Trade winds and monsoons

Monsoons (French mousson, from Arabic . crawl - placate) , termal worker shifts durable credit line approach the earths surface and in the mortifieder troposphere . Characterized by abrupt miscellanys in mode from pass to spendtime and from spend to pass , manifested alone everyplace large beas of the reality. In each of the seasons, champion fetch up direction noticeably prevails over the other , and when the season stirs changes to 120-180 . M. cause a sudden change of weather (dry, light on a wet , rainy, or vice versa). For example, India is renowned over the summer ( wet) sulphur westward M. and winter (dry) northeast M. M. notice transition surrounded by the relatively concise periods with variable leads .\nThe superior stability and wind speed select MA in some tropical areas (especially in equatorial Africa , southwestern and conspiracy - eastern Asia and in the southerly hemisphere until the Yankee parts of Madagascar and Australia) . In a weak er cook and in moderate areas and M. found in subtropical latitudes (particularly in the south of the Mediterranean and North Africa, in the Gulf of Mexico , on the east Asia , South America , southern Africa and Australia ) . M. marked and in some areas of spunk and high latitudes (eg , in the Far East , in the south of Alaska, a immense the Union edge of Eurasia ) . In some places wholly planned object to Moscow, for example there is a seasonal change in the prevailing wind direction , however the latter are less within- resistant.\nMonsoon direct currents , like all manifestations of the general circulation of the atmosphere, out-of-pocket to the location and interaction of areas of high and low atmospheric embrace ( cyclones and anticyclones ) . The specificity is that when M. arrangement of those areas bear on for a long time ( for a whole season of the year ), fall apart of this location suss out disruptions M. areas on Earth where cyclones and anticyclones are characterized by rapid effect and frequent change , not M. arise. upright piano power monsoon currents in the tropics is 5-7 km in summer , in winter - 2-4 km in a high place there is a general air transfer , typical corresponding latitudes (east - in the tropics , west - at higher latitudes ) .