编号
zgly0001586623
文献类型
期刊论文
文献题名
雅鲁藏布江流域降水中氧稳定同位素的时空变化(英文)
作者单位
InstituteofTibetanPlateauResearchCAS
InstituteofTibetanPlateauResearch
CAS
InstituteofTibetanWaterResourceReconnaissanceandDesigning
KeyLaboratoryofCryosphereandEnvironment
ColdandAridRegionsEnvironmentalandEngineeringRese
母体文献
Journal of Geographical Sciences
年卷期
2007年03期
年份
2007
分类号
P426.65
关键词
YarlungZangboRiverBasin
δ18O
precipitation
temporalandspatialvariations
文摘内容
This paper reveals the temporal and spatial variations of stable isotope in precipita-tion of the Yarlung Zangbo River Basin based on the variations of δ18O in precipitation at four stations (Lhaze,Nugesha,Yangcun and Nuxia) in 2005. The results show that δ18O of pre-cipitation has distinct seasonal changes in the Yarlung Zangbo River Basin. The higher value of δ18O occurs in spring prior to monsoon precipitation,and the lower value occurs during monsoon precipitation. From the spatial variations,with the altitude-effect and rainout process during moisture transport along the Yarlung Zangbo River Valley,18O of precipitation is gradually depleted. Thus,δ18O of precipitation decreases gradually from the downstream to the upstream,and the lapse rate of δ18O in precipitation is approximately 0.34‰/100m and 0.7‰/100km for the two reasons. During monsoon precipitation,spatial variation of δ18O in precipitation is dominated by the amount effect in the large scale synoptic condition.