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Insolation change is a primary driver for climate variation at orbital scales [1,2].During the Holocene (ca.11.7 ka BP to present),orbitally induced seasonal variations in insolation varied markedly,with a long-term decrease in boreal summer (hereafter summer)and increase in boreal winter (hereafter winter) [2].This offers an opportunity to investigate the climate system's response to insolation forcing.However,previous studies that focused on Holo-cene temperature reconstructions and simulations [3-5] have raised the question of how temperature responds to insolation changes.
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篇名 Model-data divergence in global seasonal temperature response to astronomical insolation during the Holocene
来源期刊 科学通报(英文版) 学科
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年,卷(期) 2022,(1) 所属期刊栏目 Earth Sciences
研究方向 页码范围 25-28
页数 4页 分类号
字数 语种 英文
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科学通报(英文版)
半月刊
1001-6538
11-1785/N
大16开
北京东黄城根北街16号
2-177
1950
eng
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