Mountain and valley breezes are named for their respective origins in mountainous terrain. During the day, the sun heats the mountain slopes faster than the valleys, causing warm air to rise and creating a valley breeze that flows uphill. At night, the opposite occurs: the slopes cool more quickly than the valleys, causing cooler, denser air to flow down from the mountains, resulting in a mountain breeze. These breezes are named based on the direction of airflow relative to the terrain.
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.
Mountain breezes form due to temperature differences between the mountain slopes and the valleys. During the night, the air on the mountain slopes cools more quickly than the air in the valleys, causing the denser, cooler air to flow down into the valleys. This downward movement of cool air creates a breeze that can be felt in the lower elevations. As the sun rises, the process can reverse, leading to valley breezes during the day.
Breezes in valleys are formed because as the air warms during the day it rises along the slopes of the hills and mountains. As the warm air rises, cooler air is drawn in behind it causing a breeze.
During the day, the sun heats the mountain slopes, causing the air to rise due to convection currents. At night, the mountain cools faster than the surrounding air, creating denser air that flows down the slope due to gravity. This daily cycle of air movement is known as a mountain/valley breeze.
A hanging valley forms when a smaller glacier flows into a larger glacier, leaving the smaller valley elevated above the main valley floor after the larger glacier retreats. A cirque is created by the erosion of a mountain side by a glacier, resulting in a bowl-shaped depression. An arete is a sharp ridge formed between two cirques that erode toward each other. A horn is a pointed mountain peak that results from the glacial erosion of multiple cirques surrounding a summit, sharpening it into a distinctive shape.
Mountain breezes happen at night, valley breezes happen during the day.
Local winds
Local winds
yes
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.
Mountain breezes are the breezes in which mountains give off oxygen and carbon to create moisture, then it flows down to the cities causing cold wind. Valley Breezes are the air trapped in the valleys below making its way to the top and spreading out to combine with the mountain breezes.
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.
There are several types of breezes, but the most commonly referenced are sea breezes, land breezes, valley breezes, and mountain breezes. Sea breezes occur during the day when cooler air from the ocean moves inland, while land breezes occur at night when the land cools faster than the sea. Valley breezes form during the day as warm air rises from the valley, and mountain breezes occur at night as cooler air flows down from the mountains. Each type is influenced by local topography and temperature differences.
Local winds
A valley breeze flows up a valley or mountain slope.A mountain breeze blows down a mountain slope.For more information see the answers to the Related Questions shown below.
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.
it iss by daaa suns distance btw the earth