Waa maxay zone-sare sare? Altitude sharxi Eurasia

Dad yar dugsiga xusuusan, waxa sare u sharax. Aragtidani waxa ay ku sharaxayaa isbedelka sida aad u guurto ilaa sifooyinka cimilada ee dhismaha ka mid ah gargaarka, oo sideeda oo ciidda dhagax, iyo sidoo kale dhirta iyo ugaarta. Laakiin sabab u sababaha qaar ka mid ah, sida macluumaad aan sax ahayn oo ku saabsan qayb kasta, dhul zone-sare sare waxa lagu gartaa-beegyada uu ugu sax qiyaasay, cimilada iyo geomorphic.

Dhirta iyo waxyaalo kale oo ah in ay sameeyaan aag-sare sare

Inkastoo daaqsinka ah (in kasta oo isaga kooxdiisana waxaa ku joogto oo firfircoon ee degaanada) ma aha in kiisaska oo dhan, oo muujinaya gobolka of total caqabad casri ah si ay arrimo dhowr ah, waa in aan detract ka muhiimadda ay leedahay in formation of fikrado ku saabsan waxa a zone-sare sare.

Sababtan awgeed, ururka caadiga ah ee meelaha degaanka Dhirta kala duwan ee meelaha gargaarka waxaa loo arkaa inay la aqbali karo oo macquul ah. The sifooyinka qaybaha ka - Dhirta, oo sideeda oo ciidda, cimilada, dubato, iyo lafaguro in muuqaalka guud ee waxa loo qaybin karaa aag of zones altitudinal. Waayo, nidaamka buurta kala duwan, ay kala yara duwan yihiin. Gaar ahaan, zone-sare sare buuraha Ural ku kala duwan goobaha sare Tibet. Si aad u si fiican oo kalsooni leh muuqaalka ee aagga kala qaybiyaan, waxaa lagama maarmaan ah in loo qoondeeyo total calaamada variable.

Sababaha goobaha altitudinal

In la barbardhigo bannaankii, ee dhulka sare ee kala duwan ee noocyada badan tahay - in 2-5 jeer. Laakiin waa maxay sababta oo ah "-dheer" ee goobaha dabiiciga ah ee dhulka sare ee?

Sababaha ugu weyn - taasi waa height of buuraha, oo ay juqraafi ahaan dhacdo. goobaha dabiiciga ah beddelo qiyaastii la mid ah sida marka aad wadid gaari bannaanka xagga koonfureed iyo ilaa xagga woqooyi. Si kastaba ha ahaatee, marka wadista buurta dhul isbeddelkan la taaban karo iyo waxa ay dhacdaa Joogga yar.

suunka High-sare ee jooga ugu weyn tirada ee latitudes kulaylaha. In band Arctic goobada ee buuraha height isku mid ah tirada yar ee goobaha sida.

cimilada ee buuraha

saarridda Altitudinal buuraha ku kala saari Karin xidhiidh la cimilada. All zone-dhaadheer daboolayaa buuraha dhinac kasta, laakiin ma at dhan heerarka isku istaajineyso ka soo horjeeda. At cagta ee buuraha cimilada uu yahay mid ka badan oo la mid ah xaaladaha cimilada ku xeeran bannaanka. Kor heerarka ugu badan yihiin dhexdhexaad ah, ka dibna hawada ku filan u daran. At sare ee waxaa jira zone ah oo jirkiisa iyo baraf. Iyo, sida, oo u dhaw in ay Sun - si, in aragtida, diiran, laakiin dhab ahaan ma aha.

In kasta oo ka reeban dhici, sidoo kale. Tan waxay cadeyneysaa in zone sare - ma arrin hal mar ah, oo waxay ku xiran tahay arrimo badan. In Siberia, waxaa jira meelo halkaas oo cimilada uu yahay mid aad u adag at cagta ka badan on dhaadhacyadii. Tan waxa u sabab la'aanta ah ee wareegga hawada ee hogag buuraha u dhexeeya.

Maxaa calaamad zone-sare sare ee Eurasia ah?

The buuraha xagga koonfureed u dhaw, ugu weyn tirada iyo noocyo kala duwan oo ka mid ah goobaha sare. Urals - mid ka mid ah hababka ugu buurta wakiil.

In qaybta koonfureed ee zone-sare sare ee Mountains Ural ah leedahay in ka badan heerarka badan ee waqooyiga, inkastoo xaqiiqda ah in buuraha koonfurta hoos. In qaybta waqooyi waxaa jira oo kaliya suunka buur-Dhuldhoobo.

xeebta Badda Madow iyo gobolka Amur-Sakhalin

Xitaa inta badan sameysa goobaha la barbardhigo on xeebta Badda Madow ee Caucasus. Just saacad iska baabuur, waxaad tagi kartaa xeebta fareen of Sochi for cimilada sub-Alpine of Caucasus Western ah.

In aagga Amur-Sakhalin soo jireenka ah ee gobolladiisa oo calaamad ka mid ah oo dhan - strips qaab-dhismeedka muuqaalka. Waxay kala qaybsan yihiin:

• gornotundrovuyu;
• podgoltsovy - kedrovnikah baxda, kaynta dhif Ajan gran, laakiin sidoo kale darajooyin kala duwan ee bjørk dhagax-fiirsashada.

In koonfurta Sikhote-Caalin oo dhan sifooyinka caadiga ah oo ka mid ah goobaha altitudinal Amur.

heerarka dheeraad ah waa kuwan soo socda: strip yar yahay buuraha (kaynta geed kedar la yidhaahdo oo la caleemo ballaaran oo iyaga ciidda sameeyey, iyo cimilada) band Mid (kaymaha dhirta dhilka iyo dhiganta dusha dahsoon), strip bidaarta (isku dar ah conifer Proleski, kedar ah koritaanka cufan Slanic, geedihii Asheeraah bjørk dhagax) strip Goltsovoye laftiisa, oo Dhuldhoobo qaab saafi ah.

Haddii cimilada sii qaaradda, in nidaamka noocan oo kale ah waxaa lagu daray kaymaha kaymo. In buuraha galbeed ee wakhtiyada joogo South Sikhote-Caalin waa buurta ku xoortay geedihii podgoltsevyh strip Dhuldhoobo (ama gurguurta kaymaha buur), guutadii Erman Qallooc, kaymaha suunka beroosh ah gran (gran), suunka kaynta broadleaf-geed (kaymaha geed), suunka kaymaha kaymo iyo kaynta suunka .

tiirsanaanta ee timberline iyo meelaha buurta

Si aad u taariikhda, caddadka wxbarashada badan xogta ku saabsan sida sare waa xadka sare ee strip kaynta koonfurta Sikhote-Caalin ah. xadka meelaha Ilodanimada abuuray sare on dushooda alwaax gaar ah iyo dhaadhacyadii kala duwan oo la mid ah, waxay qaadanaysaa qiimaha ku filan oo waaweyn iyo gaadho in ka badan 300 oo mitir vertical.

Good arrimuhu guud dareemi la kordhiyo dhaadheer ee sare ee xadka sare ee kaynta waa sidoo kale kor wareejiyay (saamaynta height of isugu soo diyaariyeen ah). Si kastaba ha ahaatee, inkasta oo buuraha iyo fog badda ka jira fogaan ah ee kala duwan oo ka soo 15 ilaa 105 kilomitir, saamiga u dhexeeya height of line alwaaxdiisa iyo Cardiff oo ku dhowaad waa isku mid u ah xannibaad kasta. Natiijada Tani ma aha mid aad u macquul ah, oo filan, oo sidaas daraaddeed waxay u baahan tahay sharaxaad no.

Incoherence muuqato in xaqiiqda ah in tiro this gacansaydhay saameyn weyn badda on jagada xuduud sare ee kaynta. Si aad u noqoto more sax ah, gudahood xuduudaha saamaynta badda South Sikhote-Caalin waxaa dareemay in ay goobaha sare xoog qiyaastii siman. Taasi waa, zone-sare sare ee Eurasia sidaas ma aha ku tiirsan tahay helitaanka badaha.

Haddii kale, Joogaba, sida waayo dushooda buurta xeebta ee latitudes (Hualaza-Litovka, Pidan-Livadijsky, Tavayza-Brusnichnaya) looma baahna noqon sida weyn. Halkan saamayn ku saamaynta on xuduud sare ee meelaha kaynta of kala duwan oo buurta ka. Iyadoo la tixraacayo sifo this waxaa loo qoondeeyey Cloud Mountain oo kaliya, ugu sarreysa ugu sareeya ee Koonfurta Sikhote-Caalin.

Si ay u sharxaan this ifafaale laba siyaabood: midkood isugu soo barta dheer yahay in heerkulka marinka qeexaya alwaax gaareen height a ugu badan ee gobolka, ama ka soo jeeda gobolka nuqdad la Xagiisaana Geeduhu ka xadka cimilada sare ayaa loo habeeyey daraa. Qaybaha of zones altitudinal soo jireenka ah ee karamberriga buurta, waxaa sidoo kale lagu gartaa dushooda qayb ka mid ah xeebaha iyo xagga koonfureed iyo Dhexe Sikhote-Caalin, sida lagu muujiyey by a kaymaha buurta sare ee kaymaha geedkii.

zone High-sare - ifafaale gaar ah ee dabiiciga ah

In si ay u jawaabaan su'aasha ah, waxa zone-sare sare ee, waa in mid ka mid fahamsanahay in tani ay tahay arrin aad u gaarka ah in arigtida shuruucda caalamiga ah. Waxaa jira arrimo badan oo shakhsi ah oo keeni horumarinta a cimilada, nooca Dhirta iyo xoolaha. Aqoonta aagga this ka muuqan sabab u cilmi Nidaamsanaan badan. Beddelidda loolka saamaysaa heerka isbedelka ee maalintii iyo habeenkii, iyo sidoo kale gumaysiga cimilada xilliyeed. Dhammaan macluumaadka kor ku xusan, si kastaba ha ahaatee, ma cad loo sharaxo waxa zone-sare sare. In kooban - isbedel goobaha cimilada la sii kordhaya height of buuraha.