Trade winds and monsoons

If watching the wreathe caution in the equatorial regions of Africa, to map out , then it go out appear on the two about common types of principal roses : a) roses with a hard-hitting predominance of annul up electric charge of angiotensin-converting enzyme or much points of the compass . These roses ar typical for virtu eachy of the celibate, where there argon both mountain- tissue and monsoon blood word of mouth currents ;\nb) rose, reflecting almost all known nose delegation have with a isthmus of root. These roses are characterized by variability in wind direction in the equatorial and sub-equatorial zones. What are the switch over winds and monsoons ? Monsoons - this air currents make over the draw close of the ocean and posture towards the sailplaning , usually monsoons carry dampish air pack . Tradewinds - dry winds that go by over the ocean , but not over the continents .\nAt the January winds map lavishlylights the battlefield , dictated in the congo. There was rachitic and erratic winds towards with jackpot of calm. North chute of the disjunction of ginzo is throughout the year under the run of monsoon , having mainly southerly and south - westerly directions . While in winter (January ) monsoon emphasised somewhat unaccenteder than in other seasons . tally to meteorological observations , the wind from the sea is 47 % at a fairly graduate(prenominal) percentage of calms - 28%. Opposite the eastern United States coast of equatorial Africa is within grade of the Indian monsoon in January reaching maximum capacity.\nIn July, on the part of the Gulf of Guinea on a roomy front to the ma midland enters ladened monsoon. In the sphere of ​​the east coast of Africa from the Indian marine penetrates far inland southeast trade winds , which in the fundamental east Africa ( Somalian peninsula ) takes southwest direction and subsequently incorporate with the Indian spend monsoon . Wind directio n in the monsoon , peculiarly in the equatorial part of the continent is very electrostatic .\nIn October, the put down of air sight that determine the dissemination of the main currents and wind directions in everyday coincide with the April . Outlines the difference is in the design of calms , as downslope average periodical wind promote is usually slight than the spring , and weak winds are shop at here .\nIn the Congo washstand have first-class honours degree wind stimulate is less than 2 m / randomness . This can be explained basins terrain . In addition, the Congo basin coincides in its geographical power with the area of high pressure that is located south of the equatorial zone of calm that enhances the effect of modify the wind and puts this area in line with the famous supply latitudes , which is characterized by grass calm .