1. Hotter air goes up (examples: hot steam, flame, etc), cooler air stays down (mist, etc) and replaces the air that went up: the horizontal moving of the air thus formed is the wind.
2. Land heats up & cools down faster than the sea (that's why sea appears to be "warm" at night).
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So: at night, the land cools down, the sea stays warm, so the lower air from land replaces the air that lifts above the sea - wind blows from land towards the sea.
At daytime, land heats up more than the sea, land air goes up, sea air replaces it - the wind blows from sea towards land.
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.
The four types of breezes are land breeze (blows from land to water at night), sea breeze (blows from sea to land during the day), mountain breeze (cold air descending from mountains at night), and valley breeze (warm air rising in valleys during the day).
A sea breeze is usually a mild wind that blows over open waters. There are offshore?æwind breezes which are identical to a sea breeze, but have higher wind speeds.
Typically, land breezes are cooler than water breezes because land heats up and cools down more quickly than water. This temperature difference creates the conditions for the air to move from the cooler land to the warmer water during a land breeze, and from the cooler water to the warmer land during a sea breeze.
Land breezes and sea breezes are both types of local wind patterns that are caused by the temperature difference between land and water. During the day, land heats up more quickly than water, creating a low-pressure area over the land and a high-pressure area over the water, resulting in a sea breeze blowing from the water to the land. At night, the land loses heat faster than water, creating a high-pressure area over the land and a low-pressure area over the water, leading to a land breeze blowing from the land to the water.
Land breezes occur during the time of night.
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.
The four types of breezes are land breeze (blows from land to water at night), sea breeze (blows from sea to land during the day), mountain breeze (cold air descending from mountains at night), and valley breeze (warm air rising in valleys during the day).
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.
A sea breeze is usually a mild wind that blows over open waters. There are offshore?æwind breezes which are identical to a sea breeze, but have higher wind speeds.
Yes, I think I know. A sea breeze comes from the west,bringing moisture in from the sea. A land breeze (I call it a "lee" breeze) comes from the east,TAKING AWAY moisture (dessicating/drying) and pumping it BACK INTO the sea. Breezes from the east,are also sometimes called "zephyrs".
a sea breeze is caused by the sea winds and occurs at the night, while land breezes are during the day and are from land:) lol.
'land breeze's' are cool breezes at night caused by differences in heating and cooling rates of land and water
Sea breezes and land breezes are both caused by temperature differences between land and water. During the day, the land heats up faster than the water, creating a sea breeze that blows from the cooler water towards the warmer land. At night, the land cools down faster than the water, generating a land breeze that moves from the cooler land towards the warmer water.
Typically, land breezes are cooler than water breezes because land heats up and cools down more quickly than water. This temperature difference creates the conditions for the air to move from the cooler land to the warmer water during a land breeze, and from the cooler water to the warmer land during a sea breeze.
Mountain breezes typically form during the night. As the sun sets, the air in the valley cools more quickly than the air on the mountain, creating a temperature difference. This temperature difference causes the air to flow from the mountain down into the valley, creating a mountain breeze.
Valley breezes and mountain breezes are considered convection currents because they result from the differential heating and cooling of the air in these geographic features. During the day, the sun heats the valley or mountain slope, causing the air to rise and create an upslope breeze (valley breeze). At night, the land cools faster than the air, resulting in the air sinking and flowing down the slope (mountain breeze). This cycle of warm air rising and cool air sinking is characteristic of convection currents.