Local winds are winds that blow over short distances caused by unequal heating of the earths surface in a small area.
The small air circulation patterns that move short distances and can blow from any direction are called local winds. These winds are typically influenced by local topography, temperature differences, and changes in pressure. Examples include sea breezes, mountain breezes, and valley breezes.
wind speed is more when there is more pressure difference. with increase in temperature at a place the air expands , rises and creates low pressure. if the place near to it has very high pressure compared to the pressure at that place then strong and speed winds blow.
air moves from high to low, creating difference in temperature
As we know, low air pressure often causes it to rain. When moist winds blow over mountains, the air on the other side is thinned out - the pressure is lowered. This causes rain to fall.
when the winds eventually blow over the land, they moderate the temperature of the air over the land.
Well, it has to do with high pressure, low pressure, horse latitudes and doldrums.
It's the change in air temperature. Cold air heats up and becomes hot air and rises up since hot air is lighter than cold air. The other cold air stays nearer to the ground and that is what causes the winds to blow.
Winds are simply air that is 'sucked' from a high-pressure area to a low-pressure area.
air pressure
Local winds are winds that blow over short distances caused by unequal heating of the earths surface in a small area.
Air pressure toward regions of lower air pressure
The small air circulation patterns that move short distances and can blow from any direction are called local winds. These winds are typically influenced by local topography, temperature differences, and changes in pressure. Examples include sea breezes, mountain breezes, and valley breezes.
ocean currents may be considerably warmer or colder than the normal surface air temperatures. their effect is greatest when the prevailing winds blow from the water to the land.
They come from planet Mars the solar winds blow them onto earth.
Air density is subject to change by temperature and altitude. When air experiences a large change in either temperature or altitude, it expands or contracts, creating motion in the air. When high pressure and low pressure systems meet, winds can grow exponentially, as warm air rises over cooler air.
Winds blowing is the effect of change in the temperature in the air. Since hot air is lighter than cold air, hot air develops from cold air nearer above ground, and when it's hot enough, it becomes lighter and rises up. Cold air stays nearer to the ground and the force of hot air coming up and cold air staying put forms winds. If the winds are big that means the change of temperature is big too.