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An example of the impact of the westerlies is when dust plumes, originating in the Gobi Desert combine with pollutants and spread large distances downwind, or eastward, into North America. [8] The westerlies can be particularly strong, especially in the Southern Hemisphere, where there is less land in the middle to cause the progression of west ...
The westerlies play an important role in carrying the warm, equatorial waters and winds to the western coasts of continents, [13] [14] especially in the southern hemisphere because of its vast oceanic expanse. The westerlies explain why coastal Western North America tends to be wet, especially from Northern Washington to Alaska, during the winter.
The term originally derives from the early fourteenth century sense of trade (in late Middle English) still often meaning "path" or "track". [2] The Portuguese recognized the importance of the trade winds (then the volta do mar, meaning in Portuguese "turn of the sea" but also "return from the sea") in navigation in both the north and south Atlantic Ocean as early as the 15th century. [3]
Westerly winds blowing across the Atlantic bring moist air into Europe. In years when westerlies are strong, summers are cool, winters are mild and rain is frequent. If westerlies are suppressed, the temperature is more extreme in summer and winter leading to heat waves, deep freezes and reduced rainfall. [7] [8]
The coastal Chinooks were the original term, used along the northwest coast, [1] and the term in the interior of North America is later and derives from the coastal term. [ 2 ] Along the Pacific Northwest coast, where the name is pronounced / t ʃ ɪ ˈ n ʊ k / ('chin'+'uk'), [ 2 ] the name refers to wet, warm winds off the ocean from the ...
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The horse latitudes are the latitudes about 30 degrees north and south of the Equator. [1] They are characterized by sunny skies, calm winds, and very little precipitation. They are also known as subtropical ridges or highs. It is a high-pressure area at the divergence of trade winds and the westerlies.
Llevantades (north-north-east and east-north-east on the east coast of Spain) Lodos (southwesterly towards Turkey. Strong "Lodos" events occur 6 - 7 times a year bringing 35 kt winds into Marmara Sea. The winds are funnelled SE from the Mediterranean and through the Dardanelles Strait.) Maestro (cold northerly in the Adriatic Sea)