dustbowl
It's prevailing Winds
Hurricanes are primarily driven by easterly winds called trade winds near the equator and westerly winds known as the westerlies in higher latitudes. These winds help steer hurricanes across the Atlantic Ocean.
The prevailing winds in Alaska are known as westerlies. These winds blow from the west to the east, helping to influence the weather patterns and climate in the region.
Winds between 28 knots and 55 knots on the Beaufort scale are known as gale force winds.
westward
dust bowl
A dusty wind is called a "haboob." It is a type of intense dust storm that occurs in arid regions, typically associated with thunderstorms or strong winds.
pressure.
Globally.
The calm region produced by converging trade winds is called the doldrums. This area is known for its light winds and minimal atmospheric pressure, making it difficult for sailors to navigate through.
Siroccos are hot winds, often dusty or rainy, blowing from North Africa across the Mediterranean to southern Europe. The winds come from the Sahara and reaches hurricane speeds in North Africa and Southern Europe.
Winds are produced when there is a difference in atmospheric pressure. Air moves from areas of high pressure in the atmosphere to areas of low pressure. This movement of air is experienced as wind.
100 Tradewinds Cheetah 594 were produced in 1968
The Harmattan is a cold-dry and dusty trade wind, blowing over the West African subregion of the Sahara Desert.
The huge sandstorms located in West Africa are known as the Harmattan. These sandstorms are dry and dusty winds that blow from the Sahara Desert southwards across the region, bringing haze, reduced visibility, and sometimes health issues due to the fine dust particles in the air.
Steady winds became known as trade winds.
Steady winds became known as trade winds.