Yanayin yanayi

Rabe-raben yanayi tsari ne da ke rarraba yanayin duniya. Rarraba yanayi na iya daidaitawa tare da rarrabuwar halittu, saboda yanayin shine babban tasiri ga rayuwa a yanki. Ɗaya daga cikin mafi yawan amfani da shi shine tsarin rarraba yanayi na Köppen wanda aka fara haɓaka a cikin 1884. ^[1]

Akwai hanyoyi da yawa don rarraba yanayin yanayi zuwa gwamnatoci iri ɗaya. Asali, an ayyana yanayin yanayi a tsohuwar Girka don bayyana yanayin ya danganta da latitudes na wuri. Hanyoyin rarrabuwar yanayi na zamani za a iya raba su gabaɗaya zuwa hanyoyin kwayoyin halitta, waɗanda ke mai da hankali kan abubuwan da ke haifar da yanayi, da hanyoyin haɓaka, waɗanda ke mai da hankali kan tasirin yanayi. Misalan rarrabuwar kwayoyin halitta sun haɗa da hanyoyin da suka dogara da mitar nau'ikan nau'ikan iska daban-daban ko wurare a cikin rikicewar yanayi na synoptic. Misalan rarrabuwar kawuna sun haɗa da yankunan yanayi da aka ayyana ta taurin tsire-tsire, evapotranspiration, ko ƙungiyoyi tare da wasu kwayoyin halitta, kamar a yanayin rarrabuwar yanayi na Köppen. Rawancin gama gari na waɗannan tsare-tsare na rarrabuwa shine cewa suna samar da iyakoki daban-daban tsakanin shiyyoyin da suka ayyana, maimakon sauyin yanayi a hankali a hankali.

1. ↑ Beck, Hylke E.; Zimmermann, Niklaus E.; McVicar, Tim R.; Vergopolan, Noemi; Berg, Alexis; Wood, Eric F. (30 October 2018). "Present and future Köppen-Geiger climate classification maps at 1-km resolution". Scientific Data (in Turanci). 5: 180214. Bibcode:2018NatSD...580214B. doi:10.1038/sdata.2018.214. ISSN 2052-4463. PMC 6207062. PMID 30375988.