the continent. A similar warming of the Sahara is seen in future projections using both phase 3 and 5 of the Coupled Model Intercomparison Project (CMIP3 and CMIP5). Though previous studies of future projections indicate a west–east drying–wetting contrast over the Sahel, PlioMIP2 simulations indicate a uniform rainfall increase in that region in warm climates characterized by increasing greenhouse gas forcing. We note that this effect will further depend on the long-term response of the vegetation to the CO2 forcing.
Climate of the Past ... arrow_drop_down Climate of the Past (CP); OpenAPC Global InitiativeArticle . Conference object . 2021 . Peer-reviewedLicense: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/cp-17-1777-2021&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 9 citations 9 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert Climate of the Past ... arrow_drop_down Climate of the Past (CP); OpenAPC Global InitiativeArticle . Conference object . 2021 . Peer-reviewedLicense: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/cp-17-1777-2021&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Preprint , Other literature type , Review 2021 Sweden, Norway, Germany, Lithuania, Austria, FinlandPublisher:Copernicus GmbH Funded by:EC | BONUS+EC| BONUS+H. E. M. Meier; H. E. M. Meier; M. Kniebusch; C. Dieterich; M. Gröger; E. Zorita; R. Elmgren; K. Myrberg; K. Myrberg; M. P. Ahola; A. Bartosova; E. Bonsdorff; F. Börgel; R. Capell; I. Carlén; T. Carlund; J. Carstensen; O. B. Christensen; V. Dierschke; C. Frauen; C. Frauen; M. Frederiksen; E. Gaget; E. Gaget; A. Galatius; J. J. Haapala; A. Halkka; G. Hugelius; G. Hugelius; B. Hünicke; J. Jaagus; M. Jüssi; J. Käyhkö; N. Kirchner; E. Kjellström; K. Kulinski; A. Lehmann; G. Lindström; W. May; P. A. Miller; P. A. Miller; V. Mohrholz; B. Müller-Karulis; D. Pavón-Jordán; M. Quante; M. Reckermann; A. Rutgersson; O. P. Savchuk; M. Stendel; L. Tuomi; M. Viitasalo; R. Weisse; W. Zhang;handle: 10138/342962 , 11250/3043839 , 10138/354283
Based on the Baltic Earth Assessment Reports of this thematic issue in Earth System Dynamics and recent peer-reviewed literature, current knowledge of the effects of global warming on past and future changes in climate of the Baltic Sea region is summarised and assessed. The study is an update of the Second Assessment of Climate Change (BACC II) published in 2015 and focuses on the atmosphere, land, cryosphere, ocean, sediments, and the terrestrial and marine biosphere. Based on the summaries of the recent knowledge gained in palaeo-, historical, and future regional climate research, we find that the main conclusions from earlier assessments still remain valid. However, new long-term, homogenous observational records, for example, for Scandinavian glacier inventories, sea-level-driven saltwater inflows, so-called Major Baltic Inflows, and phytoplankton species distribution, and new scenario simulations with improved models, for example, for glaciers, lake ice, and marine food web, have become available. In many cases, uncertainties can now be better estimated than before because more models were included in the ensembles, especially for the Baltic Sea. With the help of coupled models, feedbacks between several components of the Earth system have been studied, and multiple driver studies were performed, e.g. projections of the food web that include fisheries, eutrophication, and climate change. New datasets and projections have led to a revised understanding of changes in some variables such as salinity. Furthermore, it has become evident that natural variability, in particular for the ocean on multidecadal timescales, is greater than previously estimated, challenging our ability to detect observed and projected changes in climate. In this context, the first palaeoclimate simulations regionalised for the Baltic Sea region are instructive. Hence, estimated uncertainties for the projections of many variables increased. In addition to the well-known influence of the North Atlantic Oscillation, it was found that also other low-frequency modes of internal variability, such as the Atlantic Multidecadal Variability, have profound effects on the climate of the Baltic Sea region. Challenges were also identified, such as the systematic discrepancy between future cloudiness trends in global and regional models and the difficulty of confidently attributing large observed changes in marine ecosystems to climate change. Finally, we compare our results with other coastal sea assessments, such as the North Sea Region Climate Change Assessment (NOSCCA), and find that the effects of climate change on the Baltic Sea differ from those on the North Sea, since Baltic Sea oceanography and ecosystems are very different from other coastal seas such as the North Sea. While the North Sea dynamics are dominated by tides, the Baltic Sea is characterised by brackish water, a perennial vertical stratification in the southern subbasins, and a seasonal sea ice cover in the northern subbasins. Peer reviewed
OceanRep; Earth Syst... arrow_drop_down Digitala Vetenskapliga Arkivet - Academic Archive On-lineArticle . 2022 . Peer-reviewedhttps://doi.org/10.5194/esd-20...Preprint . 2021 . Peer-reviewedLicense: CC BYData sources: CrossrefPublikationer från Uppsala Universitet; Digitala Vetenskapliga Arkivet - Academic Archive On-lineOther literature type . Article . 2022 . Peer-reviewedCopernicus Publications; Earth System Dynamics (ESD)Other literature type . 2022Data sources: Copernicus PublicationsHELDA - Digital Repository of the University of HelsinkiReview . 2022 . Peer-reviewedData sources: HELDA - Digital Repository of the University of HelsinkiHELDA - Digital Repository of the University of HelsinkiReview . Other literature type . 2022Data sources: HELDA - Digital Repository of the University of HelsinkiVirtual Library of Klaipeda UniversityArticle . 2022Data sources: Virtual Library of Klaipeda Universityadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/esd-2021-67&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 73 citations 73 popularity Top 1% influence Top 10% impulse Top 1% Powered by BIP!more_vert OceanRep; Earth Syst... arrow_drop_down Digitala Vetenskapliga Arkivet - Academic Archive On-lineArticle . 2022 . Peer-reviewedhttps://doi.org/10.5194/esd-20...Preprint . 2021 . Peer-reviewedLicense: CC BYData sources: CrossrefPublikationer från Uppsala Universitet; Digitala Vetenskapliga Arkivet - Academic Archive On-lineOther literature type . Article . 2022 . Peer-reviewedCopernicus Publications; Earth System Dynamics (ESD)Other literature type . 2022Data sources: Copernicus PublicationsHELDA - Digital Repository of the University of HelsinkiReview . 2022 . Peer-reviewedData sources: HELDA - Digital Repository of the University of HelsinkiHELDA - Digital Repository of the University of HelsinkiReview . Other literature type . 2022Data sources: HELDA - Digital Repository of the University of HelsinkiVirtual Library of Klaipeda UniversityArticle . 2022Data sources: Virtual Library of Klaipeda Universityadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/esd-2021-67&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2021Publisher:Copernicus GmbH Funded by:ARC | Discovery Projects - Gran..., ARC | ARC Future Fellowships - ...ARC| Discovery Projects - Grant ID: DP180100048 ,ARC| ARC Future Fellowships - Grant ID: FT180100606Jun Shao; Lowell D. Stott; Laurie Menviel; Andy Ridgwell; Malin Ödalen; Mayhar Mohtadi;Abstract. During the early part of the last glacial termination (17.2–15 ka) and coincident with a ∼35 ppm rise in atmospheric CO2, a sharp 0.3‰–0.4‰ decline in atmospheric δ13CO2 occurred, potentially constraining the key processes that account for the early deglacial CO2 rise. A comparable δ13C decline has also been documented in numerous marine proxy records from surface and thermocline-dwelling planktic foraminifera. The δ13C decline recorded in planktic foraminifera has previously been attributed to the release of respired carbon from the deep ocean that was subsequently transported within the upper ocean to sites where the signal was recorded (and then ultimately transferred to the atmosphere). Benthic δ13C records from the global upper ocean, including a new record presented here from the tropical Pacific, also document this distinct early deglacial δ13C decline. Here we present modeling evidence to show that rather than respired carbon from the deep ocean propagating directly to the upper ocean prior to reaching the atmosphere, the carbon would have first upwelled to the surface in the Southern Ocean where it would have entered the atmosphere. In this way the transmission of isotopically light carbon to the global upper ocean was analogous to the ongoing ocean invasion of fossil fuel CO2. The model results suggest that thermocline waters throughout the ocean and 500–2000 m water depths were affected by this atmospheric bridge during the early deglaciation.
add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/cp-17-1507-2021&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesgold 5 citations 5 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/cp-17-1507-2021&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publication2021Publicly fundedAuthors: Helen Coxall; Tom Dunkley Jones; Gayatri Marliyani; Emanuela Piga;Helen Coxall; Tom Dunkley Jones; Gayatri Marliyani; Emanuela Piga;doi: 10.1144/jgs2021-006
The Nanggulan section in south central Java comprises open marine sediments and volcanic deposits of Eocene–Oligocene age that accumulated in a marginal basin within the young Sunda Arc complex. A new borehole captures the stratigraphy and showcases the exceptional preservation of calcareous microfossils across an apparently complete Eocene–Oligocene Transition (EOT), a time interval significant for the initiation of continental-scale glaciation on Antarctica. Low-resolution benthic and planktonic foraminifera oxygen and carbon stable isotopes (δ18O and δ13C) record increasing δ18O and δ13C in the basal Oligocene, allowing correlation to global records. Isotopic values imply warm temperatures and relatively high nutrients along the SE Java margin. The Nanggulan EOT is a valuable archive for reconstructing ocean–climate behaviour and plankton evolution and extinction in the Indo-Pacific Warm Pool. The borehole also adds to understanding of the early stages of Sunda Arc volcanism. Supplementary material: Supplementary figures, tables and appendices are available at https://doi.org/10.6084/m9.figshare.c.5429453
Journal of the Geolo... arrow_drop_down Journal of the Geological Society; OpenAPC Global InitiativeArticle . Conference object . 2021 . Peer-reviewedLicense: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1144/jgs2021-006&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 2 citations 2 popularity Average influence Average impulse Average Powered by BIP!more_vert Journal of the Geolo... arrow_drop_down Journal of the Geological Society; OpenAPC Global InitiativeArticle . Conference object . 2021 . Peer-reviewedLicense: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1144/jgs2021-006&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2021Publisher:Springer Science and Business Media LLC Funded by:EC | MUSESEC| MUSESAuthors: Constantino, S. M.; Schlüter, M.; Weber, E. U.; Wijermans, N.;Constantino, S. M.; Schlüter, M.; Weber, E. U.; Wijermans, N.;AbstractThe complex, context-dependent, and dynamic nature of human behavior is increasingly recognized as both an important cause of sustainability problems and potential leverage for their solution. Human beings are diverse, as are the social, ecological, and institutional settings in which they are embedded. Despite this recognition and extensive knowledge about human decision-making in the behavioral sciences, empirical analysis, formal models, and decision support for sustainability policy in natural resource management often either neglect human behavior or are based on narrow and overly simplistic assumptions. Integrating insights from behavioral sciences into sustainability research and policy remains a challenge. This is in part due to the abundance and fragmentation of theories across the social sciences and in part the challenges of translating research across disciplines. We provide a set of tools to support the integration of knowledge about human behavior into empirical and model-based sustainability research. In particular, we (i) develop a process-oriented framework of embedded human cognition (Human Behavior-Cognition in Context or HuB-CC), (ii) select an initial set of 31 theories with the potential to illuminate behavior in natural resource contexts and map them onto the framework, and (iii) suggest pathways for using the framework and mapping to encourage trans-disciplinary investigations, identify and compare theories, and facilitate their integration into empirical research, formal models, and ultimately policy and governance for sustainability. Our theory selection, framework, and mapping offer a foundation—a “living” platform—upon which future collaborative efforts can build to create a resource for scholars and practitioners working at the intersection of social sciences and natural resource management.
Sustainability Scien... arrow_drop_down add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/s11625-021-00989-w&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routeshybrid 30 citations 30 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert Sustainability Scien... arrow_drop_down add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/s11625-021-00989-w&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type , Preprint 2021 Netherlands, United Kingdom, Norway, Brazil, Norway, France, FrancePublisher:Copernicus GmbH Funded by:NSERC, UKRI | SWEET:Super-Warm Early Eo..., EC | PLIO-ESS +5 projectsNSERC ,UKRI| SWEET:Super-Warm Early Eocene Temperatures and climate: understanding the response of the Earth to high CO2 through integrated modelling and data ,EC| PLIO-ESS ,NSF| The Management and Operation of the National Center for Atmoshperic Research (NCAR) ,NSF| Collaborative Research: Paleoclimate perspective on the response of Southwest North American rainfall to elevated greenhouse gases ,NWO| Perturbations of System Earth: Reading the Past to Project the Future - A proposal to create the Netherlands Earth System Science Centre (ESSC) ,NWO| Mechanisms of major climate system reorganisations in the Cenozoic ,NSF| Collaborative Research: Arctic Temperature Amplification during the Middle Pliocene (ArcAMP): Assessing the interaction among feedback mechanismsSathyanadh, Anusha; Monteil, Guillaume; Scholze, Marko; Klosterhalfen, Anne; Laudon, Hjalmar; Wu, Zhendong; Gerbig, Christoph; Peters, Wouter; Bastrikov, Vladislav; Nilsson, Mats, B; Peichl, Matthias; Oldeman, Arthur, M; Baatsen, Michiel, L J; von Der Heydt, Anna, S; Dijkstra, Henk, A; Tindall, Julia, C; Abe-Ouchi, Ayako; Booth, Alice, R; Brady, Esther, C; Chan, Wing-Le; Chandan, Deepak; Chandler, Mark, A; Contoux, Camille; Feng, Ran; Guo, Chuncheng; Haywood, Alan, M; Hunter, Stephen, J; Kamae, Youichi; Li, Qiang; Li, Xiangyu; Lohmann, Gerrit; Lunt, Daniel, J; Nisancioglu, Kerim, H; Otto-Bliesner, Bette, L; Peltier, W, Richard; Pontes, Gabriel, M; Ramstein, Gilles; Sohl, Linda, E; Stepanek, Christian; Tan, Ning; Zhang, Qiong; Zhang, Zhongshi; Wainer, Ilana; Williams, Charles, J R;The mid-Pliocene warm period (3.264–3.025 Ma) is the most recent geological period during which atmospheric CO2 levels were similar to recent historical values (∼400 ppm). Several proxy reconstructions for the mid-Pliocene show highly reduced zonal sea surface temperature (SST) gradients in the tropical Pacific Ocean, indicating an El Niño-like mean state. However, past modelling studies do not show these highly reduced gradients. Efforts to understand mid-Pliocene climate dynamics have led to the Pliocene Model Intercomparison Project (PlioMIP). Results from the first phase (PlioMIP1) showed clear El Niño variability (albeit significantly reduced) and did not show the greatly reduced time-mean zonal SST gradient suggested by some of the proxies. In this work, we study El Niño–Southern Oscillation (ENSO) variability in the PlioMIP2 ensemble, which consists of additional global coupled climate models and updated boundary conditions compared to PlioMIP1. We quantify ENSO amplitude, period, spatial structure and “flavour”, as well as the tropical Pacific annual mean state in mid-Pliocene and pre-industrial simulations. Results show a reduced ENSO amplitude in the model-ensemble mean (−24 %) with respect to the pre-industrial, with 15 out of 17 individual models showing such a reduction. Furthermore, the spectral power of this variability considerably decreases in the 3–4-year band. The spatial structure of the dominant empirical orthogonal function shows no particular change in the patterns of tropical Pacific variability in the model-ensemble mean, compared to the pre-industrial. Although the time-mean zonal SST gradient in the equatorial Pacific decreases for 14 out of 17 models (0.2 ∘C reduction in the ensemble mean), there does not seem to be a correlation with the decrease in ENSO amplitude. The models showing the most “El Niño-like” mean state changes show a similar ENSO amplitude to that in the pre-industrial reference, while models showing more “La Niña-like” mean state changes generally show a large reduction in ENSO variability. The PlioMIP2 results show a reasonable agreement with both time-mean proxies indicating a reduced zonal SST gradient and reconstructions indicating a reduced, or similar, ENSO variability. International audience
CORE (RIOXX-UK Aggre... arrow_drop_down Copernicus Publications; Climate of the Past (CP)Other literature type . 2021Data sources: Copernicus Publicationshttps://doi.org/10.5194/cp-202...Preprint . 2021 . Peer-reviewedLicense: CC BYData sources: CrossrefNORCE Research Archive; Norwegian Open Research ArchivesArticle . 2021 . Peer-reviewedBergen Open Research Archive - UiB; Norwegian Open Research ArchivesArticle . 2021 . Peer-reviewedLicense: CC BYMémoires en Sciences de l'Information et de la Communication; HAL-CEAArticle . 2021License: CC BYFull-Text: https://hal.science/hal-03469874/documentMémoires en Sciences de l'Information et de la Communication; HAL-CEAArticle . 2021License: CC BYFull-Text: https://hal.science/hal-03495127/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/cp-2021-58&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 9 citations 9 popularity Top 10% influence Average impulse Top 10% Powered by BIP!visibility 4visibility views 4 download downloads 1 Powered bymore_vert CORE (RIOXX-UK Aggre... arrow_drop_down Copernicus Publications; Climate of the Past (CP)Other literature type . 2021Data sources: Copernicus Publicationshttps://doi.org/10.5194/cp-202...Preprint . 2021 . Peer-reviewedLicense: CC BYData sources: CrossrefNORCE Research Archive; Norwegian Open Research ArchivesArticle . 2021 . Peer-reviewedBergen Open Research Archive - UiB; Norwegian Open Research ArchivesArticle . 2021 . Peer-reviewedLicense: CC BYMémoires en Sciences de l'Information et de la Communication; HAL-CEAArticle . 2021License: CC BYFull-Text: https://hal.science/hal-03469874/documentMémoires en Sciences de l'Information et de la Communication; HAL-CEAArticle . 2021License: CC BYFull-Text: https://hal.science/hal-03495127/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/cp-2021-58&type=result"></script>'); --> </script>
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description Publicationkeyboard_double_arrow_right Article , Research , Conference object , Preprint 2021 Sweden, Belgium, Italy, Germany, Denmark, Belgium, United KingdomPublisher:IOP Publishing Funded by:UKRI | RootDetect: Remote Detect..., UKRI | Improved Loss Modelling o...UKRI| RootDetect: Remote Detection and Precision Management of Root Health ,UKRI| Improved Loss Modelling of SMC ComponentsAbbasi, R.; Ackermann, M.; Andeen, K.; Fox, D.; Franckowiak, A.; Friedman, E.; Fritz, A.; Fürst, Philipp; Gaisser, T. K.; Gallagher, J.; Ganster, Erik; Garcia, Alfonso; Garrappa, S.; Anderson, T.; Gerhardt, L.; Ghadimi, A.; Glaser, C.; Glauch, T.; Glüsenkamp, T.; Goldschmidt, A.; Gonzalez, J. G.; Goswami, S.; Grant, D.; Grégoire, T.; Anton, G.; Griswold, S.; Gündüz, M.; Günther, C.; Haack, Christian; Hallgren, A.; Halliday, R.; Halve, Lasse Yannik; Halzen, F.; Minh, M. Ha; Hanson, K.; Argüelles, C.; Hardin, J.; Harnisch, A. A.; Haungs, A.; Hauser, Simon; Hebecker, D.; Helbing, K.; Henningsen, F.; Hettinger, E. C.; Hickford, S.; Hignight, J.; Ashida, Y.; Hill, C.; Hill, G. C.; Hoffman, K. D.; Hoffmann, R.; Hoinka, T.; Hokanson-Fasig, B.; Hoshina, K.; Huang, F.; Huber, M.; Huber, T.; Axani, S.; Hultqvist, K.; Hünnefeld, M.; Hussain, R.; In, S.; Iovine, N.; Ishihara, A.; Jansson, M.; Japaridze, G. S.; Jeong, M.; Jones, B. J. P.; Bai, X.; Kang, D.; Kang, W.; Kang, X.; Kappes, A.; Kappesser, D.; Karg, T.; Karl, M.; Karle, A.; Katz, U.; Kauer, M.; V., A. Balagopal; Kellermann, Moritz; Kelley, J. L.; Kheirandish, A.; Kin, K.; Kintscher, T.; Kiryluk, J.; Klein, S. R.; Koirala, R.; Kolanoski, H.; Kontrimas, T.; Barbano, A.; Köpke, L.; Kopper, C.; Kopper, S.; Koskinen, D. J.; Koundal, P.; Kovacevich, M.; Kowalski, M.; Kozynets, T.; Kun, E.; Kurahashi, N.; Barwick, S. W.; Lad, N.; Gualda, C. Lagunas; Lanfranchi, J. L.; Larson, M. J.; Lauber, F.; Lazar, J. P.; Lee, J. W.; Leonard, K.; Leszczyńska, A.; Li, Y.; Adams, J.; Bastian, B.; Lincetto, M.; Liu, Q. R.; Liubarska, M.; Lohfink, E.; Mariscal, C. J. Lozano; Lu, L.; Lucarelli, F.; Ludwig, A.; Luszczak, W.; Lyu, Y.; Basu, V.; Ma, W. Y.; Madsen, J.; Mahn, K. B. M.; Makino, Y.; Mancina, S.; Maris, I. C.; Maruyama, R.; Mase, K.; McElroy, T.; McNally, F.; Baur, S.; Mead, J. V.; Meagher, K.; Medina, A.; Meier, M.; Meighen-Berger, S.; Micallef, J.; Mockler, D.; Montaruli, T.; Moore, R. W.; Morse, R.; Bay, R.; Moulai, M.; Naab, R.; Nagai, R.; Naumann, U.; Necker, J.; Nguyễn, L. V.; Niederhausen, H.; Nisa, M. U.; Nowicki, S. C.; Nygren, D. R.; Beatty, J. J.; Pollmann, A. Obertacke; Oehler, M.; Olivas, A.; O'Sullivan, E.; Pandya, H.; Pankova, D. V.; Park, N.; Parker, G. K.; Paudel, E. N.; Paul, Larissa; Becker, K.-H.; Heros, C. Pérez de los; Peters, L.; Peterson, J.; Philippen, Saskia; Pieloth, D.; Pieper, S.; Pittermann, M.; Pizzuto, A.; Plum, M.; Popovych, Y.; Tjus, J. Becker; Porcelli, A.; Rodriguez, M. Prado; Price, P. B.; Pries, B.; Przybylski, G. T.; Raab, C.; Raissi, A.; Rameez, M.; Rawlins, K.; Rea, I. C.; Bellenghi, C.; Rehman, A.; Reichherzer, P.; Reimann, René; Renzi, G.; Resconi, E.; Reusch, S.; Rhode, W.; Richman, M.; Riedel, B.; BenZvi, S.; Robertson, S.; Rongen, Martin; Rott, C.; Ryckbosch, D.; Cantu, D. Rysewyk; Safa, I.; Sandrock, A.; Sandroos, J.; Santander, M.; Sarkar, S.; Satalecka, K.; Aguilar, J. A.; Bernardini, E.; Schneider, A.; Schneider, J.; Schröder, F. G.; Schumacher, Lisa Johanna; Schwefer, Georg; Sclafani, S.; Silva, M.; Smithers, B.; Soedingrekso, J.; Soldin, D.; Spiczak, G. M.; Spiering, C.; Stachurska, J.; Stein, R.; Stettner, Jöran Benjamin; Stezelberger, T.; Stuttard, T.; Sullivan, G. W.; Taboada, I.; Tenholt, F.; Ter-Antonyan, S.; Tollefson, K.; Tomankova, L.; Toscano, S.; Blaufuss, E.; Trettin, A.; Tung, C. F.; Turcati, A.; Turley, C. F.; Elorrieta, M. A. Unland; Blot, S.; Vandenbroucke, J.; van Eijndhoven, N.; van Santen, J.; Verpoest, S.; Walck, C.; Watson, T. B.; Weaver, C.; Weldert, J.; Wendt, C.; Whitehorn, N.; Wiebusch, Christopher; Wolf, M.; Yoshida, S.; Yuan, T.; Böser, S.; Ahlers, M.; Botner, O.; Bradascio, F.; Bron, S.; Burgman, A.; Campana, M. A.; Chen, C.; Chirkin, D.; Clark, B. A.; Clark, K.; Coleman, A.; Collin, G. H.; Conrad, J. M.; Coppin, P.; Correa, P.; Cowen, D. F.; Cross, R.; Dave, P.; De Clercq, C.; DeLaunay, J. J.; Dembinski, H.; Desai, A.; Desiati, P.; de Vries, K. D.; de Wasseige, G.; de With, M.; DeYoung, T.; Diaz, A.; Díaz-Vélez, J. C.; Dujmovic, H.; Eller, P.; Evenson, P. A.; Fazely, A. R.; Fienberg, A. T.; Finley, C.;Ultraluminous infrared galaxies (ULIRGs) have infrared luminosities L $_{IR}$ ��� 10$^{12}$ L $_{���}$, making them the most luminous objects in the infrared sky. These dusty objects are generally powered by starbursts with star formation rates that exceed 100 M $_{���}$ yr$^{���1}$, possibly combined with a contribution from an active galactic nucleus. Such environments make ULIRGs plausible sources of astrophysical high-energy neutrinos, which can be observed by the IceCube Neutrino Observatory at the South Pole. We present a stacking search for high-energy neutrinos from a representative sample of 75 ULIRGs with redshift z ��� 0.13 using 7.5 yr of IceCube data. The results are consistent with a background-only observation, yielding upper limits on the neutrino flux from these 75 ULIRGs. For an unbroken E $^{���2.5}$ power-law spectrum, we report an upper limit on the stacked flux at 90% confidence level. In addition, we constrain the contribution of the ULIRG source population to the observed diffuse astrophysical neutrino flux as well as model predictions. The astrophysical journal 926(1), 59 (2022). doi:10.3847/1538-4357/ac3cb6 Published by Univ., Chicago, Ill. [u.a.]
arXiv.org e-Print Ar... arrow_drop_down arXiv.org e-Print ArchiveOther literature type . Preprint . 2021Data sources: arXiv.org e-Print ArchiveVrije Universiteit Brussel Research Portal; Journal of Physics : Conference SeriesArticle . Conference object . 2021 . 2022 . Peer-reviewedLicense: CC BYPublikationsserver der RWTH Aachen UniversityArticle . 2022Data sources: Publikationsserver der RWTH Aachen UniversityGhent University Academic BibliographyArticle . 2022Data sources: Ghent University Academic BibliographyOxford University Research Archive; The Astrophysical JournalArticle . 2022 . Peer-reviewedLicense: CC BYedoc-Server. Open-Access-Publikationsserver der Humboldt-Universität zu BerlinArticle . 2022 . Peer-reviewedCopenhagen University Research Information SystemArticle . 2022Data sources: Copenhagen University Research Information SystemVrije Universiteit Brussel Research PortalArticle . 2022Data sources: Vrije Universiteit Brussel Research PortalVrije Universiteit Brussel Research PortalConference object . 2022Data sources: Vrije Universiteit Brussel Research PortalPublikationsserver der RWTH Aachen UniversityPreprint . 2021Data sources: Publikationsserver der RWTH Aachen UniversityGhent University Academic BibliographyArticle . 2022Data sources: Ghent University Academic Bibliographyedoc-Server. Open-Access-Publikationsserver der Humboldt-Universität zu BerlinArticle . 2022 . Peer-reviewedLicense: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 7 citations 7 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert arXiv.org e-Print Ar... arrow_drop_down arXiv.org e-Print ArchiveOther literature type . Preprint . 2021Data sources: arXiv.org e-Print ArchiveVrije Universiteit Brussel Research Portal; Journal of Physics : Conference SeriesArticle . Conference object . 2021 . 2022 . Peer-reviewedLicense: CC BYPublikationsserver der RWTH Aachen UniversityArticle . 2022Data sources: Publikationsserver der RWTH Aachen UniversityGhent University Academic BibliographyArticle . 2022Data sources: Ghent University Academic BibliographyOxford University Research Archive; The Astrophysical JournalArticle . 2022 . Peer-reviewedLicense: CC BYedoc-Server. Open-Access-Publikationsserver der Humboldt-Universität zu BerlinArticle . 2022 . Peer-reviewedCopenhagen University Research Information SystemArticle . 2022Data sources: Copenhagen University Research Information SystemVrije Universiteit Brussel Research PortalArticle . 2022Data sources: Vrije Universiteit Brussel Research PortalVrije Universiteit Brussel Research PortalConference object . 2022Data sources: Vrije Universiteit Brussel Research PortalPublikationsserver der RWTH Aachen UniversityPreprint . 2021Data sources: Publikationsserver der RWTH Aachen UniversityGhent University Academic BibliographyArticle . 2022Data sources: Ghent University Academic Bibliographyedoc-Server. Open-Access-Publikationsserver der Humboldt-Universität zu BerlinArticle . 2022 . Peer-reviewedLicense: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2021 Switzerland, Germany, ItalyPublisher:American Association for the Advancement of Science (AAAS) Funded by:EC | RESOLUTION, EC | SUCCESSEC| RESOLUTION ,EC| SUCCESSAlan Cooper; Chris S. M. Turney; Jonathan G. Palmer; Alan G. Hogg; Matt S. McGlone; Janet M. Wilmshurst; Andrew Lorrey; Timothy J Heaton; James M. Russell; Ken McCracken; Julien Anet; Eugene Rozanov; Marina Friedel; Ivo Suter; Thomas Peter; Raimund Muscheler; Florian Adolphi; Anthony Dosseto; J. Tyler Faith; Pavla Fenwick; Christopher J. Fogwill; Konrad A Hughen; Matthew Lipson; Jiabo Liu; Norbert R. Nowaczyk; Eleanor Rainsley; Christopher Bronk Ramsey; Paolo Sebastianelli; Yassine Souilmi; Janelle Stevenson; Zoë Thomas; Raymond Tobler; Roland Zech;pmc: PMC7612203
handle: 11585/839023
Cooper et al . (Research Articles, 19 February 2021, p. 811) propose that the Laschamps geomagnetic inversion ~42,000 years ago drove global climatic shifts, causing major behavioral changes within prehistoric groups, as well as events of human and megafaunal extinction. Other scientific studies indicate that this proposition is unproven from the current archaeological, paleoanthropological, and genetic records.
Archivio istituziona... arrow_drop_down Europe PubMed CentralArticle . 2021Full-Text: http://europepmc.org/articles/PMC7612203Data sources: PubMed CentralGFZ German Research Centre for GeosciencesArticle . 2021Data sources: GFZ German Research Centre for GeosciencesGFZ German Research Centre for GeosciencesArticle . 2021Data sources: GFZ German Research Centre for GeosciencesScienceOther literature type . Article . 2021 . Peer-reviewedZHAW digitalcollection; ScienceOther literature type . Article . 2022 . 2021 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess Routesbronze 4 citations 4 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert Archivio istituziona... arrow_drop_down Europe PubMed CentralArticle . 2021Full-Text: http://europepmc.org/articles/PMC7612203Data sources: PubMed CentralGFZ German Research Centre for GeosciencesArticle . 2021Data sources: GFZ German Research Centre for GeosciencesGFZ German Research Centre for GeosciencesArticle . 2021Data sources: GFZ German Research Centre for GeosciencesScienceOther literature type . Article . 2021 . Peer-reviewedZHAW digitalcollection; ScienceOther literature type . Article . 2022 . 2021 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1126/science.abh3655&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Preprint , Article , Other literature type 2021 DenmarkPublisher:Copernicus GmbH Funded by:SNSF | EGRIP: The Swiss Contribu..., UKRI | Developing and testing a ...SNSF| EGRIP: The Swiss Contribution ,UKRI| Developing and testing a new Energy from Waste gasification feedstockGiulia Sinnl; Mai Winstrup; Tobias Erhardt; Eliza Cook; Camilla Marie Jensen; Anders Svensson; Bo Møllesøe Vinther; Raimund Muscheler; Sune Olander Rasmussen;Abstract. Ice-core timescales are vital for the understanding of past climate; hence they should be updated whenever significant amounts of new data can contribute to improvements. Here, the Greenland ice-core chronology was revised for the last 3835 years by synchronizing six deep ice-cores and three shallow ice-cores from the central Greenland ice sheet. A layer-counting bias was found in all ice cores because of site-specific signal disturbances, and a manual comparison of all ice cores was deemed necessary to increase timescale accuracy. A new method was applied by combining automated counting of annual layers on multiple parallel proxies and manual fine-tuning. After examining sources of error and their correlation lengths, the uncertainty rate was quantified to be one year per century. The new timescale is younger than the previous Greenland chronology by about 13 years at 3800 years ago. The most recent 800 years are largely unaffected by the revision, while the slope of the offset between timescales is steepest between 800 and 1000 years ago. Moreover, offset-oscillations of about 5 years around the average are observed between 2500 and 3800 years ago. The non-linear offset behavior is attributed to previous mismatches of volcanic eruptions, to the much more extensive data set available to this study, and to the finer resolution of the new ice-core matching. In response to volcanic eruptions, averaged water isotopes and layer thicknesses from Greenland ice cores provide evidence of notable cooling lasting for up to a decade, longer than reported in previous studies of volcanic forcing. By analysis of the common variations of cosmogenic radionuclides, the new ice-core timescale is found to be in alignment with the IntCal20 curve. Radiocarbon dated evidence found in the proximity of eruption sites such as Vesuvius or Thera was compared to the ice-core dataset; no conclusive evidence was found regarding if these two eruptions can be matched to acidity spikes in the ice cores. A hitherto unidentified cooling event in the ice cores is observed at about 3600 years ago (1600 BCE), which could have been caused by a large eruption which is, however, not clearly recorded in the acidity signal. The hunt for clear signs of the Thera eruption in Greenland ice-cores thus remains elusive.
https://doi.org/10.5... arrow_drop_down https://doi.org/10.5194/cp-202...Preprint . 2021 . Peer-reviewedLicense: CC BYData sources: CrossrefCopenhagen University Research Information SystemArticle . 2022Data sources: Copenhagen University Research Information SystemOnline Research Database In TechnologyArticle . 2022Data sources: Online Research Database In TechnologyCopernicus Publications; Climate of the Past (CP)Other literature type . 2022Data sources: Copernicus Publicationsadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess Routesgold 9 citations 9 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert https://doi.org/10.5... arrow_drop_down https://doi.org/10.5194/cp-202...Preprint . 2021 . Peer-reviewedLicense: CC BYData sources: CrossrefCopenhagen University Research Information SystemArticle . 2022Data sources: Copenhagen University Research Information SystemOnline Research Database In TechnologyArticle . 2022Data sources: Online Research Database In TechnologyCopernicus Publications; Climate of the Past (CP)Other literature type . 2022Data sources: Copernicus Publicationsadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/cp-2021-155&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2021 France, Netherlands, FrancePublisher:Elsevier BV Frank, Anja,; Frei, Robert; Moutafi, Ioanna; Voutsaki, Sofia; Orgeolet, Raphaël; Kristiansen, Kristian; Frei, Karin,;Sr isotopes are a powerful tool used to reconstruct human mobility in archaeology. This requires extensive bioavailable 87Sr/86Sr baselines used as reference for deciphering potential areas of origin. We define the first extensive bioavailable Sr isotope baselines for the different geographical regions and surface lithologies of Greece by combining new Sr data with previously published bioavailable 87Sr/86Sr data. We present 82 new Sr concentrations and 87Sr/86Sr signatures of plants, soil leachates, surface waters and spring waters from Central Greece and combine these with published baseline values from all over Greece. We define individual baselines for ten of the thirteen geographical regions of Greece. We also provide soil leachate 87Sr/86Sr ratios from the two archaeological Bronze Age sites of Kirrha and Ayios Vasileios in Central and Southern Greece and demonstrate the validity and applicability of the new baselines for these sites. The bioavailable 87Sr/86Sr compositions of Central Greece define a narrow range of 87Sr/86Sr values between 0.70768 — 0.71021, with the widest range observed for the soil leachates. Sr derived from carbonate weathering appears to be the most important Sr source sampled by the proxies. There is an overall larger variability in baseline ranges of the different geographical regions, the narrowest is that for West Greece and the widest that for West Macedonia. In addition, we computed statistical Sr isotope ranges for the five main surface lithological groups characterising the sampling sites of the various proxies. Narrowly ranged, unradiogenic bioavailable Sr isotope signatures are typical of areas characterised by igneous outcrops as well as by Cenozoic and Mesozoic sediments. Areas, where Palaeozoic and Precambrian bedrock outcrops dominate, produce significantly wider ranges. Our study promotes the usefulness of multi-proxy baselines for geographical reference purposes and thus their promising applicability for future human mobility studies.
NARCIS; The Science ... arrow_drop_down NARCIS; The Science of The Total EnvironmentArticle . 2021The Science of The Total EnvironmentArticle . 2021 . Peer-reviewedLicense: Elsevier TDMData sources: CrossrefHyper Article en Ligne - Sciences de l'Homme et de la Société; Hal-DiderotArticle . 2021License: CC BY NC NDHAL AMU; Mémoires en Sciences de l'Information et de la CommunicationArticle . 2021License: CC BY NC NDadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen bronze 13 citations 13 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert NARCIS; The Science ... arrow_drop_down NARCIS; The Science of The Total EnvironmentArticle . 2021The Science of The Total EnvironmentArticle . 2021 . Peer-reviewedLicense: Elsevier TDMData sources: CrossrefHyper Article en Ligne - Sciences de l'Homme et de la Société; Hal-DiderotArticle . 2021License: CC BY NC NDHAL AMU; Mémoires en Sciences de l'Information et de la CommunicationArticle . 2021License: CC BY NC NDadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.scitotenv.2021.148156&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2021Funded by:NSERC, NSF | Collaborative Research: P..., NSF | Collaborative Research: A... +1 projectsNSERC ,NSF| Collaborative Research: Paleoclimate perspective on the response of Southwest North American rainfall to elevated greenhouse gases ,NSF| Collaborative Research: Arctic Temperature Amplification during the Middle Pliocene (ArcAMP): Assessing the interaction among feedback mechanisms ,NSF| The Management and Operation of the National Center for Atmoshperic Research (NCAR)Zhongshi Zhang; Daniel Lunt; Ellen Berntell; Stephen Hunter; Wing-Le Chan; Qiang Li; Charles Williams; Linda Sohl; Christian Stepanek; Xiangyu Li;Abstract. The mid-Pliocene warm period (mPWP; ∼3.2 million years ago) is seen as the most recent time period characterized by a warm climate state, with similar to modern geography and ∼400 ppmv atmospheric CO2 concentration, and is therefore often considered an interesting analogue for near-future climate projections. Paleoenvironmental reconstructions indicate higher surface temperatures, decreasing tropical deserts, and a more humid climate in West Africa characterized by a strengthened West African Monsoon (WAM). Using model results from the second phase of the Pliocene Modelling Intercomparison Project (PlioMIP2) ensemble, we analyse changes of the WAM rainfall during the mPWP by comparing them with the control simulations for the pre-industrial period. The ensemble shows a robust increase in the summer rainfall over West Africa and the Sahara region, with an average increase of 2.5 mm/d, contrasted by a rainfall decrease over the equatorial Atlantic. An anomalous warming of the Sahara and deepening of the Saharan Heat Low, seen in >90 % of the models, leads to a strengthening of the WAM and an increased monsoonal flow into the continent. A similar warming of the Sahara is seen in future projections using both phase 3 and 5 of the Coupled Model Intercomparison Project (CMIP3 and CMIP5). Though previous studies of future projections indicate a west–east drying–wetting contrast over the Sahel, PlioMIP2 simulations indicate a uniform rainfall increase in that region in warm climates characterized by increasing greenhouse gas forcing. We note that this effect will further depend on the long-term response of the vegetation to the CO2 forcing.
Climate of the Past ... arrow_drop_down Climate of the Past (CP); OpenAPC Global InitiativeArticle . Conference object . 2021 . Peer-reviewedLicense: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 9 citations 9 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert Climate of the Past ... arrow_drop_down Climate of the Past (CP); OpenAPC Global InitiativeArticle . Conference object . 2021 . Peer-reviewedLicense: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/cp-17-1777-2021&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Preprint , Other literature type , Review 2021 Sweden, Norway, Germany, Lithuania, Austria, FinlandPublisher:Copernicus GmbH Funded by:EC | BONUS+EC| BONUS+H. E. M. Meier; H. E. M. Meier; M. Kniebusch; C. Dieterich; M. Gröger; E. Zorita; R. Elmgren; K. Myrberg; K. Myrberg; M. P. Ahola; A. Bartosova; E. Bonsdorff; F. Börgel; R. Capell; I. Carlén; T. Carlund; J. Carstensen; O. B. Christensen; V. Dierschke; C. Frauen; C. Frauen; M. Frederiksen; E. Gaget; E. Gaget; A. Galatius; J. J. Haapala; A. Halkka; G. Hugelius; G. Hugelius; B. Hünicke; J. Jaagus; M. Jüssi; J. Käyhkö; N. Kirchner; E. Kjellström; K. Kulinski; A. Lehmann; G. Lindström; W. May; P. A. Miller; P. A. Miller; V. Mohrholz; B. Müller-Karulis; D. Pavón-Jordán; M. Quante; M. Reckermann; A. Rutgersson; O. P. Savchuk; M. Stendel; L. Tuomi; M. Viitasalo; R. Weisse; W. Zhang;handle: 10138/342962 , 11250/3043839 , 10138/354283
Based on the Baltic Earth Assessment Reports of this thematic issue in Earth System Dynamics and recent peer-reviewed literature, current knowledge of the effects of global warming on past and future changes in climate of the Baltic Sea region is summarised and assessed. The study is an update of the Second Assessment of Climate Change (BACC II) published in 2015 and focuses on the atmosphere, land, cryosphere, ocean, sediments, and the terrestrial and marine biosphere. Based on the summaries of the recent knowledge gained in palaeo-, historical, and future regional climate research, we find that the main conclusions from earlier assessments still remain valid. However, new long-term, homogenous observational records, for example, for Scandinavian glacier inventories, sea-level-driven saltwater inflows, so-called Major Baltic Inflows, and phytoplankton species distribution, and new scenario simulations with improved models, for example, for glaciers, lake ice, and marine food web, have become available. In many cases, uncertainties can now be better estimated than before because more models were included in the ensembles, especially for the Baltic Sea. With the help of coupled models, feedbacks between several components of the Earth system have been studied, and multiple driver studies were performed, e.g. projections of the food web that include fisheries, eutrophication, and climate change. New datasets and projections have led to a revised understanding of changes in some variables such as salinity. Furthermore, it has become evident that natural variability, in particular for the ocean on multidecadal timescales, is greater than previously estimated, challenging our ability to detect observed and projected changes in climate. In this context, the first palaeoclimate simulations regionalised for the Baltic Sea region are instructive. Hence, estimated uncertainties for the projections of many variables increased. In addition to the well-known influence of the North Atlantic Oscillation, it was found that also other low-frequency modes of internal variability, such as the Atlantic Multidecadal Variability, have profound effects on the climate of the Baltic Sea region. Challenges were also identified, such as the systematic discrepancy between future cloudiness trends in global and regional models and the difficulty of confidently attributing large observed changes in marine ecosystems to climate change. Finally, we compare our results with other coastal sea assessments, such as the North Sea Region Climate Change Assessment (NOSCCA), and find that the effects of climate change on the Baltic Sea differ from those on the North Sea, since Baltic Sea oceanography and ecosystems are very different from other coastal seas such as the North Sea. While the North Sea dynamics are dominated by tides, the Baltic Sea is characterised by brackish water, a perennial vertical stratification in the southern subbasins, and a seasonal sea ice cover in the northern subbasins. Peer reviewed
OceanRep; Earth Syst... arrow_drop_down Digitala Vetenskapliga Arkivet - Academic Archive On-lineArticle . 2022 . Peer-reviewedhttps://doi.org/10.5194/esd-20...Preprint . 2021 . Peer-reviewedLicense: CC BYData sources: CrossrefPublikationer från Uppsala Universitet; Digitala Vetenskapliga Arkivet - Academic Archive On-lineOther literature type . Article . 2022 . Peer-reviewedCopernicus Publications; Earth System Dynamics (ESD)Other literature type . 2022Data sources: Copernicus PublicationsHELDA - Digital Repository of the University of HelsinkiReview . 2022 . Peer-reviewedData sources: HELDA - Digital Repository of the University of HelsinkiHELDA - Digital Repository of the University of HelsinkiReview . Other literature type . 2022Data sources: HELDA - Digital Repository of the University of HelsinkiVirtual Library of Klaipeda UniversityArticle . 2022Data sources: Virtual Library of Klaipeda Universityadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 73 citations 73 popularity Top 1% influence Top 10% impulse Top 1% Powered by BIP!more_vert OceanRep; Earth Syst... arrow_drop_down Digitala Vetenskapliga Arkivet - Academic Archive On-lineArticle . 2022 . Peer-reviewedhttps://doi.org/10.5194/esd-20...Preprint . 2021 . Peer-reviewedLicense: CC BYData sources: CrossrefPublikationer från Uppsala Universitet; Digitala Vetenskapliga Arkivet - Academic Archive On-lineOther literature type . Article . 2022 . Peer-reviewedCopernicus Publications; Earth System Dynamics (ESD)Other literature type . 2022Data sources: Copernicus PublicationsHELDA - Digital Repository of the University of HelsinkiReview . 2022 . Peer-reviewedData sources: HELDA - Digital Repository of the University of HelsinkiHELDA - Digital Repository of the University of HelsinkiReview . Other literature type . 2022Data sources: HELDA - Digital Repository of the University of HelsinkiVirtual Library of Klaipeda UniversityArticle . 2022Data sources: Virtual Library of Klaipeda Universityadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/esd-2021-67&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2021Publisher:Copernicus GmbH Funded by:ARC | Discovery Projects - Gran..., ARC | ARC Future Fellowships - ...ARC| Discovery Projects - Grant ID: DP180100048 ,ARC| ARC Future Fellowships - Grant ID: FT180100606Jun Shao; Lowell D. Stott; Laurie Menviel; Andy Ridgwell; Malin Ödalen; Mayhar Mohtadi;Abstract. During the early part of the last glacial termination (17.2–15 ka) and coincident with a ∼35 ppm rise in atmospheric CO2, a sharp 0.3‰–0.4‰ decline in atmospheric δ13CO2 occurred, potentially constraining the key processes that account for the early deglacial CO2 rise. A comparable δ13C decline has also been documented in numerous marine proxy records from surface and thermocline-dwelling planktic foraminifera. The δ13C decline recorded in planktic foraminifera has previously been attributed to the release of respired carbon from the deep ocean that was subsequently transported within the upper ocean to sites where the signal was recorded (and then ultimately transferred to the atmosphere). Benthic δ13C records from the global upper ocean, including a new record presented here from the tropical Pacific, also document this distinct early deglacial δ13C decline. Here we present modeling evidence to show that rather than respired carbon from the deep ocean propagating directly to the upper ocean prior to reaching the atmosphere, the carbon would have first upwelled to the surface in the Southern Ocean where it would have entered the atmosphere. In this way the transmission of isotopically light carbon to the global upper ocean was analogous to the ongoing ocean invasion of fossil fuel CO2. The model results suggest that thermocline waters throughout the ocean and 500–2000 m water depths were affected by this atmospheric bridge during the early deglaciation.
add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/cp-17-1507-2021&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routesgold 5 citations 5 popularity Top 10% influence Average impulse Average Powered by BIP!more_vert add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/cp-17-1507-2021&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publication2021Publicly fundedAuthors: Helen Coxall; Tom Dunkley Jones; Gayatri Marliyani; Emanuela Piga;Helen Coxall; Tom Dunkley Jones; Gayatri Marliyani; Emanuela Piga;doi: 10.1144/jgs2021-006
The Nanggulan section in south central Java comprises open marine sediments and volcanic deposits of Eocene–Oligocene age that accumulated in a marginal basin within the young Sunda Arc complex. A new borehole captures the stratigraphy and showcases the exceptional preservation of calcareous microfossils across an apparently complete Eocene–Oligocene Transition (EOT), a time interval significant for the initiation of continental-scale glaciation on Antarctica. Low-resolution benthic and planktonic foraminifera oxygen and carbon stable isotopes (δ18O and δ13C) record increasing δ18O and δ13C in the basal Oligocene, allowing correlation to global records. Isotopic values imply warm temperatures and relatively high nutrients along the SE Java margin. The Nanggulan EOT is a valuable archive for reconstructing ocean–climate behaviour and plankton evolution and extinction in the Indo-Pacific Warm Pool. The borehole also adds to understanding of the early stages of Sunda Arc volcanism. Supplementary material: Supplementary figures, tables and appendices are available at https://doi.org/10.6084/m9.figshare.c.5429453
Journal of the Geolo... arrow_drop_down Journal of the Geological Society; OpenAPC Global InitiativeArticle . Conference object . 2021 . Peer-reviewedLicense: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1144/jgs2021-006&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 2 citations 2 popularity Average influence Average impulse Average Powered by BIP!more_vert Journal of the Geolo... arrow_drop_down Journal of the Geological Society; OpenAPC Global InitiativeArticle . Conference object . 2021 . Peer-reviewedLicense: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1144/jgs2021-006&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2021Publisher:Springer Science and Business Media LLC Funded by:EC | MUSESEC| MUSESAuthors: Constantino, S. M.; Schlüter, M.; Weber, E. U.; Wijermans, N.;Constantino, S. M.; Schlüter, M.; Weber, E. U.; Wijermans, N.;AbstractThe complex, context-dependent, and dynamic nature of human behavior is increasingly recognized as both an important cause of sustainability problems and potential leverage for their solution. Human beings are diverse, as are the social, ecological, and institutional settings in which they are embedded. Despite this recognition and extensive knowledge about human decision-making in the behavioral sciences, empirical analysis, formal models, and decision support for sustainability policy in natural resource management often either neglect human behavior or are based on narrow and overly simplistic assumptions. Integrating insights from behavioral sciences into sustainability research and policy remains a challenge. This is in part due to the abundance and fragmentation of theories across the social sciences and in part the challenges of translating research across disciplines. We provide a set of tools to support the integration of knowledge about human behavior into empirical and model-based sustainability research. In particular, we (i) develop a process-oriented framework of embedded human cognition (Human Behavior-Cognition in Context or HuB-CC), (ii) select an initial set of 31 theories with the potential to illuminate behavior in natural resource contexts and map them onto the framework, and (iii) suggest pathways for using the framework and mapping to encourage trans-disciplinary investigations, identify and compare theories, and facilitate their integration into empirical research, formal models, and ultimately policy and governance for sustainability. Our theory selection, framework, and mapping offer a foundation—a “living” platform—upon which future collaborative efforts can build to create a resource for scholars and practitioners working at the intersection of social sciences and natural resource management.
Sustainability Scien... arrow_drop_down add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/s11625-021-00989-w&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess Routeshybrid 30 citations 30 popularity Top 10% influence Average impulse Top 10% Powered by BIP!more_vert Sustainability Scien... arrow_drop_down add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/s11625-021-00989-w&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type , Preprint 2021 Netherlands, United Kingdom, Norway, Brazil, Norway, France, FrancePublisher:Copernicus GmbH Funded by:NSERC, UKRI | SWEET:Super-Warm Early Eo..., EC | PLIO-ESS +5 projectsNSERC ,UKRI| SWEET:Super-Warm Early Eocene Temperatures and climate: understanding the response of the Earth to high CO2 through integrated modelling and data ,EC| PLIO-ESS ,NSF| The Management and Operation of the National Center for Atmoshperic Research (NCAR) ,NSF| Collaborative Research: Paleoclimate perspective on the response of Southwest North American rainfall to elevated greenhouse gases ,NWO| Perturbations of System Earth: Reading the Past to Project the Future - A proposal to create the Netherlands Earth System Science Centre (ESSC) ,NWO| Mechanisms of major climate system reorganisations in the Cenozoic ,NSF| Collaborative Research: Arctic Temperature Amplification during the Middle Pliocene (ArcAMP): Assessing the interaction among feedback mechanismsSathyanadh, Anusha; Monteil, Guillaume; Scholze, Marko; Klosterhalfen, Anne; Laudon, Hjalmar; Wu, Zhendong; Gerbig, Christoph; Peters, Wouter; Bastrikov, Vladislav; Nilsson, Mats, B; Peichl, Matthias; Oldeman, Arthur, M; Baatsen, Michiel, L J; von Der Heydt, Anna, S; Dijkstra, Henk, A; Tindall, Julia, C; Abe-Ouchi, Ayako; Booth, Alice, R; Brady, Esther, C; Chan, Wing-Le; Chandan, Deepak; Chandler, Mark, A; Contoux, Camille; Feng, Ran; Guo, Chuncheng; Haywood, Alan, M; Hunter, Stephen, J; Kamae, Youichi; Li, Qiang; Li, Xiangyu; Lohmann, Gerrit; Lunt, Daniel, J; Nisancioglu, Kerim, H; Otto-Bliesner, Bette, L; Peltier, W, Richard; Pontes, Gabriel, M; Ramstein, Gilles; Sohl, Linda, E; Stepanek, Christian; Tan, Ning; Zhang, Qiong; Zhang, Zhongshi; Wainer, Ilana; Williams, Charles, J R;The mid-Pliocene warm period (3.264–3.025 Ma) is the most recent geological period during which atmospheric CO2 levels were similar to recent historical values (∼400 ppm). Several proxy reconstructions for the mid-Pliocene show highly reduced zonal sea surface temperature (SST) gradients in the tropical Pacific Ocean, indicating an El Niño-like mean state. However, past modelling studies do not show these highly reduced gradients. Efforts to understand mid-Pliocene climate dynamics have led to the Pliocene Model Intercomparison Project (PlioMIP). Results from the first phase (PlioMIP1) showed clear El Niño variability (albeit significantly reduced) and did not show the greatly reduced time-mean zonal SST gradient suggested by some of the proxies. In this work, we study El Niño–Southern Oscillation (ENSO) variability in the PlioMIP2 ensemble, which consists of additional global coupled climate models and updated boundary conditions compared to PlioMIP1. We quantify ENSO amplitude, period, spatial structure and “flavour”, as well as the tropical Pacific annual mean state in mid-Pliocene and pre-industrial simulations. Results show a reduced ENSO amplitude in the model-ensemble mean (−24 %) with respect to the pre-industrial, with 15 out of 17 individual models showing such a reduction. Furthermore, the spectral power of this variability considerably decreases in the 3–4-year band. The spatial structure of the dominant empirical orthogonal function shows no particular change in the patterns of tropical Pacific variability in the model-ensemble mean, compared to the pre-industrial. Although the time-mean zonal SST gradient in the equatorial Pacific decreases for 14 out of 17 models (0.2 ∘C reduction in the ensemble mean), there does not seem to be a correlation with the decrease in ENSO amplitude. The models showing the most “El Niño-like” mean state changes show a similar ENSO amplitude to that in the pre-industrial reference, while models showing more “La Niña-like” mean state changes generally show a large reduction in ENSO variability. The PlioMIP2 results show a reasonable agreement with both time-mean proxies indicating a reduced zonal SST gradient and reconstructions indicating a reduced, or similar, ENSO variability. International audience
CORE (RIOXX-UK Aggre... arrow_drop_down Copernicus Publications; Climate of the Past (CP)Other literature type . 2021Data sources: Copernicus Publicationshttps://doi.org/10.5194/cp-202...Preprint . 2021 . Peer-reviewedLicense: CC BYData sources: CrossrefNORCE Research Archive; Norwegian Open Research ArchivesArticle . 2021 . Peer-reviewedBergen Open Research Archive - UiB; Norwegian Open Research ArchivesArticle . 2021 . Peer-reviewedLicense: CC BYMémoires en Sciences de l'Information et de la Communication; HAL-CEAArticle . 2021License: CC BYFull-Text: https://hal.science/hal-03469874/documentMémoires en Sciences de l'Information et de la Communication; HAL-CEAArticle . 2021License: CC BYFull-Text: https://hal.science/hal-03495127/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.5194/cp-2021-58&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 9 citations 9 popularity Top 10% influence Average impulse Top 10% Powered by BIP!visibility 4visibility views 4 download downloads 1 Powered bymore_vert CORE (RIOXX-UK Aggre... arrow_drop_down Copernicus Publications; Climate of the Past (CP)Other literature type . 2021Data sources: Copernicus Publicationshttps://doi.org/10.5194/cp-202...Preprint . 2021 . Peer-reviewedLicense: CC BYData sources: CrossrefNORCE Research Archive; Norwegian Open Research ArchivesArticle . 2021 . Peer-reviewedBergen Open Research Archive - UiB; Norwegian Open Research ArchivesArticle . 2021 . Peer-reviewedLicense: CC BYMémoires en Sciences de l'Information et de la Communication; HAL-CEAArticle . 2021License: CC BYFull-Text: https://hal.science/hal-03469874/documentMémoires en Sciences de l'Information et de la Communication; HAL-CEAArticle . 2021License: CC BYFull-Text: https://hal.science/hal-03495127/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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