Qoondaynta, noocyada iyo roobab cimilada. Cimilada iyo noocyada roobabka

Noocyada roobab cimilada waa in la tixgeliyaa oo xidhiidh dhow la leh fikradda ah "cimilada". Waa walxahaasi waa aasaasiga ah haddii aan u fiirsada xaaladaha gobolka gaar ah.

Erayga "cimilada" The waxaa loogu tala galay xaalad ah jawiga at meel gaar ah. Formation of the nooca cimilada, joogto waxay ku xiran tahay arrimo badan, oo waxay leeyihiin sharciyo u gaar ah ka muuqan. The xaaladaha isku mid ah oo aan la ogaan karaa meelaha qaarkood. Noocyada roobab cimilada kala duwan on dhammaan qaaradaha ee dunida dacaladeeda.

Cimilada saamayn ku yeelan karaan waxyaabo sida shucaaca qoraxda, cadaadiska Hawada, qoyaan iyo heerkulka, roobab, jihada dabaysha iyo xoog, cloudiness, gargaarka.

cimilada

Muddada dheer cimilada - waa cimilada. saamaynta A weyn ku dul Eebay xaddiga kulaylka qoraxda galaya dusha dhulka ee. tiradaasi ku xiran tahay height ee qorraxda duhurkii - lool. Qadarka ugu weyn ee kulaylka qoraxda helay at dhulbaraha in ay ulaha laga gelin lahaa, qiimaha this hoos.

Sidoo kale waa arrin ugu muhiimsan ee saamaynta cimilada, waa u hesheen sidii labada dhinac ee dhulka iyo badda, taas oo kuu ogolaanaya in aad loo qoondeeyo noocyada badda iyo continental ee cimilada.

Marine (Oceanic) sifo cimilada ee badda, jasiiradaha iyo qaybo ka mid xeebaha qaaradda. Noocaan wuxuu ka soo jireenka ah isbedbedelka sanadlaha yar maalin ah ee heerkulka hawada iyo qadar weyn oo roobab atmosfeerta.

cimilada Continental lagu gartaa goobaha qaaradda. Tusiyaha dhulweynaha qaaradda ku xiran tahay celceliska isbedbedelka heerkulka hawada sannadlaha ah.

Arrin kale oo saamayn ku xaaladaha cimilada, waxaad wici kartaa badda hadda ka. tiirsanaanta Tan waxaa lagu muujiyey in wax isbedel ah oo heerkulka hawada mass. Waxay leeyihiin qof u gaar ah sida roobka iyo cimilada u dhow badda.

Waa heerkulka hawada - factor ee soo socda, kuwaas oo saameyn ku cimilada iyo cimilada lama quudhsan karin. Isbedelka xaaladaha abuuro dhaqdhaqaaqa kaamerada of cadaadiska hawada, la xirrira zone cadaadiska Hawada sare iyo hoose. Ayaa sheegay in goobaha wareejiyo mass hawada. The dabiiciga ah kala kulantay mass kala duwan hawada foomamka hore Hawada, taas oo ah waxa lagu gartaa cloudiness, roobab, xawaaraha dabaysha oo sii kordhaya isbedelka heerkulka.

dhexgalka A adag oo ka mid ah qodobada kor ku xusan foomamka ee dhulalka noocyo ka mid ah xaaladaha cimilada.

Qoondee noocyada kuwaas oo cimilada: Equatorial, monsoon kulaylaha, qalalan kulaylaha, Mediterranean, qalalan dadka fareen, badda qoraxda, qaaradeed, monsoon oo iscelin dhexdhexaad ah, subarctic iyo cidhifka woqooyi ama Antarctic.

noocyada cimilada. Sharax kooban dhammaan noocyada kala duwan ee cimilada

nooca Equatorial waxa lagu gartaa heerkulka sanadle ah celceliska gudahood + 26˚S, wax badan oo roobab sanadka oo dhan, heysatay by tacsida diiran oo qoyan hawada iyo qaybiyey gobollada Equatorial of Africa, South America iyo Oceania.

Noocyada roobab waa si toos ah ay ku xidhan tahay gobolka. Hoos waxaa ku qoran waxaanu ka fiirsan noocyada cimilada, taas oo ah waxa lagu gartaa jawi kulaylaha.

Noocyada cimilada kulaylaha

Weather adduunka oo dhan waa wax kala duwan. Tropical nooca cimilada monsoon leedahay sifooyinka soo socda: heerkulka ee January - + 20 ° C, in July - + 30ºC, 2000 roobab mm, heysatay by dabeelaha Mansoon. Waa baahsan Koonfurta iyo South-East Asia, West iyo Bartamaha Africa, Northern Australia.

cimilada qalalan Tropical lagu gartaa heerkulka January + 12˚S, July - + 35 ° C, roobab yar gudahood 200 mm, dabaylaha ganacsiga adkaan. Qaybiyey North Africa, Central Australia.

nooca Mediterranean ee cimilada la garan karo by xuduudaha soo socda: heerkulka ee January + 7s, ee July + 22˚S; 200 roobab mm inta lagu jiro xagaaga marka cadaadiska sare Hawada jirta Anticyclones ee xilliga qaboobaha - duufaanaha. Qaybiyey by cimilada ee Mediterranean ee Mediterranean, South Africa, Southwest Australia, Western California.

akhrinta heerkulka kala duwan oo qalalan fareen cimilada ka 0s ee January si + 40 ° C ee July, iyadoo noocan ah roobabka cimilada kama badna 120 mm in jawi qalalan heysatay mass hawada qaaradda. Dhulka faafidda noocan oo kale ah xaaladaha cimilada - qaybaha gudaha ee qaaradood ah.

cimilada badda qoraxda waxa lagu gartaa tilmaamayaasha sida heerkulka ka + 2 ° C si + U17, roobab Hawada heerka of 1000 mm, waxaa lagu gartaa dabaylo galbeed. Waxa uu siidaayey territory oo ka mid ah qaybaha galbeed ee Eurasia iyo North America.

cimilada qaaradda Dhexdhexaad muujinaysaa farqiga weyn a heerkulka xilliyeed: -15˚S - + 20 ° C, roobab gudahood 400 mm, iyo baahsanaanta ee dabaylo galbeedka on meelaha ugu hooseeya qaaradood.

monsoon Dhexdhexaad muujinayaa kala duwanaanta fiiqan ee heerkulka -20˚S laga bilaabo Janaayo ilaa July ee + 23 ° C, roobab at 560 mm, joogitaanka iyo jiritaanka bari monsoon Eurasian.

Marka heerkulka nooca sub-Arctic cimilada waa in kala duwan ee ka -25˚S in +8 ° C, roobab - 200 mm, meel ku badan yihiin monsoon jawi - Eurasia iyo North America.

nooca Arctic (Antarctic), taas oo ay jiraan heerkul hoose - -40˚S - roobab 0s yar - 100 mm Anticyclones - qaybiyey zone qaaradda Australia iyo badweynta Arctic ah.

Waxaan baaritaan nooc ah, ka jirta meelaha waaweyn, qeexaa sida deegaanka Dhaqale. Waxa intaa dheer in kuwan meso- si fiican u bartay iyo microclimates oo saamayn meelaha yar qaba xaaladaha cimilada deggan.

The kala bixiyc ugu muhiimsan ee go'aaminta noocyada cimilada waa sifooyinka oo tayo iyo tiroba dhacayay meel siiyey roobabka.

Roobab iyo noocyada ay. Weather iyo Cimilada fikradda

The Earth ee cimilada ma aha labis, oo aan door la soo dhaafay in this ciyaaray by dhac tayo iyo tiro ahaanba in roobab badan dhulka. Sababaha on taas oo ay ku xiran tahay, go'aan ka Bannaanka. Noocyada roobab ku xiran tahay arrimaha soo socda: foomka jirka, meel ka mid ah waxbarashada, nooca khasaare, meesha asal ahaan.

Ha ka fikiro si aynu kasta oo arrimaha.

Sifooyinka jirka roobabka

Noocyada roobab waxaa loo kala saaraa sida ay gobolka jirka:

1. Liquid, oo ay ka mid ah meelsare oo roobka.
2. Solid - waxaa ka mid ah barafka, cereals, roobdhagaxyaale.

• dhibco biyo ah - roobka. Waa nooca ugu badan ee roobabka ku dhacaa, ka cumulonimbus iyo daruuraha Nimbostratus.
• Meelsare oo loo yaqaan dhibco cqaadir ee qoyaanka ka ballaciisu yahay ee dhowr boqol ah millimeter ah, boos ka stratus ama ceeryaan cufan at heerkulka kor ku eber.
• Foomka dega ee ku harta adag waxaa barafka, noocyada kaas oo waxaa loo arkaa barafka iyo barafka badar isku dhaceen marka heerkulku hooseeyo.
• Goon - nooc kale oo ka mid ah harta adag ee foomka of Qurub baraf size of 5-20 mm. Noocan roobabka, inkasta oo ay qaab-dhismeedka dhaco xilli diiran.

Saamaynta xilliyada on xaalladda jireed ee roobab

Iyada oo ku xidhan roobab xilli uu hoos u dhaco foomamka qaarkood. Muddo diiran waxa lagu gartaa noocyada soo socda: roob, meelsare, sayaxa, roobdhagaxyaale. In cimilada qabow, baraf suurto gal ah, grits, dhaxan, dhaxan, baraf.

Qoondaynta oo ah roobab ku xiran tahay meesha waxbarashada

In sare layers of jawiga loo sameeyay roob, meelsare, roobdhagaxyaale, oo shaciir ah, baraf cad.

On dhulka ama meel u dhow dhulka ku - sayaxa, dhaxan, baraf meelsare ka.

dabeecadda roobab Hawada

By dabiiciga ah ee roobab Hawada loo qaybin karaa drizzling roobka iyo gundhig, baahsan. Ay dabiicadda xidhan tahay qodobo badan.

Drizzling roobka waa dheer oo ay xoogga yar, oo culus lagu gartaa xoojinta sare, laakiin muddo gaaban, waxaa gundhig, xoojinta sugeysayna baahsan oo aan isbedbedelka lama filaan ah.

Dabeecadda iyo lacagta roobabka, dabcan, saamayn ku xaaladaha cimilada meel gaar ah, taas oo iyana saamayn ku cimilada guud. In kulaale, tusaale ahaan, roob lagu arki karaa oo kaliya dhowr bilood sannadkii. Inta kale ee qorraxda dubista.

roobab cimilada

noocyada cimilada iyo roobabka hawada si toos ah ee la xiriira midba midka kale. Arrimaha saamayn qaybinta baraf iyo roob, waa heerkulka, dhaqdhaqaaqa tacsida hawada, gargaarka iyo hadda badda.

Equatorial zone cimilada waxa lagu gartaa roobabka ugu sarreeya dunida oo. Dhab ahaantii Tan waxa u sabab ah heerkulka sare iyo huurka hawada sare.

Qaybsan lamadegaanka qalalan iyo noocyada cimilada kulaylaha qoyan. cimilada adduunka ayaa ayaa roobab dhexdhexaad ah, kuwaas oo ah gudahood 500-5000 mm.

nooca Monsoon waxa lagu gartaa roobab sare, ka soo badda. Shuruudaha cimilada halkan leeyihiin periodicity.

Arctic waa miskiin in precipitates ay sabab u tahay jiritaanka heerkulka Hawada hooseeyo.

On ku salaysan meel ka soo jeedo ee cayn kasta oo roobab cimilada waxa loo qaybin karaa:

• convection, oo intaba meelaha ay cimiladu kulushahay, laakiin waxay noqon karaan meelaha ay iscelin kara;
• hore, la aasaasay at shir laba tacsida hawada ee heerkulka kala duwan, waxay caan ku tahay noocyada qoraxda iyo qabow cimilada.

Si Loo soo kobo

cimilada, sifooyinka dhulka cimilada iyo noocyada roobab - fikradaha aasaasiga ah in aan dib u eegay. Iyadoo ku saleysan waxaan dhihi karaa in Earth - waa nidaam weyn, element kasta oo taas oo ah in ku tiirsanaanta toos ah ama dadban on dadka kale. Tani fahamka arrinta sharciyeynta isticmaalka hababka isku dhafan in ay tixgelisaa cimilada iyo noocyada roobab sida gudbikaraa oo xiiso sayniska. Kaliya leh daraasad dhamaystiran oo arrimahaasi waxay noqon kartaa si aad u hesho jawaabaha saxda ah su'aalaha of saynisyahano ah.

Roobab, jawiga, cimilada iyo cimilada - fikradaha oo dhan waxay xidhiidh dhow la. In waxbarashada ay tahay wax aan macquul aheyn in xitaa seegi mid qeybaha ka mid ah.