Kinematic wave modelling of saturated basal flow in a snowpack
(1997) In Hydrological Processes 11(2). p.177-187- Abstract
- Movement of snowmelt water through a thin saturated layer at the infiltrating base of a snowpack is modelled by applying the kinematic wave theory. Analytical solutions are obtained for flow depth, velocity and discharge assuming that the rate of input to the saturated layer due to vertical percolation is constant. This assumption results in a linear rise and recession of the snowmelt hydrograph. The solutions are extended to the case of time-varying input. An explicit consideration of infiltration leads to a free boundary problem.
Please use this url to cite or link to this publication:
https://lup.lub.lu.se/record/2595382
- author
- Singh, P. ; Bengtsson, Lars LU and Westerstrom, G.
- organization
- publishing date
- 1997
- type
- Contribution to journal
- publication status
- published
- subject
- in
- Hydrological Processes
- volume
- 11
- issue
- 2
- pages
- 177 - 187
- publisher
- John Wiley & Sons Inc.
- external identifiers
-
- scopus:0031076341
- ISSN
- 1099-1085
- DOI
- 10.1002/(SICI)1099-1085(199702)11:2<177::AID-HYP429>3.0.CO;2-L
- language
- English
- LU publication?
- yes
- id
- af574efd-a9b1-471a-8148-fd40660128df (old id 2595382)
- date added to LUP
- 2016-04-04 07:12:36
- date last changed
- 2022-01-29 01:54:58
@article{af574efd-a9b1-471a-8148-fd40660128df, abstract = {{Movement of snowmelt water through a thin saturated layer at the infiltrating base of a snowpack is modelled by applying the kinematic wave theory. Analytical solutions are obtained for flow depth, velocity and discharge assuming that the rate of input to the saturated layer due to vertical percolation is constant. This assumption results in a linear rise and recession of the snowmelt hydrograph. The solutions are extended to the case of time-varying input. An explicit consideration of infiltration leads to a free boundary problem.}}, author = {{Singh, P. and Bengtsson, Lars and Westerstrom, G.}}, issn = {{1099-1085}}, language = {{eng}}, number = {{2}}, pages = {{177--187}}, publisher = {{John Wiley & Sons Inc.}}, series = {{Hydrological Processes}}, title = {{Kinematic wave modelling of saturated basal flow in a snowpack}}, url = {{http://dx.doi.org/10.1002/(SICI)1099-1085(199702)11:2<177::AID-HYP429>3.0.CO;2-L}}, doi = {{10.1002/(SICI)1099-1085(199702)11:2<177::AID-HYP429>3.0.CO;2-L}}, volume = {{11}}, year = {{1997}}, }