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Incorrect ice analysis and/or forecast near coasts can give anomalous T2m temperatures at nearby land locations.  Too much ice tends to make land temperatures too cold, too little tends to keep land temperatures nearer sea temperatures.

Fig2.1.4.8-1:Broadscale bias  General bias of ice thickness from LIM2.  The scale is in m.  Red too thick, blue too thin.  The averages hide a lot of features and the bias in ice thickness in LIM2 is not uniform.

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