The Eurasian ice sheet reinforces the East Asian summer monsoon during the interglacial 500 000 years ago
Deep-sea and ice-core records show that interglacial periods were overall less "warm" before about 420 000 years ago than after, with relatively higher ice volume and lower greenhouse gases concentration. This is particularly the case for the interglacial Marine Isotope Stage 13 wh...
Main Authors: | Qiuzhen Yin, A. Berger, E. Driesschaert, H. Goosse, M. F. Loutre, M. Crucifix |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2008-05-01
|
Series: | Climate of the Past |
Online Access: | http://www.clim-past.net/4/79/2008/cp-4-79-2008.pdf |
Similar Items
-
Information on the early Holocene climate constrains the summer sea ice projections for the 21st century
by: H. Goosse, et al.
Published: (2007-12-01) -
Impact of ice sheet meltwater fluxes on the climate evolution at the onset
of the Last Interglacial
by: H. Goelzer, et al.
Published: (2016-08-01) -
Modelling the evolution of the Antarctic ice sheet since the last interglacial
by: M. N. A. Maris, et al.
Published: (2014-07-01) -
Relative impact of insolation and the Indo-Pacific warm pool surface temperature on the East Asia summer monsoon during the MIS-13 interglacial
by: Q. Z. Yin, et al.
Published: (2014-09-01) -
Last Interglacial climate and sea-level evolution from a coupled ice sheet–climate model
by: H. Goelzer, et al.
Published: (2016-12-01)