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Warm currents moderate winter temperatures.
Ocean currents redistribute thermal energy globally.
Heat redistribution would decrease, increasing temperature contrasts.
Cooling increases air density.
Strong heating near the equator causes rising air.
Coupled models help understand and predict monsoon behaviour.
Multiple data sources improve forecast accuracy.
Mountain breezes occur when cool dense air descends into valleys.
Uneven heating drives both air circulation and ocean circulation.
Global movement of air and water redistributes heat around Earth.
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