末次冰期冰盛期
Last Glacial Maximum
查看参考文献22篇
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文摘
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末次冰期冰盛期(LGM)是十分关键的气候时期,这是距我们最近的极寒冷时期,那时北美北部为一巨大冰盖,包括3部分:一个在北美北部的东南,是北美冰盖的主体,称为劳仑泰冰盖;一个在北美北部的西南方太平洋沿岸,范围较小,称为考尔的勒冰盖;另一个在北美东北部靠近北冰洋,称为因纽特冰盖,范围最小。LGM时全球陆地约有24%被冰覆盖而现代仅有11%。由于大量的水形成陆冰,海平面可能比现代低130 m,南极温度比现代低10～12℃,格陵兰可能低20℃。因此,研究LGM对认识气候变化有重要意义。[取自正文] |
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来源
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气候变化研究进展
,2011,7(5):381-382 【扩展库】
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关键词
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冰期
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LGM
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北美东北部
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地址
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1.
北京大学物理学院大气与海洋科学系, 中国气象局气候研究开放实验室, 北京, 100871
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北京大学物理学院大气与海洋科学系, 北京, 100871
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语种
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中文 |
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文献类型
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研究性论文 |
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ISSN
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1673-1719 |
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学科
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大气科学(气象学) |
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文献收藏号
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CSCD:4310623
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