Impact of assimilating sea ice concentration, sea ice thickness and snow depth in a coupled ocean–sea ice modelling system
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Published:2019-02-08
Issue:2
Volume:13
Page:491-509
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ISSN:1994-0424
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Container-title:The Cryosphere
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language:en
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Short-container-title:The Cryosphere
Author:
Fritzner SindreORCID, Graversen Rune, Christensen Kai H., Rostosky PhilipORCID, Wang KeguangORCID
Abstract
Abstract. The accuracy of the initial state is very important for the
quality of a forecast, and data assimilation is crucial for obtaining the
best-possible initial state. For many years, sea-ice concentration was the
only parameter used for assimilation into numerical sea-ice models. Sea-ice
concentration can easily be observed by satellites, and satellite
observations provide a full Arctic coverage. During the last decade, an
increasing number of sea-ice related variables have become available, which
include sea-ice thickness and snow depth, which are both important parameters
in the numerical sea-ice models. In the present study, a coupled
ocean–sea-ice model is used to assess the assimilation impact of sea-ice
thickness and snow depth on the model. The model system with the assimilation
of these parameters is verified by comparison with a system assimilating only
ice concentration and a system having no assimilation. The observations
assimilated are sea ice concentration from the Ocean and Sea Ice Satellite
Application Facility, thin sea ice from the European Space Agency's
(ESA) Soil Moisture and Ocean Salinity mission, thick sea ice from
ESA's CryoSat-2 satellite, and a new snow-depth product derived from the
National Space Agency's Advanced Microwave Scanning Radiometer
(AMSR-E/AMSR-2) satellites. The model results are verified by comparing
assimilated observations and independent observations of ice concentration
from AMSR-E/AMSR-2, and ice thickness and snow depth from the IceBridge
campaign. It is found that the assimilation of ice thickness strongly
improves ice concentration, ice thickness and snow depth, while the snow
observations have a smaller but still positive short-term effect on snow
depth and sea-ice concentration. In our study, the seasonal forecast showed
that assimilating snow depth led to a less accurate long-term estimation of
sea-ice extent compared to the other assimilation systems. The other three
gave similar results. The improvements due to assimilation were found to last
for at least 3–4 months, but possibly even longer.
Publisher
Copernicus GmbH
Subject
Earth-Surface Processes,Water Science and Technology
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