<?xml version="1.0" encoding="UTF-8"?>
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<title>Engineering</title>
<link href="http://dr.lib.sjp.ac.lk/handle/123456789/3439" rel="alternate"/>
<subtitle/>
<id>http://dr.lib.sjp.ac.lk/handle/123456789/3439</id>
<updated>2026-01-07T04:02:14Z</updated>
<dc:date>2026-01-07T04:02:14Z</dc:date>
<entry>
<title>Kalman filter based data assimilation system to improve numerical sea ice predictions in the Arctic Ocean</title>
<link href="http://dr.lib.sjp.ac.lk/handle/123456789/8899" rel="alternate"/>
<author>
<name>Mudunkotuwa, D.Y</name>
</author>
<author>
<name>De Silva, L.W.A</name>
</author>
<author>
<name>Yamaguchi, H</name>
</author>
<id>http://dr.lib.sjp.ac.lk/handle/123456789/8899</id>
<updated>2020-02-18T05:57:53Z</updated>
<published>2019-01-01T00:00:00Z</published>
<summary type="text">Kalman filter based data assimilation system to improve numerical sea ice predictions in the Arctic Ocean
Mudunkotuwa, D.Y; De Silva, L.W.A; Yamaguchi, H
With the recent changes in the Arctic climate,&#13;
increased transportation can be observed in the Arctic Ocean.&#13;
For safe navigation along the Arctic Sea routes, it is important&#13;
to accurately predict the ice conditions. In this study the iceocean&#13;
coupled Ice-POM model is improved by a Kalman filter&#13;
based data assimilation system. This system incorporates sea ice&#13;
observation data such as sea ice concentration, sea ice thickness&#13;
and sea ice velocity to improve the numerical predictions. Ocean&#13;
part of the model is based on the Princeton Ocean Model&#13;
while the Ice model considers the discrete characteristics of ice&#13;
along the ice edge. In an ice-ocean coupled model, atmospheric&#13;
forcing directly affects the accuracy of predictions. However,&#13;
different atmospheric data sets produced by different weather&#13;
agencies show large differences in the Arctic region. Model&#13;
errors largely depend upon the inaccuracies in forcing data.&#13;
This study uses an ensemble of multiple atmospheric data sets&#13;
collected from different weather agencies and the spread of the&#13;
ensemble is taken as an indicator of the model error covariance.&#13;
The Observation errors were varied according to the location&#13;
and the season. Assimilation has improved the predictions of&#13;
sea ice variables. It has also indirectly improved the ocean&#13;
conditions. This Atmospheric forcing based Kalman filter (AFKF)&#13;
method outperforms other assimilation methods such as direct&#13;
assimilation and nudging methods.
</summary>
<dc:date>2019-01-01T00:00:00Z</dc:date>
</entry>
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