describe the winter monsoon
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Monsoons are primarily seasonal winds in the warmer regions of the world caused by large temperature differences between land masses and adjacent oceans. In the winter, the circulation is from the cool land to the warmer sea, while in the summer, the opposite is true.
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Usually, winter monsoons usher in dry, cool conditions, replacing the rain and heat of their summer counterparts. Monsoons affect south, southeast and east Asia, northern Australia, west-central Africa and some warmer regions of North and South America.
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