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The small air circulation patterns that move short distances and can blow from any direction are called local winds. These winds are typically influenced by local topography, temperature differences, and changes in pressure. Examples include sea breezes, mountain breezes, and valley breezes.
Monsoons are heavy rainfalls, this is not like a tsunami.
Miami Florida.
It depends which part of the Pacific. Much of the Pacific is within 30 degrees of the equator, where the wind tends to blow from the east. In the mid-latitudes, the prevailing winds are westerly.
Tuhan.
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Where Breezes Blow - 1915 was released on: USA: 20 June 1915
they blow from the sea and then out to land
a breeze at the seaa and they blow when the wind is turned on
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The cast of Where Breezes Blow - 1915 includes: Elmer Booth Edith Borella Edward Dillon Frankie Newman Bobby Ray Fay Tincher as Fay Chester Withey
Im Waiting for You Mofooos to answer, so ANSWER! UGH >.<
The ocean is warmer than the land, so the air above it rises faster and has to be replaced by air originally over the land. Opposite of "sea breezes". Happens mostly early in the day.
The ocean is warmer than the land, so the air above it rises faster and has to be replaced by air originally over the land. Opposite of "sea breezes". Happens mostly early in the day.
Land breezes blow across the sea, from the land to the sea. If you don't know that yet, then explaining the rest to you would be useless
The small air circulation patterns that move short distances and can blow from any direction are called local winds. These winds are typically influenced by local topography, temperature differences, and changes in pressure. Examples include sea breezes, mountain breezes, and valley breezes.
Land breezes occur when the ocean surface is warmer than the adjacent land. This can occur at night, as the land cools faster than the water. The wamer water causes the air above it to rise, while air sinks over the cooler land. This creates areas of low and high pressure respectively. The air will blow from the high pressure to the low pressure, or, in other words, from the land to the ocean. This creates a land breeze.