Question

Describe five effects of the North East Trade winds in Ghana

Answer 1

Answer:

The trade winds or easterlies are the permanent east-to-west prevailing winds that flow in the Earth's equatorial region (between 30°N and 30°S latitudes). The trade winds blow predominantly from the northeast in the Northern Hemisphere and from the southeast in the Southern Hemisphere, strengthening during the winter and when the Arctic oscillation is in its warm phase. Trade winds have been used by captains of sailing ships to cross the world's oceans for centuries and enabled colonial expansion into the Americas and trade routes to become established across the Atlantic and Pacific oceans.

In meteorology, the trade winds act as the steering flow for tropical storms that form over the Atlantic, Pacific, and southern Indian Oceans and make landfall in North America, Southeast Asia, and Madagascar and eastern Africa. Trade winds also transport African dust westward across the Atlantic Ocean into the Caribbean Sea, as well as portions of southeastern North America. Shallow cumulus clouds are seen within trade wind regimes and are capped from becoming taller by a trade wind inversion, which is caused by descending air aloft from within the subtropical ridge. The weaker the trade winds become, the more rainfall can be expected in the neighboring landmasses.

Answer 2

The trade winds or easterlies are the long-lasting east-to-west winning winds that stream in the Earth's tropical area (somewhere in the range of 30°N and 30°S scopes).

• The trade winds blow transcendently from the upper east in the Northern Hemisphere and from the southeast in the Southern Hemisphere, reinforcing throughout the colder time of year and when the Arctic swaying is in its warm stage.
• Trade winds have been utilized by commanders of cruising boats to cross the world's seas for quite a long time and empowered frontier venture into the Americas and trade courses to become set up across the Atlantic and Pacific seas.
• In meteorology, the trade winds go about as the directing stream for hurricanes that structure over the Atlantic, Pacific, and southern Indian Oceans and make landfall in North America, Southeast Asia, Madagascar, and eastern Africa.
• Trade winds additionally transport African residue toward the west across the Atlantic Ocean into the Caribbean Sea, just as parts of southeastern North America.
• Shallow cumulus mists are seen inside trade wind systems and are capped from becoming taller by a trade wind reversal, which is brought about by sliding air on high from inside the subtropical edge.
• The more fragile the trade winds become, the more precipitation can be anticipated in the adjoining landmasses.