Impact of the hydrological cycle on past climate changes: three illustrations at different time scales
International audience We investigate in the paper the impact of the hydrologic cycle on climate at different periods. The aim is to illustrate how the changes in moisture transport, precipitation pattern, and weathering may alter, at regional or global scales, the CO 2 and climate equilibriums. We...
Published in: | Comptes Rendus Geoscience |
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Main Authors: | , , , , |
Other Authors: | , , , , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2005
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Subjects: | |
Online Access: | https://hal.science/hal-03013570 https://hal.science/hal-03013570/document https://hal.science/hal-03013570/file/1-s2.0-S1631071304003062-main.pdf https://doi.org/10.1016/j.crte.2004.10.016 |
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Open Polar |
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Université de Paris: Portail HAL |
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English |
topic |
Climate Glaciation Monsoon General circulation Climat Mousson Circulation générale [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
spellingShingle |
Climate Glaciation Monsoon General circulation Climat Mousson Circulation générale [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment Ramstein, Gilles Khodri, Myriam Donnadieu, Yannick Fluteau, Frédéric Goddéris, Yves Impact of the hydrological cycle on past climate changes: three illustrations at different time scales |
topic_facet |
Climate Glaciation Monsoon General circulation Climat Mousson Circulation générale [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
description |
International audience We investigate in the paper the impact of the hydrologic cycle on climate at different periods. The aim is to illustrate how the changes in moisture transport, precipitation pattern, and weathering may alter, at regional or global scales, the CO 2 and climate equilibriums. We choose three climate periods to pinpoint intricate relationships between water cycle and climate. The illustrations are the following. (i) The onset of ice-sheet build-up, 115 kyr BP. We show that the increased thermal meridian gradient of SST allows large moisture advection over the North American continent and provides appropriate conditions for perennial snow on the Canadian Archipelago. (ii) The onset of Indian Monsoon at the end of the Tertiary. We demonstrate that superimposed to the Tibetan Plateau, the shrinkage of the Tethys, since Oligocene, plays a major role to explain changes in the geographical pattern of the southeastern Asian Monsoon. (iii) The onset of Global Glaciation (750 Ma). We show that the break-up of Rodinia occurring at low latitudes is an important feature to explain how the important precipitation increase leads to weathering and carbon burial, which contribute to decrease atmospheric CO 2 enough to produce a snows ball Earth. All these periods have been simulated with a hierarchy of models appropriate to quantify the water cycle impact on climate. |
author2 |
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Modélisation du climat (CLIM) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Lamont-Doherty Earth Observatory (LDEO) Columbia University New York Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL) Institut de Physique du Globe de Paris (IPGP (UMR_7154)) Institut national des sciences de l'Univers (INSU - CNRS)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité) Laboratoire des Mécanismes et Transfert en Géologie (LMTG) Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Ramstein, Gilles Khodri, Myriam Donnadieu, Yannick Fluteau, Frédéric Goddéris, Yves |
author_facet |
Ramstein, Gilles Khodri, Myriam Donnadieu, Yannick Fluteau, Frédéric Goddéris, Yves |
author_sort |
Ramstein, Gilles |
title |
Impact of the hydrological cycle on past climate changes: three illustrations at different time scales |
title_short |
Impact of the hydrological cycle on past climate changes: three illustrations at different time scales |
title_full |
Impact of the hydrological cycle on past climate changes: three illustrations at different time scales |
title_fullStr |
Impact of the hydrological cycle on past climate changes: three illustrations at different time scales |
title_full_unstemmed |
Impact of the hydrological cycle on past climate changes: three illustrations at different time scales |
title_sort |
impact of the hydrological cycle on past climate changes: three illustrations at different time scales |
publisher |
HAL CCSD |
publishDate |
2005 |
url |
https://hal.science/hal-03013570 https://hal.science/hal-03013570/document https://hal.science/hal-03013570/file/1-s2.0-S1631071304003062-main.pdf https://doi.org/10.1016/j.crte.2004.10.016 |
genre |
Canadian Archipelago Ice Sheet |
genre_facet |
Canadian Archipelago Ice Sheet |
op_source |
Comptes Rendus Géoscience https://hal.science/hal-03013570 Comptes Rendus Géoscience, 2005, 337 (1-2), pp.125-137. ⟨10.1016/j.crte.2004.10.016⟩ |
op_relation |
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op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1016/j.crte.2004.10.016 |
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Comptes Rendus Geoscience |
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337 |
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1-2 |
container_start_page |
125 |
op_container_end_page |
137 |
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1799478076589998080 |
spelling |
ftunivparis:oai:HAL:hal-03013570v1 2024-05-19T07:38:37+00:00 Impact of the hydrological cycle on past climate changes: three illustrations at different time scales Ramstein, Gilles Khodri, Myriam Donnadieu, Yannick Fluteau, Frédéric Goddéris, Yves Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Modélisation du climat (CLIM) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Lamont-Doherty Earth Observatory (LDEO) Columbia University New York Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL) Institut de Physique du Globe de Paris (IPGP (UMR_7154)) Institut national des sciences de l'Univers (INSU - CNRS)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité) Laboratoire des Mécanismes et Transfert en Géologie (LMTG) Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) 2005-01 https://hal.science/hal-03013570 https://hal.science/hal-03013570/document https://hal.science/hal-03013570/file/1-s2.0-S1631071304003062-main.pdf https://doi.org/10.1016/j.crte.2004.10.016 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.crte.2004.10.016 hal-03013570 https://hal.science/hal-03013570 https://hal.science/hal-03013570/document https://hal.science/hal-03013570/file/1-s2.0-S1631071304003062-main.pdf doi:10.1016/j.crte.2004.10.016 info:eu-repo/semantics/OpenAccess Comptes Rendus Géoscience https://hal.science/hal-03013570 Comptes Rendus Géoscience, 2005, 337 (1-2), pp.125-137. ⟨10.1016/j.crte.2004.10.016⟩ Climate Glaciation Monsoon General circulation Climat Mousson Circulation générale [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2005 ftunivparis https://doi.org/10.1016/j.crte.2004.10.016 2024-04-23T03:41:14Z International audience We investigate in the paper the impact of the hydrologic cycle on climate at different periods. The aim is to illustrate how the changes in moisture transport, precipitation pattern, and weathering may alter, at regional or global scales, the CO 2 and climate equilibriums. We choose three climate periods to pinpoint intricate relationships between water cycle and climate. The illustrations are the following. (i) The onset of ice-sheet build-up, 115 kyr BP. We show that the increased thermal meridian gradient of SST allows large moisture advection over the North American continent and provides appropriate conditions for perennial snow on the Canadian Archipelago. (ii) The onset of Indian Monsoon at the end of the Tertiary. We demonstrate that superimposed to the Tibetan Plateau, the shrinkage of the Tethys, since Oligocene, plays a major role to explain changes in the geographical pattern of the southeastern Asian Monsoon. (iii) The onset of Global Glaciation (750 Ma). We show that the break-up of Rodinia occurring at low latitudes is an important feature to explain how the important precipitation increase leads to weathering and carbon burial, which contribute to decrease atmospheric CO 2 enough to produce a snows ball Earth. All these periods have been simulated with a hierarchy of models appropriate to quantify the water cycle impact on climate. Article in Journal/Newspaper Canadian Archipelago Ice Sheet Université de Paris: Portail HAL Comptes Rendus Geoscience 337 1-2 125 137 |