Duba wurin da ke ƙasa sannan ka amsa tambayar daga baya a cikin harshe ɗaya kamar yadda wurin yake:  Passage: Yanayin Australiya yana da tasirin tasirin tasirin teku, gami da Dipole na Tekun Indiya da El Niño <unk> Southern Oscillation, wanda ke da alaƙa da fari na lokaci-lokaci, da kuma tsarin ƙarancin yanayi na yanayi wanda ke haifar da guguwa a arewacin Ostiraliya. Wadannan abubuwan suna haifar da ruwan sama ya bambanta sosai daga shekara zuwa shekara. Yawancin arewacin ƙasar suna da yanayin zafi, galibi ruwan sama na bazara (monsoon). Yankin kudu maso yammacin ƙasar yana da yanayin Bahar Rum. Yankin kudu maso gabas daga yanayin teku (Tasmania da Victoria na gabar teku) zuwa yanayin zafi mai zafi (babban rabin New South Wales), tare da tsaunukan da ke nuna yanayin alpine da subpolar na teku. Cikin gida ya bushe zuwa semi-arid. Dangane da Bayanin Yanayin Australiya na Ofishin Meteorology na 2011, Ostiraliya tana da ƙananan yanayin zafi a shekara ta 2011 sakamakon sakamakon yanayin La Niña; duk da haka, "Matsakaicin shekaru 10 na ƙasar yana ci gaba da nuna yanayin ƙaruwa a cikin yanayin zafi, tare da 2002<unk>2011 mai yiwuwa ya kasance a cikin manyan lokutan shekaru 10 mafi zafi da aka rubuta a Australia, a 0.52 ° C (0.94 ° F) sama da matsakaicin lokaci mai tsawo". Bugu da ƙari, 2014 ita ce shekara ta uku mafi zafi a Ostiraliya tun lokacin da aka fara lura da yanayin zafin jiki na kasa a 1910. Ana amfani da ƙuntataccen ruwa a yankuna da biranen Ostiraliya da yawa don magance ƙarancin rashin ƙarfi saboda ƙaruwar yawan jama'ar birane da fari. A cikin yawancin nahiyar, manyan ambaliyar ruwa a kai a kai suna bin tsawan lokacin fari, suna fitar da tsarin kogin cikin gida, ambaliyar dam da ambaliyar manyan filayen ambaliyar cikin gida, kamar yadda ya faru a duk Gabashin Ostiraliya a cikin 2010, 2011 da 2012 bayan fari na Australiya na 2000s.  Tambaya: Wane irin yanayi ne ya fi yawa a kudu maso yammacin ƙasar?
Yankin Bahar Rum