An ensemble-based snow data assimilation framework with applications to permafrost modeling

conductivity, is a key control on the thermal state of near surface permafrost. At the same time, accurately estimating the seasonal snow cycle at the kilometre scale is a considerable hydrometeorological challenge. Consequently, snow represents a major source of uncertainty in permafrost models. To...

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Bibliographic Details
Main Authors: Aalstad, K., Westermann, S., Boike, Julia, Bertino, L., Aas, K. S.
Format: Conference Object
Language:unknown
Published: 2016
Subjects:
Online Access:https://epic.awi.de/id/eprint/43316/
https://media.gfz-potsdam.de/bib/ICOP/ICOP_2016_Book_of_Abstracts.pdf
https://hdl.handle.net/10013/epic.49777