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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Antarctica
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Victoria Land
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McMurdo dry valleys (1)
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Asia
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Primary terms
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Asia
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calcium (1)
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meteorology (2)
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nitrogen (1)
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United States
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soils
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snowmelt
Brine formation in cold desert, shallow groundwater systems: Antarctic Ca-Cl brine chemistry controlled by cation exchange, microclimate, and organic matter
Characterization of the Grigna karst aquifer (Northern Italy) by springs monitoring and tracer tests
Heavy Rainfall-triggered Flash Floods around the Amarnath Holy Cave
Susceptibility assessment of landslides caused by snowmelt in a typical loess area in the Yining County, Xinjiang, China
A Perspective on Rishiganga-Dhauliganga Flash Flood in the Nanda Devi Biosphere Reserve, Garhwal Himalaya, India
Monitoring of Rainfall and Soil Moisture at the Rebaixader Catchment (Central Pyrenees)
A study of the gas–water characteristics and their implications for the coalbed methane accumulation modes in the Southern Junggar Basin, China
Influence of Desert Springs on Habitat of Endangered Zuni Bluehead Sucker ( Catostomus discobolus yarrowi )
Annual cycle of temperature and snowmelt runoff in Satluj River Basin using in situ data
Abstract Melting of snow and ice contributes a large amount of water to the streamflow in the Satluj River. During the winter season, there is low base flow in the river as compared to spring and summer. Temperature is one of the key factors which directly impacts snow and ice melting throughout the year. A substantial amount of snowmelt only occurs when all the snow in a pack reaches isothermal condition. It is therefore very important to know the duration of impact of temperature on snowmelt runoff. Since the Himalayas have very few stations observing hydrological as well as meteorological conditions, it is difficult to validate the snowmelt models and examine changes in small-scale features in river basins of the region. The present study examines the annual cycle and interannual variability of runoff in the Satluj Basin in the western Himalayas and documents the impact of temperature on snowmelt runoff of Satluj River using daily in situ data for the period 1982–2005. A multivariate regression model using precipitation and surface temperature has been developed to predict the discharge of Satluj River at a daily scale. It is seen that after every warm phase and cold phase of temperature, the impact persists for around one month and affects the snowmelt runoff during January, February and March at lower- and higher-elevation stations such as Bhakra and Kasol, respectively. The effect of a large fall and rise in temperature is noticed on snowmelt runoff measured at all the discharge stations, while a small temperature change does not affect the observed discharge at all the stations. The remote sensing and reanalysis data are consistent with in situ data in the basin, and there is no major change in peak month of discharge or the amplitude during two different periods at Rampur gauge station.