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pro vyhledávání: '"Bagniewski, Witold"'
The Earth's climate has experienced numerous critical transitions during its history, which have often been accompanied by massive and rapid changes in the biosphere. Such transitions are evidenced in various proxy records covering different timescal
Externí odkaz:
http://arxiv.org/abs/2212.06239
Tipping points (TPs) in the Earth system have been studied with growing interest and concern in recent years due to the potential risk of anthropogenic forcing causing abrupt, and possibly irreversible, climate transitions. Paleoclimate records are e
Externí odkaz:
http://arxiv.org/abs/2206.06832
Publikováno v:
In Global and Planetary Change August 2023 227
Autor:
Rousseau, Denis-Didier1,2,3 (AUTHOR) denis-didier.rousseau@umontpellier.fr, Bagniewski, Witold4 (AUTHOR), Cheng, Hai5 (AUTHOR)
Publikováno v:
Scientific Reports. 12/21/2023, Vol. 13 Issue 1, p1-15. 15p.
Autor:
Rousseau, Denis-Didier1,2,3 (AUTHOR) denis-didier.rousseau@umontpellier.fr, Bagniewski, Witold4 (AUTHOR), Lucarini, Valerio5,6,7 (AUTHOR)
Publikováno v:
Scientific Reports. 7/12/2023, Vol. 13 Issue 1, p1-13. 13p.
Autor:
Bagniewski, Witold1 (AUTHOR) wbagniewski@lmd.ipsl.fr, Rousseau, Denis-Didier2,3,4 (AUTHOR), Ghil, Michael1,5 (AUTHOR)
Publikováno v:
Scientific Reports. 3/18/2023, Vol. 13 Issue 1, p1-18. 18p.
Akademický článek
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The past 3.2 Myr have seen drastic climate changes with the development, waxing and waning of huge continental ice sheets over the Northern Hemisphere. These striking phenomena have been observed in various records from ice cores, as well as marine a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::73dff0d682e00b7a066ebf5457356908
https://hal-insu.archives-ouvertes.fr/insu-03299662
https://hal-insu.archives-ouvertes.fr/insu-03299662
Publikováno v:
Climate of the Past Discussions; 8/11/2021, p1-35, 35p
Autor:
Bagniewski, Witold
Oxygen isotope (δ18O) records from sediment cores, ice cores, and speleothems are a key proxy for reconstructing past climate. Since they are subject to changes in land ice, sea ice, ocean circulation, precipitation, evaporation, river discharge, an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a62d804b4fc5a947f96305d018bee629