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The Role of Glaciers in the Hydrologic Regime of the Amu Darya and Syr Darya Basins
作者:
Alford, Donald
来源地址:
http://hdl.handle.net/10986/24082
关键词:
SNOWFALLALBEDOFLOODINGGAUGINGABLATIONSNOW WATER EQUIVALENTALTITUDEMELTING SNOWCOVERINGCALIBRATIONFLOWCONFLUENCETEMPERATUREABSORPTIONSNOWMELT WATERANNUAL RUNOFFDISCHARGEMETEOROLOGYWATER SYSTEMSHYDROLOGYCHEMICAL WEATHERINGPROGRAMSWATER SUPPLYRESERVOIRSQUANTIFICATIONSNOW ACCUMULATIONEVAPOTRANSPIRATIONWATER TOWERSAVALANCHESGASMEASUREMENTSHUMIDITYSOLAR RADIATIONAERIAL PHOTOGRAPHYWATER RESOURCESCATCHMENT AREASAERIAL PHOTOGRAPHSRADIATIONSNOW COVERICE COVERSPRINGRIPARIAN COUNTRIESCATCHMENT BASINSINTERNATIONAL WATERDEBRISLEADSMELTINGBASINSCONTAMINANTSARIDITYWATER USEWATERSNOWDRIFTSCLOUDSHYPSOMETRIC CURVEWATER RESOURCES MANAGEMENTDRAINAGE BASINSNOW LINERAINFALLSCIENCESDRAINAGEGLACIERSAQUIFERSCONSUMPTIVE USENAVIGATIONAL CHARTSSTREAMFLOWCHEMISTRYSNOW PACKCLIMATOLOGICAL DATARUNOFFBASINFROSTLEADCLIMATE CHANGEDROUGHTBARRIERSSNOW MELTCLIMATEGLACIAL LAKESSNOW FALLSNOW DEPTHSNOWMELTDRAINAGE AREACATCHMENTCOLORSDRAINSMONITORING STATIONSRIVERSANNUAL STREAM FLOWANNUAL FLOWDRAINFLOW GAUGINGWATER RESOURCES PLANNINGSURFACE RUNOFFHYDROLOGIC REGIMEEROSIONENGINEERING HYDROLOGYLAKESLANDICE MELTENGINEERINGSNOW FIELDSIRRIGATIONWATERSHEDBRIGHTNESSGROUNDWATERMETERSCONSERVATIONCOALICEEARTH SCIENCESGLACIER RUNOFFICE AGELESSRAINPRESSURECATCHMENT AREASEAICE DYNAMICSPIPESGAUGING STATIONSCLIMATOLOGYEVAPORATIONGLACIER—RUNOFFRIPARIANCHANNELENERGYMINERALSREMOTE SENSINGReportRapportInforme
年份:
2015
出版地:
Washington,USA
语种:
English
摘要:
The headwaters of the Amu Darya and Syr Darya in the western Tien Shan, Pamir and Hindu Kushmountains are a major source of stream flow into the Aral Sea Basin. The water security—affectingenergy and food security—of this region and the consequent regional dynamics and politics are connected tothese headwaters. Recent concerns related to climate change, glacier retreat and stream flow from these mountains haveserved to illustrate the very limited understanding that exists concerning the hydrologic regimes of the mountainheadwaters of these major river systems as well as of the glaciers, that are a component of those regimes. A better understanding of these hydrologic processes is critical for assessing the amount andtiming of water supply and hydropower available (both current and future) for the various countries in theCentral Asia region that have headwaters originating in these mountains. Such an understanding is also criticalin making estimates of runoff changes under a climate change future. This is the main objective of this study.

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