Parameterizing deep water percolation improves subsurface temperature simulations by a multilayer firn model.
Deep preferential percolation of melt water in snow and firn brings water lower along the vertical profile than a laterally homogeneous wetting front. This widely recognized process is an important source of uncertainty in simulations of subsurface temperature, density, and water content in seasonal...
Main Authors: | , , , , , , |
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Other Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2017
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Subjects: | |
Online Access: | https://dspace.library.uu.nl/handle/1874/352696 |