Yanayi na Alps

Yanayin tsaunukan tsaunuka shine yanayin,ko matsakaicin yanayin yanayi na tsawon lokaci, na ainihin yankin tsakiyar tsaunukan Turai. Yayin da iska ke tashi daga matakin teku zuwa manyan yankuna na sararin samaniya yanayin zafi yana raguwaTasirin yanayin tsaunin tsaunuka akan iskar da ke tafe shine tilasta iska mai ɗumi daga ƙananan yanki zuwa wani yanki na sama inda yake faɗaɗa cikin girma akan farashin daidaitaccen asarar zafi, sau da yawa tare da hazo na danshi a cikin nau'in dusar ƙanƙara,ruwan sama.ko ƙanƙara.

 Yanayi azaman aikin ɗagawa 
Domin iska tana yin sanyi yayin da take tashi, yanayin tsaunukan tsaunuka ya dogara da tsayin daka.Tsaunukan Alps sun ƙunshi nau'o'in yankuna daban-daban na yanayi, ta tsayi. Waɗannan yankuna za'a iya kwatanta su ta hanyar rarrabuwar yanayi na Köppen,kuma sun dace da yankunan biotic na Alps.

Har zuwa kusan  na haɓakawa, an rarraba yanayin a matsayin teku ko Cfb a ƙarƙashin tsarin Köppen.Rubel, Franz; Brugger, Katharina; Haslinger, Klaus; Auer, Ingeborg (January 24, 2017). "The climate of the European Alps: Shift of very high resolution Köppen-Geiger climate zones 1800–2100". Meteorologische Zeitschrift. 26 (2): 115–125.Kamar yawancin yankunan arewacin Turai, lokacin rani yana da laushi kuma lokacin sanyi yana da sanyi,amma ba sanyi ba.Ana daidaita yanayin yanayi ta kusanci zuwa Tekun Atlantika.Yanayin ya haifar da yankin ƙwayoyin cuta na colline acikin ƙananan wurare,wanda ke da yanayin dazuzzukan dazuzzuka na gandun daji na Yammacin Turai .Tsakanin kusan ,yanayin yana canzawa zuwa ko dai yanayi mai ɗanɗano na nahiyar(Dfb ƙarƙashin tsarin Köppen),ko yanayin teku na Cfc, ya danganta da wurin.Rubel, Franz; Brugger, Katharina; Haslinger, Klaus; Auer, Ingeborg (January 24, 2017). "The climate of the European Alps: Shift of very high resolution Köppen-Geiger climate zones 1800–2100". Meteorologische Zeitschrift. 26 (2): 115–125.Yayin da tsayin daka ya karu, lokacin sanyi ya zama sanyi kuma lokacin zafi ya zama guntu. Cakuɗa da bishiyoyin conifer da ciyayi sun mamaye wannan yanki na montane, yana haifar da canji na ecoregion zuwa Alps conifer da gauraye gandun daji.

Tsakanin kusan ,yanayin ya zama subctic (Dfc a ƙarƙashin tsarin Köppen),tare da gajeren lokacin rani.Rubel, Franz; Brugger, Katharina; Haslinger, Klaus; Auer, Ingeborg (January 24, 2017). "The climate of the European Alps: Shift of very high resolution Köppen-Geiger climate zones 1800–2100". Meteorologische Zeitschrift. 26 (2): 115–125. Gajeren lokacin girma yana canza dajin ya zama nau'i ne kawai.A kusan , yanayin ya zama sanyi sosai don tallafawa bishiyoyi, kuma an rarraba shi azaman yanayi mai tsayi (ET a ƙarƙashin tsarin Köppen). Rubel, Franz; Brugger, Katharina; Haslinger, Klaus; Auer, Ingeborg (January 24, 2017). "The climate of the European Alps: Shift of very high resolution Köppen-Geiger climate zones 1800–2100". Meteorologische Zeitschrift. 26 (2): 115–125.Lokacin bazara ya zama sanyi kuma kawai ciyawa da ƙananan tsire-tsire suna dacewa don girma.Wannan yanayi mai tsayi ya kai kusan .

Sama da kusan , yanayin yana canzawa zuwa yanayin ƙanƙara, inda matsakaicin zafin jiki koyaushe yana ƙasa da .A wannan tsaunukan, babu tsiro da zai iya girma kuma ƙasa ko dai dutsene ko kankara.Rubel, Franz; Brugger, Katharina; Haslinger, Klaus; Auer, Ingeborg (January 24, 2017). "The climate of the European Alps: Shift of very high resolution Köppen-Geiger climate zones 1800–2100". Meteorologische Zeitschrift. 26 (2): 115–125.

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