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...

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Bibliographic Details
Main Authors: Marchenko, S., van Pelt, W.J.J., Claremar, B., Machguth, H., Reijmer, C.H., Pettersson, R., Pohjola, V.A.
Other Authors: Sub Dynamics Meteorology, Marine and Atmospheric Research
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Online Access:https://dspace.library.uu.nl/handle/1874/352696