Waa maxay murugada ku kala horjeeda?

depression Polar - formation dabiici ah. Hababka dabiiciga ah si ay u siiyaan iyo in la garto oo isticmaalaya farriimaha caadiga saadaasha hawada sidaas ma aha mid fudud. Sidaa darteed, waxay khatar ku ah ragga baxriyiinta ah, sidayaal hawada iyo hawlaha kale ee insaanka ee gobollada waqooyiga. Sidee aan la saadaalin karin iyo murugo kala horjeeda halis ah, ugub ah, aynu talaabo talaabo ah.

History of daahfurka

depression Polar - ugub ah in loola jeedaa nidaamka cimilada ah miisaanka yar, taas oo muddo kooban ah iyo waxa lagu gartaa cadaadis hoose. Waxaa la aasaasay in ka badan badaha ee labada barka dhanka ah aagga ugu weyn ee kala horjeeda. waxbarashada Early soo jeediyay in sababta ugu weyn ee ay dhacdo - xasilooni kaamerada. Laakiin bayaankan ahaa mid aad uga fog xaqiiqda. Later waxaan bartay shuruudaha formation. Waayo, markii ugu horeysay ee noocan ah ee nidaamka dabiiciga ah waxaa laga helay oo ku images saadaasha in ay noqdaan dad lagu heli karaa 60-mada ay qarnigii la soo dhaafay.

At latitudes sare, khabiiro ku xaqiiqdii ahaa Uubo a badan oo dhan daruuraha. Waxay la ogan meelaha baraf-free kor ku soo sheegnay iyo badaha, in ka badan Labrador, iyo sidoo kale Gacanka Alaska. Waxaa la ogaaday in jabka kala horjeeda ayuuna si degdeg ah ku filan Atmospheric. asxaabta Nordic duufaanaha Antarctic badanaa taagta daran, maxaa yeelay dhan qaaradda la kulma isbedbedelka heerkulku kala duwan. In kasta oo mararka qaar xitaa gudahood Ocean Southern ah u arki karaan dhaqdhaqaaqa of this ifafaale.

images Satellite noo oggolaan in ay ku tirinnaa in jabka kala horjeeda waxa lagu gartaa noocyo kala duwan oo qaabab daruur in la abuuri karaa ka guutooyin muquuninta daruuraha dabooli xarunta ama u dhaw in ay hore kala horjeeda in ay qaataan image ee comma ah. Dhab ahaantii, waxay ku xiran tahay qaabka iyo heerka uu khatar ah ifafaale cimilada, xooga iyo xawaaraha of faafinta.

hab ay of formation

Marka hore kala horjeeda bilaabmaa ay la ruxruxo horumarka ka daadanayo enhancer lays jawi kulaylaha hawada mass soo saaray jabka kala horjeeda. La tixgaliyo nidaamka horumarinta dhinaca bari, duufaanta diiran, kuwaas oo hawada isku dayayaan in ay taqaluseyso qabow waa ka duwan yahay kan ka soo horjeeda, kuwaas oo isaga soo socota oo ka eryay hoos qorraxda diirto tacsida ah. Natiijada dhaqdhaqaaqa this yihiin xubno ka soo horjeeda noqdo hoos cadaadis at dusha sare, xarunta oo la hareereeyey by isobar dabayshii crosswise Suurka.

Sidaas darteed, hawada qubanayo in muhimka ah ee niyad-jabka iyo intii ka sii weynayd habeen faraha. Sida nidaamka this hore qabow dhawaado diiran, taas oo keenta in wajiga qabsamin. In kasta oo ay joogaan hawada heerkulka hooseeyo iyo sare ee mooshinka duufaan ah dabeecadda, tilmaamay by isobar iyo jihada dabaysha oo korka ka jira mid ka duwan hore sida line qaybinaysa u dhexeeya durdurraa ka soo socda, oo ku yaalla gobolka danbe ee niyad-jabka. Tani waxay keenaysaa in isbadal ee hore. Iyada oo ku xidhan nooca geedi socodka ee go'aaminta qabsamin Metamorphosis ciyaarta waa mid qabow ama diiran. On this ku xiran tahay muujinta dibadda oo duufaantu dhulka.

waqti Si

Inta lagu jiro jiritaanka noocan oo kale ah habka cimilada waxay ku xiran tahay sida ay u dheer tamarta laga yaabo in la beddelaa tamar ogeed. depression Polar halaagnay markay u dhaxaysa layers hawada ku yaalla xaafadda ka, farqiga u baaba'aa cadaadis hoose iyo sare. Its daciifaan degdeg ah waxay dhacdaa marka barakaca ah ee dusha barafka ama qiyaas dalka. Marka la eego xiriirka tooska ah la sara ah ee dabaylaha hawada oo xoog badan, waxay si weyn u saamayn ku yeelan karaan cimilada.

Saamaynta cimilada

Sababtoo ah hawada diiran baxdo si tartiib tartiib ah Lugbuur, ilaa iyo inta ay ka gaarayso xasiloonida, formation of foomamka daruur oo israac raacsan. Haddii daruuraha cirrus samada ka muuqdo, ka dibna dhinaca diiran hore. Sida uu ku soo dhawaaday daruuraha hoose iyo si ka sii weyn tahay. Inta badan gogosha portends roob wanaagsan ugu danbeyn beddelin roob weyn. Oo cuntadaydii horeba aynu ka filan karto samada qoraxdu goob cumulus.

Imaanshiyaha hore qabow cimilada si lama filaan ah badala. In Samooyinka waxaa jira daruuraha cumulonimbus, sida munaaraddii, keeno, sida caadiga ah, roob wanaagsan culus iyo onkodka. Si lama filaan ah, jihada dabaysha lagu beddelayba waa inay xagga woqooyi ama waqooyi-galbeed. Xaaladda duufaanka uu yeesho si lama filaan ah oo muddo gaaban.

Waa maxay farqiga u?

Waa maxay murugada ku kala duwan yihiin aad kaliga Hemisphere ka Koonfureed keligeed sida Waqooyiga? Ku dhawaad waxba, in kastoo ay jiraan waa line qaybinaysa muhiim ah. Xaaladda hore, dabaysha on hore diiran woqooyi u jeesta xagga waqooyi-galbeed, iyo dhaxanta - xagga galbeed in ay koonfur-galbeed, ee labaad - dhaqdhaqaaqa waa la mid ah sida in of War fallaadhihii on saacba. Laakiin feature in murugada kasta horjeeda - arrin qofka, taas oo ah, waxaa jira model ah la qurxiyey, kaasoo kara si aad u sharaxdo.

saadaal macquul

Si Saadaasha cimilada ee Niyadjabka kaliga laga yaabaa on shardi ah in aag aad u ballaaran daboolay by indhaynta Injiillada. Tusaale ahaan, aagga daraasadda qaarada Yurub waa in ay ballaariso galbeed, oo ay ku jiraan aagga xiga Atlantic. Maxaa yeelay, nidaamka dabiiciga ah sida caadiga ah sida ay leeyihiin xawaare ka mid ah 1000 km per maalintii. Haddii galku waa la fuliyay in sare layers of jawiga, waxay si aad ah loo fududeeyo doonaa shaqada on aragti ee waaxda, halkaas oo ay jiraan duufaanta ah.

Wax caadi ah marka murugada hore Akhristoow galay qoyska ballaaran, ku lug leh dhismaha mooshin sare agagaarka socodka ugu weyn. Kuwa ugu badan waa kuwa ka soo baxa ku laayeen oo hawada qabow. Wakiilka kasta xiga ee calaamad u ah qoyska sida ah jidka u dhaw dhulbaraha badan ururka ka horeeyey.