El Intaba-mlilo iMauna Loa yaqhuma ngoNovemba 27. Leli qiniso alimangazanga muntu njengoba le ntaba-mlilo ingenye yeziqhuma kakhulu emhlabeni. Kodwa-ke, sebeqalile ukukhathazeka mayelana ne-carbon dioxide ekhishwayo emkhathini futhi ingathinta ukufudumala kwembulunga yonke namuhla, ngakho-ke, ukushintsha kwesimo sezulu.
Kulesi sihloko sizokutshela ngomphumela wokukhishwa kwe-carbon dioxide ephuma endaweni yentaba-mlilo yaseMauna Loa emkhathini futhi kuyathinta ukushintsha kwesimo sezulu.
I-carbon dioxide nokushintsha kwesimo sezulu
Ukufudumala kwemvelo kwemvelo yikho okugcina izinga lokushisa lizinzile futhi kwenza iplanethi yethu ikwazi ukuhlalwa. Le carbon dioxide igcinwa emkhathini futhi ngenxa yokukhishwa kwezintaba-mlilo, imikhiqizo ebolile, njll. Nokho, ukukhathazeka ngokukhishwa kwe-carbon dioxide entaba-mlilo yaseMauna Loa kuyakhula. Kucatshangwa ukuthi kungase kwenze isimo sibe sibi ngokushintsha kwesimo sezulu.
Okuqinisekile ukuthi izilinganiso ze-carbon dioxide ziyaphazanyiswa yilokhu kuqhuma. Lezi zinguquko ekukhishweni kwesisi esibamba ukushisa azinawo umthelela esilinganisweni esijwayelekile sendawo yokuhlola njengoba lesi sikhungo sokuhlola singalinganisi ukugxila kwendawo, kodwa kunalokho okwaziwa ngokuthi. isizinda se-carbon dioxide concentration. Leli inani le-carbon dioxide emkhathini jikelele.
Indawo yokuhlola itholakala phezu kwentaba-mlilo phakathi nolwandle ngokunembile ukuze kugwenywe iziphazamiso eziningi kanye nemithombo yendawo yokungcola. Ngaphezu kwalokho, selokhu kwaqala ukuqhuma bebelungiselela ukubona izinguquko ezikhiqizwe igesi yendawo bese bezilungisa kumarekhodi abo.
Okuthakaselwa yilesi sibukeli ukulinganisa isizinda se-carbon dioxide lapho ungabona khona imiphumela yokukhishwa kwesisi esibamba ukushisa zenzeke endaweni eqhele ngezinkulungwane zamakhilomitha ukusuka endaweni yokubuka izinto. Endabeni yemithombo yendawo yokukhipha umoya kulula kakhulu ukubona ukuchezuka ezilinganisweni kuye ngokuthi umoya uya ngakuphi.
Ukuthi izinto ezikhishwayo zithinta kanjani ukushintsha kwesimo sezulu
Uma singabaza ukuthi ukukhishwa kwesikhutha kulokhu kuqhuma kukuthinta kanjani ukushintsha kwesimo sezulu, singasho ukuthi akukho nhlobo. Phela, cishe ama-degree Celsius amabili angu-1.3 izinga lokushisa elivamile leplanethi eliye laphakama akukaze kwenziwe kusukela ezikhathini zangaphambi kwezimboni. Lokhu kuqhuma ngeke kubangele ukuguquka kwesimo sezulu kubi kakhulu.
Esikalini sendawo noma sesifunda kanye nezikhathi ezingekho mfushane, kungaphawulwa ukuthi ukugxila kwe-carbon dioxide zingashintshwa ngendlela encomekayo ngenxa yalezi zinqumo. Kodwa ukuqhuma okunjalo akubalulekile ekulinganiseni komhlaba wonke kwesizinda se-carbon dioxide.
Ngiyethemba ukuthi ngalolu lwazi ungafunda kabanzi mayelana nomthelela wokukhishwa kwegesi evela entaba-mlilo iMauna Loa.