Search results
Results From The WOW.Com Content Network
The westerlies, anti-trades, [2] or prevailing westerlies, are prevailing winds from the west toward the east in the middle latitudes between 30 and 60 degrees latitude. They originate from the high-pressure areas in the horse latitudes (about 30 degrees) and trend towards the poles and steer extratropical cyclones in this general manner. [ 3 ]
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 westerlies (blue arrows) and trade winds (yellow and brown arrows) The trade winds or easterlies are permanent east-to-west prevailing winds that flow in the Earth's equatorial region. The trade winds blow mainly from the northeast in the Northern Hemisphere and from the southeast in the Southern Hemisphere , strengthening during the winter ...
Nordeste (moderate wind from northwest in brazilian Northeast region) Carpinteiro (strong southeasterly wind along the southern Atlantic coast of Brazil) [citation needed] Garua, la garúa, or garoa (dry winds hitting the lower western slopes of the Andes) [citation needed] Minuano (southern Brazil) Zonda wind (on the eastern slope of the Andes ...
The westerlies and trade winds Winds are part of Earth's atmospheric circulation Easterly winds, on average, dominate the flow pattern across the poles, westerly winds blow across the mid-latitudes of the Earth, polewards of the subtropical ridge , while easterlies again dominate the tropics .
Mistral wind blowing near Marseille.In the centre is the Château d'If.. The mistral (Catalan: mestral, Corsican: maestrale, Croatian: maestral, Greek: μαΐστρος, Italian: maestrale, Maltese: majjistral) is a strong, cold, northwesterly wind that blows from southern France into the Gulf of Lion in the northern Mediterranean. [1]
In the mid-latitude westerlies, upper level troughs and ridges often alternate in a high-amplitude pattern. For a trough in the westerlies, the region just west of the trough axis is typically an area of convergent winds and descending air – and hence high pressure –, while the region just east of the trough axis is an area of fast ...
A Western Disturbance over Northern India and Pakistan in November 2012. A western disturbance is an extratropical storm originating in the Mediterranean region that brings sudden winter rain to the northwestern parts of the Indian subcontinent, [1] [2] which extends as east as up to northern parts of Bangladesh and South eastern Nepal. [3]