globalchange  > 气候变化事实与影响
DOI: 10.1175/JCLI-D-12-00520.1
Scopus记录号: 2-s2.0-84888055716
论文题名:
The climate of the MIS-13 interglacial according to HadCM3
作者: Muri H.; Berger A.; Yin Q.; Karami M.P.; Barriat P.-Y.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2013
卷: 26, 期:23
起始页码: 9696
结束页码: 9712
语种: 英语
Scopus关键词: East Asian summer monsoon ; Ice sheet ; Insolation forcing ; Marine isotopic stages ; Monsoons ; Paleoclimates ; Sea surface temperature (SST) ; Teleconnections ; Atmospheric pressure ; Atmospheric thermodynamics ; Climate change ; Incident solar radiation ; Climate models ; atmosphere-ocean coupling ; climate modeling ; general circulation model ; geological record ; high pressure ; ice sheet ; interglacial ; marine isotope stage ; monsoon ; paleoclimate ; sea surface temperature ; teleconnection ; Asia ; Atlantic Ocean ; Atlantic Ocean (North) ; Eurasia ; North America ; Pacific Ocean ; Pacific Ocean (Tropical) ; Sea of Japan
英文摘要: The climate of the Marine Isotopic Stage 13 (MIS-13) is explored in the fully coupled atmosphere-ocean general circulation model the Hadley Centre Coupled Model, version 3 (HadCM3). It is found that the strong insolation forcing at the time imposed a strengthened land-ocean thermal contrast, resulting in an intensified summer monsoon over Asia. The addition of land ice over North America and Eurasia results in a stationary wave feature across the Eurasian continent. This leads to a high pressure anomaly over the Sea of Japan with increased advection of warm moist air onto the Chinese landmasses. This in turn reinforces the East Asian summer monsoon (EASM), highlighting the counterintuitive notion that, depending on the background insolation and its size, ice can indeed contribute to strengthening the EASM. The modeling results support the geological record indication of a strong EASM 500 000 years ago. Furthermore, Arctic Oscillation, El Niño-Southern Oscillation, and Indian Ocean dipole-like teleconnection features are discussed in the MIS-13 environment. It is shown that the change in the tropical Pacific sea surface temperature has the potential to impact the North Atlantic climate through an atmospheric "bridge". © 2013 American Meteorological Society.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/51482
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作者单位: Earth and Life Institute, Georges Lemaître Centre for Earth and Climate Research, Université Catholique de Louvain, Louvain-la-Neuve, Belgium; Department of Geosciences, Meteorology and Oceanography Section, University of Oslo, Postboks 1022 Blindern, 0315 Oslo, Norway

Recommended Citation:
Muri H.,Berger A.,Yin Q.,et al. The climate of the MIS-13 interglacial according to HadCM3[J]. Journal of Climate,2013-01-01,26(23)
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