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- W2481854263 abstract "The last interglacial maximum (125 ka BP) is usually considered the warmest time period of the last 200 ky. This article reviews the climate simulations for this time period focusing on the agreements and discrepancies of the model results with one another and with the evidence from paleoclimatic reconstructions. The northern summer response reflects the direct thermodynamic response to increased insolation, and models of different complexities broadly agree both in the simulated pattern and in magnitude. The agreement is worse in northern winter: while the simpler models generally reflect the thermodynamic direct response to the insolation decrease, comprehensive models show enhanced warming over regions of the northern continents as a result of changes in atmospheric dynamics. Such a warming is consistent with the evidence for warmth from paleoclimatic reconstructions. Yet, it is also reproduced in simple models including a dynamic terrestrial vegetation component as a result of climate–biosphere interactions, and the simulated changes in vegetation are consistent with the fossil data. Thus, the exact interplay of dynamics and biosphere during the last interglacial still needs be clarified. The advent of comprehensive models including dynamic biosphere components will hopefully contribute to this purpose." @default.
- W2481854263 created "2016-08-23" @default.
- W2481854263 creator A5080968415 @default.
- W2481854263 date "2014-01-01" @default.
- W2481854263 modified "2023-09-25" @default.
- W2481854263 title "Paleoclimate Modeling of the Last Interglacial☆" @default.
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- W2481854263 doi "https://doi.org/10.1016/b978-0-12-409548-9.09412-4" @default.
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