Simulation of modern and glacial climates with a coupled global model of intermediate complexity

被引：313

作者：

Ganopolski, A ^{[1
]}

Rahmstorf, S ^{[1
]}

Petoukhov, V ^{[1
]}

Claussen, M ^{[1
]}

机构：

[1] Potsdam Inst Climate Impact Res, D-14412 Potsdam, Germany

来源：

NATURE | 1998年 / 391卷 / 6665期

关键词：

D O I：

10.1038/34839

中图分类号：

O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];

学科分类号：

07 ; 0710 ; 09 ;

摘要：

A global coupled ocean-atmosphere model of intermediate complexity is used to simulate the equilibrium climate of both today and the Last Glacial Maximum, around 21,000 years ago. The model successfully predicts the atmospheric and oceanic circulations, temperature distribution, hydrological cycle and sea-ice covet of both periods without using 'flux adjustments'. Changes in oceanic circulation, particularly in the Atlantic Ocean, play an important role in glacial cooling.

引用

页码：351 / 356

页数：6

共 51 条

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