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      Improved modeling of snow and glacier melting by a progressive two-stage calibration strategy with GRACE and multisource data: How snow and glacier meltwater contributes to the runoff of the Upper Brahmaputra River basin? : A TWO-STAGE MODEL CALIBRATION STRATEGY

      1 , 1 , 1 , 1 , 2
      Water Resources Research
      Wiley

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          Potential impacts of a warming climate on water availability in snow-dominated regions.

          All currently available climate models predict a near-surface warming trend under the influence of rising levels of greenhouse gases in the atmosphere. In addition to the direct effects on climate--for example, on the frequency of heatwaves--this increase in surface temperatures has important consequences for the hydrological cycle, particularly in regions where water supply is currently dominated by melting snow or ice. In a warmer world, less winter precipitation falls as snow and the melting of winter snow occurs earlier in spring. Even without any changes in precipitation intensity, both of these effects lead to a shift in peak river runoff to winter and early spring, away from summer and autumn when demand is highest. Where storage capacities are not sufficient, much of the winter runoff will immediately be lost to the oceans. With more than one-sixth of the Earth's population relying on glaciers and seasonal snow packs for their water supply, the consequences of these hydrological changes for future water availability--predicted with high confidence and already diagnosed in some regions--are likely to be severe.
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            GRACE measurements of mass variability in the Earth system.

            Monthly gravity field estimates made by the twin Gravity Recovery and Climate Experiment (GRACE) satellites have a geoid height accuracy of 2 to 3 millimeters at a spatial resolution as small as 400 kilometers. The annual cycle in the geoid variations, up to 10 millimeters in some regions, peaked predominantly in the spring and fall seasons. Geoid variations observed over South America that can be largely attributed to surface water and groundwater changes show a clear separation between the large Amazon watershed and the smaller watersheds to the north. Such observations will help hydrologists to connect processes at traditional length scales (tens of kilometers or less) to those at regional and global scales.
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              Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings

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                Author and article information

                Journal
                Water Resources Research
                Water Resour. Res.
                Wiley
                00431397
                March 2017
                March 2017
                March 28 2017
                : 53
                : 3
                : 2431-2466
                Affiliations
                [1 ]State Key Laboratory of Hydroscience and Engineering, Department of Hydraulic Engineering; Tsinghua University; Beijing China
                [2 ]Department of Water Resources; China Institute of Water Resources and Hydropower Research; Beijing China
                Article
                10.1002/2016WR019656
                23fef8b3-f330-4c6d-856f-d7f8417c5112
                © 2017

                http://doi.wiley.com/10.1002/tdm_license_1

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