Abstract:<p>In the Northern-Hemisphere mid latitudes the winter land-sea thermal contrast is expected to decrease with increasing CO<sub>2</sub> in the atmosphere, due to a faster warming of the continents with respect to the oceans. Moreover, the reduction of the winter thermal contrast is basin dependent, as it is influenced by regional warming patterns specific of the Atlantic and Pacific sectors, e.g. by the North-Atlantic Warming Hole.<br>In this work we run … Show more
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