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Kasafin kudin makamashi na duniya

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Kasafin kudin makamashi na duniya
scientific model (en) Fassara
Daidaitawar makamashi da rashin daidaituwa na duniya, yana nuna inda makamashi mai yawa ke tafiya: Rashin radiation yana raguwa saboda karuwar iskar gas a cikin yanayi, wanda ke haifar da rashin daidaito na makamashi na duniya na kimanin 460 TW. Hakanan an nuna kashi da ke shiga kowane yanki na tsarin yanayi.

Kasafin kudin makamashi na Duniya (ko ma'aunin makamashi) shine ma'auni tsakanin makamashi da Duniya ke karɓa daga Rana da makamashi wanda Duniya ta rasa zuwa sararin samaniya. Ƙananan hanyoyin samar da makamashi, kamar zafi na ciki na Duniya, ana la'akari da su, amma suna ba da gudummawa kaɗan idan aka kwatanta da hasken rana. Kasafin kudin makamashi kuma yana la'akari da yadda makamashi ke motsawa ta hanyar tsarin yanayi. Sun yana dumama wurare masu zafi fiye da Yankunan polar. Sabili da haka, adadin hasken rana da wani yanki ya karɓa ba a rarraba shi ba daidai ba. Yayin da makamashi ke neman daidaito a duk faɗin duniya, yana motsa hulɗa a cikin tsarin yanayi na Duniya, watau, ruwa Duniya, kankara, yanayi, dutse, da duk abubuwan da ke rayuwa.[1] : 2224 Sakamakon shine yanayin duniya.[2]

Kasafin Gudun makamashi na duniya ya dogara da dalilai da yawa, kamar su aerosols na yanayi, iskar gas, albedo na ƙasa, girgije, da tsarin Amfani da ƙasa. Lokacin da iskar makamashi mai shigowa da fita ke cikin daidaituwa, Duniya tana cikin daidaituwa mai haske kuma tsarin yanayi zai kasance mai ɗorewa. Warming na duniya yana faruwa ne lokacin da duniya ke karɓar makamashi fiye da yadda take ba da shi ga sararin samaniya, kuma sanyaya na duniya yana faru ne lokacin da makamashi mai fita ya fi girma.

Nau'ikan ma'auni da lura da yawa suna nuna rashin daidaituwa tun aƙalla shekara ta 1970. Yawan dumama daga wannan taron da mutum ya haifar ba shi da wani misali. : 54 Babban asalin canje-canje a cikin makamashi na Duniya ya fito ne daga canje-canjen da mutum ya haifar a cikin abun da ke cikin yanayi. A cikin shekara ta 2005 zuwa 2019 Rashin daidaituwa na makamashi na duniya (EEI) ya kai kimanin 460 TW ko a duniya 0.90±0.15 W / m2 .

Yana ɗaukar lokaci don duk wani canji a cikin kasafin kuɗin makamashi don haifar da duk wani canjin gagarumin canji a yanayin zafin duniya. Wannan ya faru ne saboda yanayin zafi na Tekuna, ƙasa da cryosphere. Yawancin samfuran yanayi suna yin lissafi daidai na wannan inertiya, kwararar makamashi da adadi.

Kasafin kudin makamashi na duniya ya hada da "mafi yawan makamashi da ke da alaƙa da tsarin yanayi". Wadannan su ne "babban kasafin kudin makamashi na sararin samaniya; kasafin kudin makamashin sama; canje-canje a cikin kayan makamashi a duniya da kuma kwararar makamashi ta ciki a cikin tsarin yanayi".[1]

Gudun makamashi na duniya

[gyara sashe | gyara masomin]
Incoming, saman-na-atmosphere (TOA) shortwave flux radiation, yana nuna makamashi da aka karɓa daga Sun kamar yadda aka ƙaddara daga ma'aunin CERES (26-27 Janairu 2012). Yankunan fari mafi haske suna nuna mafi girman haskakawa (ƙananan shawo kan) na hasken rana, yayin da yankunan shuɗi mafi duhu suna nuna mafi girma shawo kan.

Duk da manyan canja wurin makamashi a ciki da daga Duniya, yana riƙe da yawan zafin jiki na yau da kullun saboda, gabaɗaya, akwai ƙarancin riba ko asarar: Duniya tana fitowa ta hanyar radiation na yanayi da na ƙasa (wanda aka canza zuwa tsawo na lantarki) zuwa sararin samaniya game da adadin makamashi kamar yadda yake karɓa ta hanyar hasken rana (duk nau'ikan radiation na lantarki).

Babban asalin canje-canje a cikin makamashi na Duniya ya fito ne daga canje-canjen da mutum ya haifar a cikin abun da ke cikin yanayi, wanda ya kai kimanin 460 TW ko a duniya 0.90±0.15 W / m2. 

Makamashi na hasken rana mai shigowa (shortwave radiation)

[gyara sashe | gyara masomin]

Jimlar adadin makamashi da aka karɓa a kowane dakika a saman Yanayin duniya (TOA) ana auna shi a cikin watts kuma ana ba da shi ta hanyar hasken rana na yau da kullun yankin sashi na Duniya ya dace da radiation. Saboda yankin farfajiyar wani yanki ya ninka sau hudu yankin sashi na wani yanki (watau yankin da'irar), matsakaicin TOA a duniya da na shekara-shekara shine kashi ɗaya cikin huɗu na ma'aunin hasken rana don haka kusan 340 watts ne a kowace murabba'in mita (W / m2). Tun da yake sha ya bambanta da wuri da kuma bambancin rana, yanayi da shekara-shekara, lambobin da aka nakalto sune matsakaicin shekaru da yawa da aka samu daga ma'aunin tauraron dan adam da yawa

  1. 1.0 1.1 Cite error: Invalid <ref> tag; no text was provided for refs named IPCC AR6 glossary
  2. "ACS Climate Science Toolkit Greenhouse Gases". www.acs.org. ACS. Archived from the original on 31 May 2023. Retrieved 18 June 2023