Modeling a strong East Asian summer monsoon in a globally cool Earth, the MIS-13 case
International audience Deep-sea and ice-core records show a significant reduced amplitude of the ice volume, temperature and greenhouse gases variations before Marine Isotope Stage (MIS) 11, about 400 000 years ago, with less warm (more glaciated) interglacials and less cold glacials. At the same ti...
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ftinsu:oai:HAL:hal-00298203v1 2023-11-12T04:18:37+01:00 Modeling a strong East Asian summer monsoon in a globally cool Earth, the MIS-13 case Yin, Q. Z. Berger, A. Driesschaert, E. Goosse, H. Loutre, M. F. Crucifix, M. Institut d'Astronomie et de Géophysique Georges Lemaître (UCL-ASTR) Université Catholique de Louvain = Catholic University of Louvain (UCL) 2007-11-26 https://hal.science/hal-00298203 https://hal.science/hal-00298203/document https://hal.science/hal-00298203/file/cpd-3-1261-2007.pdf en eng HAL CCSD European Geosciences Union (EGU) hal-00298203 https://hal.science/hal-00298203 https://hal.science/hal-00298203/document https://hal.science/hal-00298203/file/cpd-3-1261-2007.pdf info:eu-repo/semantics/OpenAccess ISSN: 1814-9340 EISSN: 1814-9359 Climate of the Past Discussions https://hal.science/hal-00298203 Climate of the Past Discussions, 2007, 3 (6), pp.1261-1282 [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 2007 ftinsu 2023-10-25T16:28:11Z International audience Deep-sea and ice-core records show a significant reduced amplitude of the ice volume, temperature and greenhouse gases variations before Marine Isotope Stage (MIS) 11, about 400 000 years ago, with less warm (more glaciated) interglacials and less cold glacials. At the same time, the loess in northern China, the sedimentary core in the eastern Tibetan Plateau and the palaeosols in southern China all record an unusually warm and wet climate during MIS-13 (about 500 000 years ago), indicating an extremely strong East Asian summer monsoon. To understand this seeming paradox of a strong East Asian summer monsoon occurring during the cool MIS-13, a three-dimension Earth system Model of Intermediate complexity is used. Modeling results show that this very strong MIS-13 East Asian summer monsoon, identified from the precipitation, horizontal and vertical (omega) wind, and pressure (geopotential) fields, results from the astronomical and ice sheet forcings. North Hemisphere summer at perihelion both at 529 and 506 ka BP leads to an East Asian summer monsoon stronger than during the Pre-Industrial time. In addition, the ice sheets reinforce the East Asian summer monsoon through the propagation of a perturbation wave which is induced mainly by the Eurasian ice sheet and is influenced by the Tibetan Plateau. Article in Journal/Newspaper ice core Ice Sheet Institut national des sciences de l'Univers: HAL-INSU |
institution |
Open Polar |
collection |
Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
spellingShingle |
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences Yin, Q. Z. Berger, A. Driesschaert, E. Goosse, H. Loutre, M. F. Crucifix, M. Modeling a strong East Asian summer monsoon in a globally cool Earth, the MIS-13 case |
topic_facet |
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
description |
International audience Deep-sea and ice-core records show a significant reduced amplitude of the ice volume, temperature and greenhouse gases variations before Marine Isotope Stage (MIS) 11, about 400 000 years ago, with less warm (more glaciated) interglacials and less cold glacials. At the same time, the loess in northern China, the sedimentary core in the eastern Tibetan Plateau and the palaeosols in southern China all record an unusually warm and wet climate during MIS-13 (about 500 000 years ago), indicating an extremely strong East Asian summer monsoon. To understand this seeming paradox of a strong East Asian summer monsoon occurring during the cool MIS-13, a three-dimension Earth system Model of Intermediate complexity is used. Modeling results show that this very strong MIS-13 East Asian summer monsoon, identified from the precipitation, horizontal and vertical (omega) wind, and pressure (geopotential) fields, results from the astronomical and ice sheet forcings. North Hemisphere summer at perihelion both at 529 and 506 ka BP leads to an East Asian summer monsoon stronger than during the Pre-Industrial time. In addition, the ice sheets reinforce the East Asian summer monsoon through the propagation of a perturbation wave which is induced mainly by the Eurasian ice sheet and is influenced by the Tibetan Plateau. |
author2 |
Institut d'Astronomie et de Géophysique Georges Lemaître (UCL-ASTR) Université Catholique de Louvain = Catholic University of Louvain (UCL) |
format |
Article in Journal/Newspaper |
author |
Yin, Q. Z. Berger, A. Driesschaert, E. Goosse, H. Loutre, M. F. Crucifix, M. |
author_facet |
Yin, Q. Z. Berger, A. Driesschaert, E. Goosse, H. Loutre, M. F. Crucifix, M. |
author_sort |
Yin, Q. Z. |
title |
Modeling a strong East Asian summer monsoon in a globally cool Earth, the MIS-13 case |
title_short |
Modeling a strong East Asian summer monsoon in a globally cool Earth, the MIS-13 case |
title_full |
Modeling a strong East Asian summer monsoon in a globally cool Earth, the MIS-13 case |
title_fullStr |
Modeling a strong East Asian summer monsoon in a globally cool Earth, the MIS-13 case |
title_full_unstemmed |
Modeling a strong East Asian summer monsoon in a globally cool Earth, the MIS-13 case |
title_sort |
modeling a strong east asian summer monsoon in a globally cool earth, the mis-13 case |
publisher |
HAL CCSD |
publishDate |
2007 |
url |
https://hal.science/hal-00298203 https://hal.science/hal-00298203/document https://hal.science/hal-00298203/file/cpd-3-1261-2007.pdf |
genre |
ice core Ice Sheet |
genre_facet |
ice core Ice Sheet |
op_source |
ISSN: 1814-9340 EISSN: 1814-9359 Climate of the Past Discussions https://hal.science/hal-00298203 Climate of the Past Discussions, 2007, 3 (6), pp.1261-1282 |
op_relation |
hal-00298203 https://hal.science/hal-00298203 https://hal.science/hal-00298203/document https://hal.science/hal-00298203/file/cpd-3-1261-2007.pdf |
op_rights |
info:eu-repo/semantics/OpenAccess |
_version_ |
1782335226745192448 |