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- W397740701 abstract "The temporary storage of precipitation in snowpack and the subsequent melting greatly influences the hydrologic regime. During the period of snow storage, there will be little or no water input to the ground. The groundwater reservoir will gradually decline by draining to the stream, whose discharge recedes in proportion to the falling groundwater level and flow. During snowmelt, the groundwater reservoir recovers and stream discharge may reach its annual peak by contributions from groundwater as well as overland flow. This chapter presents and discusses findings of isotope studies in catchments where snowmelt accounts for an important part of the total water input, with the focus on isotopic and hydrologic conditions related to meltwater input. Isotope studies have made a considerable contribution to our knowledge of catchment flow processes. The importance of direct measurements of the isotope content of the water input to the ground, that is, the snowpack drainage, must be emphasized in studies of snowmelt runoff. Other methodological problems concern the spatial variability of the isotope content of the pre-event water contributing to streamflow, and how to handle temporal variability of the isotope content of the water input. When it comes to snowmelt infiltration and runoff, it can be noted that no studies have been found where isotopes have been used in connection with measurements of soil frost and related analysis of the water flow." @default.
- W397740701 created "2016-06-24" @default.
- W397740701 creator A5012368671 @default.
- W397740701 date "1998-01-01" @default.
- W397740701 modified "2023-10-18" @default.
- W397740701 title "Snowmelt-Dominated Systems" @default.
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- W397740701 doi "https://doi.org/10.1016/b978-0-444-81546-0.50019-7" @default.
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