Tasirin canjin yanayi

Sakamakon canjin yanayi ya bambanta a cikin lokaci da wuri. Har zuwa yanzu Arctic ya yi zafi da sauri fiye da sauran yankuna saboda sauyin yanayi. Yanayin iska a saman ƙasa ya karu da kusan sau biyu fiye da yadda suke yi a kan teku, wanda ke haifar da raƙuman zafi masu tsanani. Wadannan yanayin za su daidaita idan aka kawo iskar gas mai guba. Gilashin kankara da tekuna suna shan yawancin zafi mai yawa a cikin yanayi, suna jinkirta tasirin a can amma suna sa su hanzarta sannan su ci gaba bayan yanayin zafi ya daidaita. Hawan matakin teku wani damuwa ne na dogon lokaci a sakamakon haka. Sakamakon dumama teku ya hada da raƙuman ruwa, rarraba teku, deoxygenation, da canje-canje ga raƙuman teku. : 10 Tekun kuma yana da ƙarancin ƙwayoyin cuta yayin da yake shan carbon dioxide daga yanayi.
Yanayin yanayin da sauyin yanayi ya fi fuskantar barazana nan da nan suna cikin tsaunuka, da murjani reefs, da kuma Arctic. Yawan zafi yana haifar da sauye-sauyen yanayi a wuraren da suka wuce karfin dabbobi don daidaitawa. Nau'o'in suna tserewa zafi ta hanyar ƙaura zuwa sandunan kuma zuwa ƙasa mafi tsayi lokacin da za su iyahttps://www.bbc.com/hausa/topics/c7zp510jdzpt. Hawan ruwan teku yana barazana ga wuraren dausayin bakin teku da ambaliya. Rage danshin ƙasa a wasu wurare na iya haifar da kwararowar hamada da lalata yanayin halittu kamar dajin Amazon:9 A 2 °C (3.6 °F) na ɗumamar, kusan kashi 10% na nau'in ƙasa za su kasance cikin haɗari sosai. 

 Canje-canje a cikin zafin jiki 
Warming na duniya yana shafar dukkan sassan tsarin yanayi na Duniya. Yanayin duniya ya tashi da   . Masana kimiyya sun ce za su kara tashi a nan gaba. Canje-canje a cikin yanayi ba daidai ba ne a duk faɗin Duniya. Musamman, yawancin yankunan ƙasa sun yi zafi da sauri fiye da yawancin yankunan teku. Arctic yana dumama da sauri fiye da sauran yankuna.Lindsey, Rebecca; Dahlman, Luann (28 June 2022). "Climate Change: Global Temperature". climate.gov. National Oceanic and Atmospheric Administration. Archived from the original on 17 September 2022. Yanayin zafi na dare ya karu da sauri fiye da yanayin zafi na rana. Tasirin a kan yanayi da mutane ya dogara da yadda duniya ke dumi. 

 Yanayi 

Yanayin ƙasa da na tsakiya, inda kusan duk yanayin ke faruwa, suna dumama saboda tasirin greenhouse. Rashin ruwa da yanayin zafi suna ƙaruwa yayin da yanayin zafi ke ƙaruwa. Rashin ruwa iskar gas ce, don haka wannan tsari shine ra'ayi mai ƙarfafa kansa.

Rashin ruwa mai yawa kuma yana shiga cikin hadari. Wannan ya sa su zama masu ƙarfi, babba, kuma mai yiwuwa na dogon lokaci. Wannan kuma yana haifar da ruwan sama da dusar ƙanƙara don zama masu ƙarfi kuma yana haifar le ƙarin haɗarin ambaliyar ruwa. Ƙarin bushewa yana kara tsananta yanayin bushewa da fari. Wannan yana ƙara haɗarin raƙuman zafi da gobarar daji.Trenberth, Ke (2011). "Changes in precipitation with climate change". Climate Research. 47 (1): 123–138. Bibcode:2011ClRes..47..123T. doi:10.3354/cr00953. Masana kimiyya sun gano ayyukan ɗan adam a matsayin dalilin yanayin yanayi na baya-bayan nan. Yanzu suna iya kimanta tasirin canjin yanayi a kan abubuwan da suka faru na yanayi mai tsanani ta amfani da tsari da ake kira ƙaddamar da abubuwan da suka shafi yanayi mai tsanani. Misali irin wannan binciken na iya duba bayanan tarihi don yanki kuma ya kammala cewa takamaiman guguwar zafi ta fi tsanani saboda canjin yanayi. Bugu da kari, sauye-sauyen lokaci na farkon kakar, an bayar da rahoton canje-canje a tsawon lokacin kakar a yankuna da yawa na duniya.Hekmatzadeh, A.A., Kaboli, S. and Torabi Haghighi, A. (2020) New indices for assessing changes in seasons and in timing characteristics of air temperature. Theoretical and Applied Climatology, 140, 1247–1261. .Aksu, H. (2022). A determination of season shifting across Turkey in the period 1965–2020. International Journal of Climatology, 42(16), 8232–8247.  A sakamakon canje-canje a cikin yanayin yanayi da hauhawar yanayin zafi na duniya, abubuwan da suka faru na yanayi masu tsanani kamar raƙuman zafi da ruwan sama mai nauyi suna faruwa akai-akai kuma tare da karuwar tsanani.
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