Using the climatic map of Eurasia in the atlas, establish the features of the course of the zero isotherm on the territory of the mainland. Explain the reasons

The zero isotherm in the west of the continent passes in its northern part, which is explained by the influence of the warm North Atlantic current. In the depths of the mainland, it sinks far to the south, because the continentality of the climate is increasing. In the east of the mainland, the isotherm rises to the north again, since in the east the warm currents of Kuroshio and the North Pacific pass.

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