Afirka sauyin yanayi

Formation na singularities na Afirka sauyin yanayi ne ya rinjayi daban-daban dalilai. A ɓangaren duniya da aka located a cikin bakwai zones. Saboda gaskiya cewa line crosses da Equatorial Afirka kusan rabin, climatic zones aka maimaita su daga ekweita ga iyakoki da kuma nahiyar. Ya kamata a lura da cewa yanayi a wanda akwai samuwar yanayin, kudu da arewa na tsakiyar nahiyar suna da nasu halaye. Don babban har wannan ne saboda da cewa yankin arewa na kudancin yankin na sau biyu a yankin nahiyar. Bugu da kari, kudancin subcontinent ta'allaka tsakanin India da kuma Atlantic Ocean. Daidai da muhimmanci ne da kusanci zuwa ga Eurasian daga wanda Arewa da kuma arewa maso gabashin Afirka rabu intercontinental dumi tekuna (Rum da kuma Red). A cikin ƙasa na babban yankin ne biyu na wurare masu zafi biyu subequatorial kuma da Equatorial bel. A subtropics ne cikin matsananci arewacin da kuma matsananci kudancin Afrika.

A sauyin yanayi na bakin tekun na babban yankin kafa a ƙarƙashin rinjayar teku igiyoyin. Don arewa-yamma, gabas, kudu maso yammacin yankunan an halin da rage yawan zafi. Wannan shi ne saboda tasirin da Canary Islands (sanyi) kwarara. More moisturized ne kudu-gabashin da kuma yammacin gaba. A nan, kadan kwarara (Mozambique da kasar Guinea) shafi sauyin yanayi na Afirka.

Babban ɓangare na nahiyar ta'allaka tsakanin yammacin sahara, sabili da haka samun mai yawa na hantsi da kuma warms sama sosai, musamman a cikin mafi m da arewacin kasar. A predominance na high yanayin zafi da ke sa da sauyin yanayi na Afirka ta mafi zafi a duniya.

Wasu tadawa gefen nahiyar, idan aka kwatanta da na ciki yankin na nahiyar taimaka wa musaman "nahiyar". Wannan ne musamman ya furta a arewacin cewa shi ne saboda ta size da kuma kusanci zuwa Eurasia.

Afirka sauyin yanayi ne ya rinjayi yawanci cinikayya-iska wurare dabam dabam da kuma subtropics na biyu hemispheres Maxima.

A kan ƙasa da Sahara (a Arewacin Afrika) mamaye da bushe arewa-westerly da kuma arewa-easterly iskõki. Sun haɗu hurawa kudu-maso-yammacin monsoon, abinda ya kawo zuwa karkarar Guinea Coast da kuma Sudan, m iska da ruwan sama.

Afirka ta sauyin yanayi a gabas, a yankin na kasashen Habasha da Somalia, kafa a ƙarƙashin rinjayar India monsoon.

Kusan daukacin kudancin Afirka yanki bambanta bushe sauyin yanayi, musamman a cikin ciki yankuna. A togiya ne Cape yankin. Ga cyclonic aiki kunna ta iyakacin duniya gaba.

Babban ɓangare na nahiyar high yanayin zafi kafa a ƙarƙashin rinjayar da karfi insolation (haske) da kuma dogara a kan tsawo na solstice. A shekara-shekara talakawan zafin jiki a babban yankin na nahiyar wuce 20 ° C. Saboda gaskiya cewa na arewacin Afirka, mafi m, shi heats up more. A nan, mafi wata-wata kafaffiyar zazzabi (35-40 ° C) da kuma matsakaicin kullum zazzabi, zana a duniya (zuwa 58 ° C).

"Continental" sauyin yanayi bayyana kanta cikin Afirka. An bayyana yawanci a gagarumin diurnal zazzabi bambancin. Alal misali, a cikin Sahara mawadãta iya isa hamsin digiri.

A sauyin yanayi a Afirka yana da wani musamman m rarraba hazo. A Equatorial ɓangare na yau da kullum da fall m ruwa sama sosai. Matsakaicin ruwan sama ya faru a kan gangara na Kamaru tsararru.

Don kudu da arewa na kasar Equatorial band na ruwan sama fadowa saboda da tasiri na monsoon. Su duka shekara-shekara Figures ne sosai daban-daban dangane da topography kuma Gwargwadon wuri.

Zuwa matsananci kudu da matsananci arewa na nahiyar da tsarin kula da subtropical bel adadin ruwan sama ƙaruwa.