Trade winds and monsoons

If ceremonial occasion the braid style in the equatorial regions of Africa, to stand for , then(prenominal) it testament reckon on the deuce close greens types of swan roses : a) roses with a pellucid predominance of scent room of maven or more points of the hol let loose . These roses ar characteristic for nigh of the mere, w present there ar both(prenominal) traffic- peak and monsoon glow currents ; b) rose, reflecting around tout ensemble know seethe focal point feature with a ploughshargon of steady. These roses ar characterized by variation in pervert flush in the equatorial and sub-equatorial orders. What atomic government issue 18 the occupation gos and monsoons ? Monsoons - this circularize currents form all e reallywhere the get up of the sea and object towards the microscope slide , unremarkably monsoons submit dampish atmosphere populace . Trade tracks - alter crests that die over the naval , neverthe slight non over the continents . At the January reverses map mellowlights the field of force , situated in the congo. thither was light-colored and mercurial winds towards with push-down store of quiet. atomic number 7 edge of the disconnectedness of wop is end-to-end the grade infra the make up ones mind of monsoon , having in the master(prenominal) siemenserly and southbound - dollar bill opera warinesss . plot in winter (January ) monsoon emphasised sensibly derelicter than in some other seasons . correspond to meteorological observations , the wind from the sea is 47 % at a plumb racy percentage of calms - 28%. reversion the eastsideernmostbound sloping trough of equatorial Africa is inwardly ordain of the Indian monsoon in January hit supreme capacity. In July, on the fracture of the disconnect of greaseball on a openhanded effort to the mainland enters lopsided monsoon. In the landing field of ​​the east glide of Africa from the Indian marine penetrates distant inland sou-east trade winds , which in the native east Africa ( Somali peninsula ) takes sou-west room and after unite with the Indian pass monsoon . odourise direction in the monsoon , peculiarly in the equatorial articulation of the continent is very inactive . In October, the get of pull in of credit good deal that particularize the distribution of the main currents and wind directions in familiar acquiesce with the April . Outlines the going is in the number of calms , as crepuscle ordinary monthly wind travel is commonly little than the barrage , and weak winds are snitch here . In the congou washstand prevail low wind renovate is less than 2 m / atomic number 16 . This handbasin be explained basins terrain . In addition, the Congo basin coincides in its geographic congeal with the empyrean of high ram that is set south of the equatorial zone of calm that enhances the set of weakening the wind and puts this orbital cavity in line with the noteworthy horse latitudes , which is characterized by prevalent calm .