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 is a cousin to the pressure. Pressure moves the wind.
A southeast wind is from the southeast toward the northwest.
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.
Trade winds are strong winds that blow towards the equator from northeast or south east direction. They are planetary winds that keep blowing from subtropical high pressure zone to equilateral low pressure zones
The warmth of the Sun creates temperature differences that change the direction of the wind.
In the northern hemisphere wind blow around high-pressure systems in a clockwise direction. In the southern hemisphere, the wind blow is in the opposite (anticlockwise) direction.
Wind is a cousin to the pressure. Pressure moves the wind.
CLOCKWISE!!
Winds are simply air that is 'sucked' from a high-pressure area to a low-pressure area.
COUNTER CLOCKWISE= low pressure CLOCK WISE= high pressure
Trade winds are strong winds that blow towards the equator from northeast or south east direction. They are planetary winds that keep blowing from subtropical high pressure zone to equilateral low pressure zones
A southeast wind is from the southeast toward the northwest.
It would blow from the mass of high pressure to the mass of low pressure.Answer 2Looking down from a satellite, the northern hemisphere high pressure systems move in a clockwise direction and anticlockwise in the southern hemisphere.Low pressure systems are the reverse of these, IE clockwise in the southern hemisphere and anticlockwise in the northern hemisphere.
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.
Winds in a northern hemisphere low pressure system rotate counterclockwise around the low pressure center.
Trade winds are strong winds that blow towards the equator from northeast or south east direction. They are planetary winds that keep blowing from subtropical high pressure zone to equilateral low pressure zones
Ignoring the coriolis effect, winds blow form high to low, therefore the wind would blow from west to east, it would be a westerly wind.