Tacsida Air suunka Equatorial. The zone cimilada Equatorial: sifooyinka

Aagga dhexe ee caalamka magaceeda waqooyi ilaa 11.4 digrii loolka koonfurta helay sababta oo ah goobta Equatorial labada dhinac ee dhulbaraha ka 5-8 digrii.

xagaaga weligeed ah

suunka Equatorial Limited subequatorial ka kooban tahay saddex qaybood:

• Qaarada South America, oo dhulka Amazon,
• Dhulweynaha Africa, Equatorial; Gacanka Guinea,
• Part of the Sunda Greater Islands iyo ugu dhow iyaga biyaha.

latitudes Equatorial daboolo labada qaybood ee labada qaybood ee dunida, qaba xaaladaha cimilada la mid ah ee Northern iyo barka Southern.

Waxbarashada Equatorial tacsida hawada

Inta ay kulaylka qorraxda siinayaa dusha dhulka ee - mid ka mid ah qodobada ugu muhiimsan ee saamaynta cimilada ee meel kasta on Earth. Degree ee kulaalaya dusha caalamka ee ku xiran tahay xagasha taas oo u dhaco si ay fallaaraha qorraxda ee. The u dhaw dhulbaraha, ugu weyn dusha kululaaneysa ee dhulka, sidaasna ay ku kordhiyaan heerkulka dhulka.

On dhulka ee qorraxda zone Equatorial xagal ee dhacdooyinka waa tan sarreysa, si heerkulka celceliska sannadlaha ah hawada ee gobollada Equatorial ee suunka waa 26 digrii, kala duwanaanshaha yar. tacsida Air oo ka mid ah Equatorial zone, kulul, kaca iyo abuuraa dhaqdhaqaaq sii weynayd ee durdurrada hawada.

At oogada Dhulka waxaa la aasaasay ka baxsan aaga ay cadaadis hoose - jabka Equatorial. Hawada kulul oo qoyan anigoo dhowrtid cokan oo waxaa halkaas qaboojiyey. Sidaas darteed of qaab beddelidda kaamerada socday hannaanka daruuraha cumulus, roobab qaab roobka.

Waxa asaasay in tacsida hawada zone-jabka suunka Equatorial had iyo heerkul sare. Huurka ee degaanka ayaa sidoo kale kor u kacay.

Tani waxay u gaar ah iyo Equatorial zone cimilada. Astaamaha u gaarka ah tacsida hawada mar walba la mid ah. Tan iyo markii ay loo sameeyay aagga atmosfeerta Cadaadiska kor Barriga iyo Badda, saynisyahano ah ma u qaybi nooc hoosaad badda iyo continental cimilada.

Maqaallo tacsida hawada

Awoodda tacsida hawada foomka suunka Equatorial Equatorial nooca cimilada, taas oo ah waxa lagu gartaa:

• heerkulka sare joogto ah hawada ee 24 ⁰ C ilaa 28 ⁰ C, kala duwanaanshaha yar hal sano gudahood la kala duwan ee 2-3 ⁰ C. isbedel ee xilli la dareemin, sannad xagaaga ku wareegsan ka taliso. Celceliska heerkulka in suunka Equatorial aanu is badalin sanadka gudihiisa.
• tiro badan oo roobab iyadoo labo danbow oo roob u dhiganta booska aynnnu qorraxda, iyo labada minima at solstices ah. Roobabka, laakiin u di'in.
• Itobiya roobab in suunka Equatorial, iyo tiradooda, a hoos-hoos sanad waa kala duwan ee gobolada kala duwan ee suunka Equatorial.

A cimilada caadiga ah Equatorial waa hanti si Amazon Galbeed iyo Congo Basin. In lacagta weysada Congo ee roobab Hawada ee sannadka soo of 1200-1500 mm in qaar ka mid ah meelaha 2000 mm sanadkiiba. degaanka ee gobolka Amazon ee waa aad u balaaran weysada ee Congo, tacsida hawada loo sameeyay by suunka Equatorial daran. tiro sanadlaha ah ee roobab gaaro 2000-3000 mm. Tani waa marar badan ka sarreeya heerka sanadlaha ah.

The zone cimilada Equatorial: sifooyinka cimilada

Waayo, qaybta galbeed ee geedka kokaha iyo xeebta waqooyi ee Guinea waxa lagu gartaa khasaaraha roobabka ugu badan, tirada badan karto 5,000 mm sannadkii meelo qaar ka mid ah, ilaa 10,000 mm sanadkiiba. On sida tiro badan oo roobab saamayn counter-u dhexeeya Equatorial North Hadda Jira Iyo South xoog leh. Meelahan, dhawaaqaa roobab badnaan xagaaga.

Itobiya roobab in suunka Equatorial xilliyeed kala duwan. muddo qalalan ama aan jirin, ama waxay qaadataa hal ilaa laba bilood. Farqiga weyn ee xaddiga roobabka ee xagaaga iyo jiilaalka ee gobolladan ay sabab u tahay harmattan dabaysha ganacsiga West African engegan oo boodh badan. Laga soo bilaabo dabayaaqadii November in ay goor hore March u dhabasho ka Sahara dhinaca Gacanka Guinea.

Equatorial suunka: Dabaylaha in qaabka cimilada

roobab profusion waxaa si toos ah oo la xidhiidha zone wada ah zone dabaylo ganacsiga intratropical, halkaas oo wada ee hadda hawada arkay. zone wada kordhiyay weheliyaan dhulbaraha, la kulmeen zone ee cadaadiska Hawada hoose iyo inta badan ee sanadkan ayaa ah Waqooyiga Dhulbadhaha. In xilli dhaca mowjadda zone wada socdo isbedel, ugu caan ah ee Badweynta Hindiya.

Halkan dabaylaha ganacsiga siiyaan si ay monsoon ee. dabayl Joogto, ku xiran tahay xilli, bedelaan jihada. tamarta dabaysha kala duwanaan karaan, ka itaalka daran si ay u noqdaan Dabayl. In zone this, la aasaasay intooda badan oo dhan ay duufaantaasi. latitudes Tropical waxaa lagu gartaa kar atmosfeerta.

Dabaylaha Ganacsiga iyo dabeelaha Mansoon

Waxay sameeyaan durdurrada hawada, taas oo degi aagga cadaadis hoose - dhulbaraha. Sababo la wareeg ah dhulka waqooyi ganacsan dabaylo dhow dhulbaraha qaadataa jihada woqooyi iyo keenidda koonfur-bari - South. Shirka, waxay sameeyaan xawaal - strip windless. Dabaylaha Ganacsiga - socodka hawada saboolka ah buunafuufid xusuus weheliyaan dhulbaraha sannadka oo dhan, ay waa dabayl ugu xasiloon caalamka.

Sayidka, roobab ugu badan ku dhacaa ee aagga Equatorial maalmood ka dib markii maailnta. hoos u dhac A yar in roobab arkay wakhtigii solstices ka dib. Korkiisana dhulka ee kululeeya oo iftiinka qoraxda, foomka daruuraha kooxahaasi. Sida caadiga ah gelinka dambe tago roobab culus oo ay la socdaan onkodka. Badda ku jira qubeyska iyo duufaanaha habeenkii, tani waa farqiga u dhexeeya cimilada badda iyo qaaradda.

Roobab dhaco wax badan in qoyaanka leeyahay waqti ay ku uumi. qoyaan qaraabo waa la hayaa at 80-95%. ciidda qoyan uumiga, kor u qaadida koritaanka, asked kaymo multi-nooc ah. Kor qoyan kaymaha ee Equatorial latitudes si joogto ah buunafuufid xusuus monsoon galbeed ee xagaaga iyo jiilaalka - bari, Africa, monsoon Guinea iyo monsoon Indonesia.