Arid
DOI10.1134/S0097807817030149
Assessing Possible Changes in Selenga R. Water Regime in the XXI Century Based on a Runoff Formation Model
Moreido, V. M.; Kalugin, A. S.
通讯作者Kalugin, A. S.
来源期刊WATER RESOURCES
ISSN0097-8078
EISSN1608-344X
出版年2017
卷号44期号:3页码:390-398
英文摘要

The runoff of the Selenga R., the largest tributary of Lake Baikal, in recent two decades corresponds to a low-water period. Such decrease can be due to the global climate processes, which have an effect on the amounts of precipitation onto and evaporation from Selenga drainage basin, which is located in arid climate zone. The adaptation of Ecomag software complex to simulating river runoff in the Selenga Basin based on global databases (relief, soils, vegetation, and weather information) is described. The model was calibrated and verified, and the statistical estimates of calculation efficiency were constructed. The obtained model of runoff formation in the Selenga Basin was used to assess the possible changes in the climate and water regime in the XXI century with the use of data of global climate models under different scenarios of greenhouse gas emissions. Throughout the XXI century, the Selenga R. runoff may decrease by 10-40%, depending on the forecasted climate conditions.


英文关键词river runoff runoff formation model Selenga Lake Baikal water regime variations CMIP5
类型Article
语种英语
国家Russia
收录类别SCI-E
WOS记录号WOS:000405126000005
WOS类目Water Resources
WOS研究方向Water Resources
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/202871
作者单位Russian Acad Sci, Water Problems Inst, Moscow 119333, Russia
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GB/T 7714
Moreido, V. M.,Kalugin, A. S.. Assessing Possible Changes in Selenga R. Water Regime in the XXI Century Based on a Runoff Formation Model[J],2017,44(3):390-398.
APA Moreido, V. M.,&Kalugin, A. S..(2017).Assessing Possible Changes in Selenga R. Water Regime in the XXI Century Based on a Runoff Formation Model.WATER RESOURCES,44(3),390-398.
MLA Moreido, V. M.,et al."Assessing Possible Changes in Selenga R. Water Regime in the XXI Century Based on a Runoff Formation Model".WATER RESOURCES 44.3(2017):390-398.
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