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距今40—30ka青藏高原特强夏季风事件及其与岁差周期关系
姚檀栋1; 刘晓东1; 李炳元2; 施雅风1
1999
Source Publication科学通报
ISSN0023-074X
Volume044Issue:014Pages:1475
Abstract古里雅冰芯记录、青藏高原和其北侧的高湖面记录、植被变化记录指示４０－３０ｋａＢＰ即欠冰期间冰阶或深海氧同位素３阶段后期，青藏高原异常的温暖湿润，温度高于现代２－４℃，降水有４成至成倍以上的增长，代表着一次特强的夏季风事件，推测其动力一方面为高原夏季低气压强盛，增大了对夏季风的吸引力；国一方面热带洋面的旺盛蒸发，助长了西南季风携丰富水汽吹越青藏高原，特强夏季风形成背景是４０－３０ｋａＢＰ正值２０ｋａ
Language英语
Document Type期刊论文
Identifierhttp://ir.igsnrr.ac.cn/handle/311030/111245
Collection中国科学院地理科学与资源研究所
Affiliation1.中国科学院寒区旱区环境与工程研究所
2.中国科学院地理科学与资源研究所
Recommended Citation
GB/T 7714		 姚檀栋,刘晓东,李炳元,等. 距今40—30ka青藏高原特强夏季风事件及其与岁差周期关系[J]. 科学通报,1999,044(014):1475.
APA 姚檀栋,刘晓东,李炳元,&施雅风.(1999).距今40—30ka青藏高原特强夏季风事件及其与岁差周期关系.科学通报,044(014),1475.
MLA 姚檀栋,et al."距今40—30ka青藏高原特强夏季风事件及其与岁差周期关系".科学通报 044.014(1999):1475.
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