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Tasirin canjin yanayi

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Infotaula d'esdevenimentTasirin canjin yanayi

Iri effect (en) Fassara
Sanadi canjin yanayi
Canjin yanayi
Thick orange-brown smoke blocks half a blue sky, with conifers in the foreground
A few grey fish swim over grey coral with white spikes
Desert sand half covers a village of small flat-roofed houses with scattered green trees
large areas of still water behind riverside buildings
Wasu tasirin sauyin yanayi: gobarar daji da ta haifar da zafi da bushewa, murjani mai launin ruwan kasa wanda ya haifar da ƙarancin teku da dumama, ƙaurawar muhalli da hamada ta haifar, da Ambaliyar bakin teku da guguwa da hauhawar matakin teku ta haifar.

Tasirin Canjin yanayi an rubuta shi sosai kuma yana girma ga yanayin duniya da al'ummomin mutane. Canje-canje ga tsarin yanayi sun haɗa da Yanayin dumama gaba ɗaya, canje-canje ga yanayin hazo, da kuma yanayin da ya fi tsanani. Yayin da yanayin ya canza yana tasiri ga yanayin halitta tare da tasirin kamar gobarar daji mai tsanani, narkewar permafrost, da hamada[1]. Wadannan canje-canje suna tasiri ga yanayin halittu da al'ummomi, kuma suna iya zama ba za a iya juyawa ba da zarar an haye maki.[2] Masu gwagwarmayar yanayi suna shiga cikin ayyuka da yawa a duniya waɗanda ke neman inganta waɗannan batutuwan ko hana su faruwa.[3]

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.[4] 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.[5]

Abubuwan da ke haifar da su [6] da tasirin da ke tattare da su [7] [8]: 3-36 na Canjin yanayi. Wasu tasirin suna aiki ne a matsayin kyakkyawan ra'ayi wanda ke kara sauyin yanayi.[9]

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 iya[10]. 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. [11]:259

Canje-canje a cikin zafin jiki

[gyara sashe | gyara masomin]
A cikin shekaru 50 da suka gabata Arctic ya fi dumi, kuma yanayin zafi a ƙasa ya karu fiye da Yanayin zafi na teku.[12]

Warming na duniya yana shafar dukkan sassan tsarin yanayi na Duniya. Yanayin duniya ya tashi da 1.1 °C (2.0 °F) . 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.[4] Yanayin zafi na dare ya karu da sauri fiye da yanayin zafi na rana.[13] Tasirin a kan yanayi da mutane ya dogara da yadda duniya ke dumi. :787

Yanayi

[gyara sashe | gyara masomin]

  Yanayin ƙasa da na tsakiya, inda kusan duk yanayin ke faruwa, suna dumama saboda tasirin greenhouse.[14] Rashin ruwa da yanayin zafi suna ƙaruwa yayin da yanayin zafi ke ƙaruwa.[15] Rashin ruwa iskar gas ce, don haka wannan tsari shine ra'ayi mai ƙarfafa kansa.[16]

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.[15] 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.[17] 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.[18][19] 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.[20]

  1. ↑ https://constructive-voices.com/ha/%C6%99ira-mai-jurewa-don-ginin-canjin-yanayi-don-matsanancin-yanayin-yanayi/
  2. ↑ https://www-bbc-com.cdn.ampproject.org/v/s/www.bbc.com/hausa/labarai-52774716.amp?amp_gsa=1&amp_js_v=a9&usqp=mq331AQIUAKwASCAAgM%3D#amp_tf=From%20%251%24s&aoh=17535993740585&referrer=https%3A%2F%2Fwww.google.com&ampshare=https%3A%2F%2Fwww.bbc.com%2Fhausa%2Flabarai-52774716
  3. ↑ CounterAct; Women's Climate Justice Collective (2020-05-04). "Climate Justice and Feminism Resource Collection". The Commons Social Change Library (in Turanci). Retrieved 2024-07-08.
  4. ↑ 4.0 4.1 Lindsey, Rebecca; Dahlman, Luann (June 28, 2022). "Climate Change: Global Temperature". climate.gov. National Oceanic and Atmospheric Administration. Archived from the original on September 17, 2022. Cite error: Invalid <ref> tag; name "Lindsey-2022" defined multiple times with different content
  5. ↑ Doney, Scott C.; Busch, D. Shallin; Cooley, Sarah R.; Kroeker, Kristy J. (2020-10-17). "The Impacts of Ocean Acidification on Marine Ecosystems and Reliant Human Communities". Annual Review of Environment and Resources (in Turanci). 45 (1): 83–112. doi:10.1146/annurev-environ-012320-083019. ISSN 1543-5938. S2CID 225741986.
  6. ↑ "The Causes of Climate Change". climate.nasa.gov. NASA. Archived from the original on 2019-12-21.
  7. ↑ "Climate Science Special Report / Fourth National Climate Assessment (NCA4), Volume I". science2017.globalchange.gov. U.S. Global Change Research Program. Archived from the original on 2019-12-14.
  8. ↑ "Extreme Weather and Climate Change". NASA.gov. National Aeronautics and Space Administration. September 2023. Archived from the original on 26 October 2023.
  9. ↑ "The Study of Earth as an Integrated System". nasa.gov. NASA. 2016. Archived from the original on 2016-11-02.
  10. ↑ https://www.bbc.com/hausa/topics/c7zp510jdzpt
  11. ↑ Empty citation (help)
  12. ↑ "GISS Surface Temperature Analysis (v4)". NASA. Retrieved 12 January 2024.
  13. ↑ Davy, Richard; Esau, Igor; Chernokulsky, Alexander; Outten, Stephen; Zilitinkevich, Sergej (January 2017). "Diurnal asymmetry to the observed global warming". International Journal of Climatology. 37 (1): 79–93. Bibcode:2017IJCli..37...79D. doi:10.1002/joc.4688.
  14. ↑ Hausfather, Zeke (21 June 2017). "Study: Why troposphere warming differs between models and satellite data". Carbon Brief. Retrieved 19 November 2019.
  15. ↑ 15.0 15.1 Trenberth, Ke (2011). "Changes in precipitation with climate change". Climate Research. 47 (1): 123–138. Bibcode:2011ClRes..47..123T. doi:10.3354/cr00953. Cite error: Invalid <ref> tag; name "Trenberth-2011" defined multiple times with different content
  16. ↑ "Climate change: evidence and causes | Royal Society". royalsociety.org. Retrieved 19 November 2019.
  17. ↑ Swain, Daniel L.; Singh, Deepti; Touma, Danielle; Diffenbaugh, Noah S. (2020-06-19). "Attributing Extreme Events to Climate Change: A New Frontier in a Warming World". One Earth (in Turanci). 2 (6): 522–527. Bibcode:2020OEart...2..522S. doi:10.1016/j.oneear.2020.05.011. ISSN 2590-3322. S2CID 222225686.
  18. ↑ 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. doi:10.1007/s00704-020-03156-w.
  19. ↑ Aksu, H. (2022). A determination of season shifting across Turkey in the period 1965–2020. International Journal of Climatology, 42(16), 8232–8247. doi:10.1002/joc.7705
  20. ↑ "Effects of Climate Change - Impacts and Examples". www.nrdc.org (in Turanci). 2022-10-24. Retrieved 2024-12-07.
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