earths atmosphere was formed as through the rotating mass of clouds and gases. there, the solid particles settled in the atmosphere and the lighter parts including gases rotated and formed the earths atmosphere. different regions exp. diff. type of pressure belts. this can be as though becoz of gravity. polar regions have high gravityand so exp. high pressue belts and vice versa.
It is False that high pressure areas on weather maps are in circles formed by isotherms.
i do't no
Wind blows from high-pressure areas to low-pressure areas. It does this simply because nature is trying to restore a balance between the different pressure areas.
When there is a great difference in air pressure between two areas, winds are strong. The air moves from high pressure to low pressure, causing faster winds to equalize the pressure difference.
Wind moves from areas of high pressure to areas of low pressure in an attempt to equalize pressure differences. This movement occurs in a circular pattern due to the Coriolis effect, which causes the wind to curve to the right in the northern hemisphere and to the left in the southern hemisphere.
It is False that high pressure areas on weather maps are in circles formed by isotherms.
Pressure moves between areas of high and low pressure through the process of air molecules moving from areas of high pressure to areas of low pressure. This movement creates wind and helps to equalize pressure differences in the atmosphere.
The relationship between air pressure and windis that air from areas of higher pressure flow to areas of lower pressure, creating wind.
i do't no
High pressure to areas of low pressure. This movement is due to the difference in air pressure between the two areas, creating a gradient that drives the flow of air.
After high-pressure areas are formed around the poles, cold polar air flows towards lower pressure regions. This movement of air is known as advection, and it helps to balance out the pressure differences between the poles and lower latitudes.
Wind blows from high-pressure areas to low-pressure areas. It does this simply because nature is trying to restore a balance between the different pressure areas.
wind!!
A steep cliff that separates two level areas of differing elevation is called a "escarpment."
When there is a great difference in air pressure between two areas, winds are strong. The air moves from high pressure to low pressure, causing faster winds to equalize the pressure difference.
Isobars are formed by connecting points on a map that have the same atmospheric pressure. Meteorologists use isobars to represent areas of high and low pressure, with closely spaced isobars indicating strong pressure gradients and potentially windy conditions.
Wind moves from areas of high pressure to areas of low pressure in an attempt to equalize pressure differences. This movement occurs in a circular pattern due to the Coriolis effect, which causes the wind to curve to the right in the northern hemisphere and to the left in the southern hemisphere.