Climate Change Data Portal
DOI | 10.1029/2020JD033965 |
Sensitivity of Water Balance in the Qaidam Basin to the Mid-Pliocene Climate | |
Wang X.; Schmidt B.; Otto M.; Ehlers T.A.; Mutz S.G.; Botsyun S.; Scherer D. | |
发表日期 | 2021 |
ISSN | 2169-897X |
卷号 | 126期号:16 |
英文摘要 | The Qaidam Basin (QB) in the northeastern Tibetan Plateau held a megalake system during the Pliocene. Today, the lower elevations in the basin are hyperarid. To understand to what extent the climate plays a role in the maintenance of the megalake system during the Pliocene, we applied the Weather Research and Forecasting model for dynamical downscaling of ECHAM5 global climate simulations for the present day and the mid-Pliocene. When imposing the mid-Pliocene climate on the QB with its modern land surface settings, the annual water balance ((Formula presented.)), that is, the change in terrestrial water storage within the QB, increases. This positive imbalance of (Formula presented.) induced solely by the changes in the large-scale climate state would lead to a readjustment of lake extent, until a new equilibrium state is reached, where loss due to evaporation over lake areas compensates for the input by runoff and precipitation. Atmospheric water transport (AWT) analysis at each border of the QB reveals that this imbalance of (Formula presented.) is caused by stronger moisture influx across the western border in winter, spring, and autumn and weaker moisture out-flux across the eastern border in summer. These changes in AWT are associated with the strengthening of the midlatitude westerlies in all seasons, except for summer, and the intensification of the East Asian Summer Monsoon. Given that the mid-Pliocene climate is an analog to the projected warm climate of the near future, our study contributes to a better understanding of climate change impacts in central Asia. © 2021. The Authors. |
英文关键词 | dynamical downscaling; Pliocene; Qaidam Basin; water balance |
来源期刊 | Journal of Geophysical Research: Atmospheres
![]() |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/237066 |
作者单位 | Chair of Climatology, Technische Universität Berlin, Berlin, Germany; Department of Geosciences, University Tübingen, Tübingen, Germany |
推荐引用方式 GB/T 7714 | Wang X.,Schmidt B.,Otto M.,et al. Sensitivity of Water Balance in the Qaidam Basin to the Mid-Pliocene Climate[J],2021,126(16). |
APA | Wang X..,Schmidt B..,Otto M..,Ehlers T.A..,Mutz S.G..,...&Scherer D..(2021).Sensitivity of Water Balance in the Qaidam Basin to the Mid-Pliocene Climate.Journal of Geophysical Research: Atmospheres,126(16). |
MLA | Wang X.,et al."Sensitivity of Water Balance in the Qaidam Basin to the Mid-Pliocene Climate".Journal of Geophysical Research: Atmospheres 126.16(2021). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。