During the day.
The Nez Perce felt that owning land was wrong because they thought that the land shouldn't be owned but just kept free.
It was sunny and had beautiful breezes and sunshine
hard to say because "most famous" is subjective. some valleys are well-known: silicon valley, san Fernando valley, great rift valley, death valley, yosemite valley, central valley, nile valley, napa valley, Rhine valley
The Yangtse Valley, Indus Valley, Tigris Valley, Euphrates Valley, Nile Valley.
Death Valley
Sea breezes are felt during the day.
breezeis a t hree
Mountain breezes happen at night, valley breezes happen during the day.
Local winds
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.
Local winds
yes
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.
I am sorry to say but they are nothing alike except the fact that they involve wind and air.
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.
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.
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.