Survival of the Qaidam mega-lake system under mid-Pliocene climates and itsrestoration under future climates

GSTDTAP > 资源环境科学

DOI	10.5194/hess-24-3835-2020
	Survival of the Qaidam mega-lake system under mid-Pliocene climates and itsrestoration under future climates
	admin
	2020-08-11
出版年	2020
国家	欧洲
领域	气候变化 ; 资源环境
英文摘要	During the Pliocene, the Qaidam Basin on the Tibetan Plateau contained a mega-lake system. During the Pleistocene, it disappeared almost completely. Today, hyperarid climates prevail in the low-altitude parts of the basin. This study reveals that today’s mean water balance of the Qaidam Basin is nearly zero and is positive during warmer, less dry years. The results explain how the mega-lake system could survive for a long time in the past and could eventually be restored in the future.
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来源平台	European Geosciences Union
引用统计
文献类型	科技报告
条目标识符	http://119.78.100.173/C666/handle/2XK7JSWQ/288110
专题	资源环境科学气候变化
推荐引用方式 GB/T 7714	admin. Survival of the Qaidam mega-lake system under mid-Pliocene climates and itsrestoration under future climates,2020.