干旱区生态环境知识资源中心(Arid): Evolution of lake water volume in global closed basins since the Last Glacial Maximum and its implication for future projection

Arid

DOI	10.1177/03091333221079776
	Evolution of lake water volume in global closed basins since the Last Glacial Maximum and its implication for future projection
	Zhang, Yuxin; Li, Yu
通讯作者	Li, Y
来源期刊	PROGRESS IN PHYSICAL GEOGRAPHY-EARTH AND ENVIRONMENT
ISSN	0309-1333
EISSN	1477-0296
出版年	2022
卷号	46 期号:4 页码:613-629
英文摘要	Mostly concurring with arid and semi-arid regions, closed basins are faced with water scarcity, prominent imbalance between water resource supply and demand, and ecological degradation. Spatial-temporal patterns of water resource change in closed basins have received increasing attention in recent years, but it is still unclear whether there is a connection between the present patterns and those under the millennial-scale natural state. According to lake records, lake models and paleoclimate simulations, we provided a preliminary impression of water volume changes in the long history of different closed basins, which clarified the linkages and differences between the past and present water volume changes. We also evaluated possible water volume changes in the near future. We found that there has been a declining trend of water volume in closed basins of mid-latitude since the Last Glacial Maximum in general, whereas there has been a rising trend of water volume in closed basins of low-latitude over the same period. Over the last few decades, the declining trend of water storage in Western North America, Sahara and Arabia and Central Eurasia possibly has inherited the decreased water volume conditions across the millennial-scale under the natural state, while the increasing water storage in Great Rift Valley and Southern Africa and the decreasing water storage in Dry Andes and Patagonia may be temporary. The assessment of near future water volume changes from a paleoclimatological perspective indicates that the water volume in parts of Western North America, northern Dry Andes, northern Sahara, and southwestern Central Eurasia will continue to decline, while in parts of southern Sahara, southern Great Rift Valley, southeastern Central Eurasia, and eastern Australia it will continue to rise.
英文关键词	Closed basins water volume lake models paleoclimate simulations last glacial maximum
类型	Article
语种	英语
收录类别	SCI-E
WOS记录号	WOS:000778095600001
WOS关键词	WESTERN NORTH-AMERICA ; CLIMATE-CHANGE ; MOISTURE EVOLUTION ; LATE PLEISTOCENE ; LEVEL VARIATIONS ; SEDIMENT CORES ; YOUNGER DRYAS ; DIATOM RECORD ; CENTRAL-ASIA ; CARBON SINK
WOS类目	Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向	Physical Geography ; Geology
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/394083
推荐引用方式 GB/T 7714	Zhang, Yuxin,Li, Yu. Evolution of lake water volume in global closed basins since the Last Glacial Maximum and its implication for future projection[J],2022,46(4):613-629.
APA	Zhang, Yuxin,&Li, Yu.(2022).Evolution of lake water volume in global closed basins since the Last Glacial Maximum and its implication for future projection.PROGRESS IN PHYSICAL GEOGRAPHY-EARTH AND ENVIRONMENT,46(4),613-629.
MLA	Zhang, Yuxin,et al."Evolution of lake water volume in global closed basins since the Last Glacial Maximum and its implication for future projection".PROGRESS IN PHYSICAL GEOGRAPHY-EARTH AND ENVIRONMENT 46.4(2022):613-629.