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The trade winds act as the steering flow for tropical cyclones that form over the world’s oceans. Its poleward progression is accelerated by the development of a heat low over the Asian, African, and North American continents during May through July, and over Australia in December. Together with the trade winds, the westerlies enabled a round-trip trade route for sailing ships crossing the Atlantic and Pacific Oceans, as the westerlies lead to the development of strong ocean currents on the western sides of oceans in both hemispheres through the process of western intensification. Trade winds also steer African dust westward across the Atlantic Ocean into the Caribbean, as well as portions of southeast North America. The trade winds blow predominantly from the northeast in the Northern Hemisphere and טלגראס כיוונים חדרה כיוונים קריית גת (telegram4israel.net) from the southeast in the Southern Hemisphere. Unlike the Westerlies, these prevailing winds blow from the east to the west, and are often weak and irregular. The Westerlies or the Prevailing Westerlies are the prevailing winds in the middle latitudes between 35 and 65 degrees latitude. The westerlies can be particularly strong, especially in the southern hemisphere, where there is less land in the middle latitudes to cause the flow pattern to amplify, which slows the winds down.
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