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Chinese Academy of Sciences Institutional Repositories Grid
Streamflow response to seasonal snow cover extent changes in large Siberian watersheds

文献类型:期刊论文

作者Yang, DQ; Robinson, D; Zhao, YY; Estilow, T; Ye, BS
刊名JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
出版日期2003-09-19
卷号108期号:D18页码:1-14
关键词runoff snow cover Siberian rivers
ISSN号2169-897X
DOI10.1029/2002JD003149
通讯作者Yang, DQ(ffdy@uaf.edu)
英文摘要[1] This study uses remotely sensed long- term ( 1966 - 1999) weekly snow cover extent data to investigate snowmelt runoff response to seasonal snow cover change in the large Siberian watersheds ( Ob, Yenisei, and Lena basins). It quantified the seasonal cycles and variations of snow cover extent and river streamflow and identified a clear correspondence of river streamflow to seasonal snow cover extent change; i. e., an association of low streamflow with high snow cover extent during the cold season and an increase in discharge associated with a decrease of snow cover extent during the melt periods. This study also examined and compared the weekly mean streamflow with the weekly basin snow cover extent for the study period. The results revealed a very strong linkage between the streamflow and snow cover extent change during the spring melt season over the large Siberian watersheds and developed a statistically significant weekly runoff- snow cover relation. This relation suggests a practical procedure of using remotely sensed snow cover information for snowmelt runoff forecasting over the large northern watersheds. Analyses of extreme ( high/ low) streamflow cases ( years) and the associated snow cover conditions indicate an association of high ( low) flood peak with late ( early) snowmelt in the Ob and Yenisei basins. Comparisons of snowmelt timing with peak flow show different associations between these two variables among the large Siberian rivers. These results demonstrate that the NOAA weekly snow cover extent data are useful for understanding and predicting streamflow changes in the Arctic regions. Snow cover water equivalent data/ products obtained by remote sensing technology and in situ snow observations are currently being examined for what we expect will eventually improve hydrologic forecasts over the large northern watersheds.
收录类别SCI
WOS关键词CLIMATE-CHANGE ; VARIABILITY ; MODEL ; PRECIPITATION ; CIRCULATION ; DISCHARGE ; UPDATE ; ICE
WOS研究方向Meteorology & Atmospheric Sciences
WOS类目Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:000185477300001
出版者AMER GEOPHYSICAL UNION
URI标识http://www.irgrid.ac.cn/handle/1471x/2556865
专题寒区旱区环境与工程研究所
通讯作者Yang, DQ
作者单位1.Univ Alaska, Water & Environm Res Ctr, Fairbanks, AK 99775 USA
2.Rutgers State Univ, Dept Geog, Piscataway, NJ 08854 USA
3.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou 730000, Peoples R China
推荐引用方式
GB/T 7714
Yang, DQ,Robinson, D,Zhao, YY,et al. Streamflow response to seasonal snow cover extent changes in large Siberian watersheds[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2003,108(D18):1-14.
APA Yang, DQ,Robinson, D,Zhao, YY,Estilow, T,&Ye, BS.(2003).Streamflow response to seasonal snow cover extent changes in large Siberian watersheds.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,108(D18),1-14.
MLA Yang, DQ,et al."Streamflow response to seasonal snow cover extent changes in large Siberian watersheds".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 108.D18(2003):1-14.

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来源:寒区旱区环境与工程研究所

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