The sides of the valley heating more quickly than the air around it
The sides of the valley cooling off more quickly than the air around it.
It is caused by the differences in temperature and elevation
a mountain breeze flows down a mountain and into a valley.
Valley breeze is a type of wind in the mountains. Katabatic wind is down hill wind.
downward
Clear day
Valley Breeze occurs in the day and Mountain breeze occurs in the night.
Convection causes it to rise, causing a valley breeze
valley breeze refreshes the mind in the morning.
Afternoons do give us an aromatic valley breeze, here.
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.
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.
a mountain breeze flows down a mountain and into a valley.
There are Four local winds: Valley Breeze, Mountain Breeze, Land Breeze, And Sea Breeze.
in the morning
After sunset the sun is no longer warming the mountain side and there is cooling of the air along the slope. The air becomes more dense and sinks into to valley. Thus the wind blows from the mountain side down into the valley and is thus called a mountain breeze.
Valley breeze is a type of wind in the mountains. Katabatic wind is down hill wind.
Northeast Monsoon!
downward