000028518 001__ 28518
000028518 041__ $$aEnglish
000028518 100__ $$aYao, Z.
000028518 245__ $$aCharacteristics of Isotope in Precipitation, River Water and Lake Water in the Manasarovar Basin of Qinghai–Tibet Plateau
000028518 260__ $$c2009
000028518 300__ $$a551-556
000028518 511__ $$aKoshi, Article
000028518 511__ $$aCryosphere
000028518 520__ $$aThe stable hydrogen and oxygen of lake, river, rain and snow waters were investigated to understand the water cycle characteristics of the drainage basin of Manasarovar Lake in Tibet. Both δD and δ 18O of river water are larger than those of lake water and the effect of altitude on both δD and δ 18O is not very significant. This phenomenon was suggested to occur because Manasarovar basin is located in Qinghai–Tibet Plateau which has low latitude, high altitude, abundant glaciers, thin air and intensive solar radiation, resulting in higher evaporation in lake water.
000028518 653__ $$aManasarovar Basin
000028518 653__ $$aIsotope
000028518 653__ $$aAtmospheric Precipitation
000028518 653__ $$aRiver Water
000028518 653__ $$aLake Water
000028518 700__ $$aLiu, J.
000028518 700__ $$aHuang, H.-Q.
000028518 700__ $$aSong, X.
000028518 700__ $$aDong, X.
000028518 700__ $$aLiu, X.
000028518 773__ $$pEnvironmental Geology
000028518 773__ $$v57 (3)
000028518 773__ $$a10.1007/s00254-008-1324-y
000028518 8564_ $$uhttp://dx.doi.org/10.1007/s00254-008-1324-y$$yExternal link
000028518 980__ $$aARTICLE