Separation of a snowmelt hydrograph by stream conductance
- 15 April 1986
- journal article
- Published by Elsevier BV in Journal of Hydrology
- Vol. 84 (1-2), 157-165
- https://doi.org/10.1016/0022-1694(86)90049-1
Abstract
By the continuous measurement of stream conductance and discharge for a long snowmelt period, the runoff components were separated and the dominancy of subsurface flow was confirmed as found in the previous paper on stream temperature analyses.Keywords
This publication has 4 references indexed in Scilit:
- Separation of the snowmelt hydrograph by stream temperaturesJournal of Hydrology, 1985
- Use of specific conductance and contact time relations for separating flow components in storm runoffWater Resources Research, 1979
- Subsurface flow from snowmelt traced by tritiumWater Resources Research, 1975
- Runoff analysis by electrical conductance of waterJournal of Hydrology, 1971