New methods designed to estimate the daily discharges of rivers in the Tibetan Plateau

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dc.contributor.author Wang, Lei
dc.contributor.author Sichangi, Arthur W.
dc.contributor.author Zeng, Tian
dc.contributor.author Li, Xiuping
dc.contributor.author Hu, Zhidan
dc.contributor.author Genanu, Mulugeta
dc.date.accessioned 2019-06-11T09:11:00Z
dc.date.available 2019-06-11T09:11:00Z
dc.date.issued 2019-05
dc.identifier.citation https://doi.org/10.1016/j.scib.2019.03.015 en_US
dc.identifier.uri http://41.89.227.156:8080/xmlui/handle/123456789/888
dc.description.abstract River discharge is a significant hydrological variable, as it represents the basin-scale integrated output of the hydrological cycle. At present, river discharge observations are usually measured at groundbased gauges across rivers worldwide. In some areas, however, measurements used in the practice of flood prediction and disaster prevention are either fully inaccessible or difficult to obtain in a timely and functional fashion [1]. It has also been reported that the scarcity of global river discharge observations may have undermined the efforts to calculate a globally meaningful estimate of the adjusted biodiversity threat [2]. The Tibetan Plateau (TP), also known as the “Asian Water Tower,” is the headwater of more than 10 large rivers that provide water for billions of people and numerous ecosystems (Fig. 1). The TP has an average elevation greater than 4000 m and an approximate area of 2.5 × 106 km2 . It is largely covered by cryospheric components (glaciers, snow, and frozen soil), and is highly sensitive to climate change [3,4]. Due to the TP’s rapid warming in recent decades, prominent glacial recession, snowmelt, and permafrost degradation have occurred, resulting in water cycle modifications, as well as variations in streamflow both over the plateau and in its downstream regions [5]. en_US
dc.language.iso en en_US
dc.publisher Science Bulletin en_US
dc.subject hydrological variable en_US
dc.title New methods designed to estimate the daily discharges of rivers in the Tibetan Plateau en_US
dc.type Article en_US


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