Tasirin Massenerhebung (Jamus don ɗaukakin hawan dutse) yana bayyana bambancin layin bishiyar bisa girman dutse da wuri. Gaba ɗaya, tsaunukan dake kewaye da manyan jeri zasu kasance suna da manyan layukan bishiya fiye da tsaunuka da ke ware saboda riƙe zafi da inuwar iska. Wannan tasirin yana da mahimmanci don tantance yanayin yanayi a yankuna masu tsaunuka, saboda yankuna masu tsayi iri ɗaya da latitude na iya samun yanayi mai zafi da sanyi sosai dangane da kewayen tsaunuka.[1]

Massenerhebung sakamako
Bayanai
Bangare na Climatology

Alal misali, a cikin Borneo, Gunung Palung, dake bakin teku, yana da gandun daji a 900 m, yayin da gandun daji na montane a Gunung Mulu ya fara a 1200m kuma a 1800m akan Dutsen Kinabalu.

Duba kuma

gyara sashe
  • Girman bambancin girman girma
  • Krummholz

Manazarta

gyara sashe
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