rise in temperature above freezing point due to the advection of warm air against a background of st – Russian translation

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rise in temperature above freezing point due to the advection of warm air against a background of steady negative temperatures

повышение температуры воздуха до 0 град. C и выше в результате адвекции тёплого воздуха на фоне установившихся отрицательных температур

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