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...
Published in: | Frontiers in Earth Science |
---|---|
Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Frontiers Media S.A.
2017
|
Subjects: | |
Online Access: | https://doi.org/10.3389/feart.2017.00016 https://doaj.org/article/fa48635311454e7186a720694b9b8230 |