Some examples of local wind patterns include sea breezes, mountain breezes, and valley breezes. Sea breezes occur when cooler air from the sea moves inland during the day, while mountain breezes are caused by cool air descending at night from mountains. Valley breezes occur when warm air rises in the daytime from a valley floor.
Sea breeze and valley breeze are two breezes that result from local topography. Sea breeze occurs during the day when the land heats up faster than the sea, causing air to rise over the land and draw in cooler air from the sea. Valley breeze occurs during the day when the valley floor heats up faster than the surrounding slopes, causing warm air to rise up the valley.
Two types of local winds are sea breezes and mountain/valley breezes. Sea breezes occur when cooler air from the water moves inland during the day, while mountain/valley breezes occur when cool air from higher elevations flows downslope at night and warm air rises during the day.
Sea breezes come from the sea onto the land, and land breezes come from the land onto the sea.
There are numerous local winds, but some common examples include sea breezes, land breezes, valley breezes, and mountain/valley winds. These winds are driven by temperature differences between land and water, or between different types of terrain, and occur on a local scale.
Sea Breezes was created in 1972.
Sea Breezes: From sea to land.Land Breezes: From land to sea.
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Sea breezes are felt during the day.
Land breezes and sea breezes are local winds that occur in specific coastal regions. Land breezes blow from land to sea at night, while sea breezes blow from sea to land during the day. They are caused by temperature differences between the land and sea.
Mountain breezes happen at night, valley breezes happen during the day.
Sea Breezes - Magazine - was created in 1919.