Ama-Meadows amelana kakhulu nokushintsha kwesimo sezulu lapho umoya ucebile ku-CO2

Idlelo eliluhlaza

Izimo zezulu ezimbi kakhuluNjengamagagasi okushisa nesomiso, bangaguqula amandla okubuyiselwa kwekhabhoni ezindaweni eziphila emhlabeni. Ngenxa yocwaningo olunzulu lwedlelo eliphakathi nendawo elisentabeni, abacwaningi bakhombisa okokuqala ukuthi ukunothisa kwe-CO2 okuvela emkhathini kuthuthukisa ukutakula kwe-l idlelo ngemuva kwalezi zehlakalo ezimbi kakhulu. Ngaphezu kwalokho, kubambezela imiphumela emibi yokucindezeleka kwamanzi.

Phakathi kwamanje kuze kube sekupheleni kwekhulu leminyaka, ukuqapha ukuguquka kwesimo sezulu kungaholela ekwandeni kokuqina nobukhali bezehlakalo zezulu ezimbi kakhulu kuhlangene namaza okushisa nesomiso. Lezi zimo zezulu ezimbi bezizoba nazo imithelela emibi emiphakathini, ikakhulukazi emadlelweni, azwelayo kusomiso futhi ondle izinkomo zobisi nezenyama. Ekugcineni, kungadala ukonakala kwenhlabathi, kunciphise okuqukethwe kwayo ngezinto eziphilayo ezinothile ngekhabhoni.

Ukwanda kwesikhutha kuyanda

Noma kunjalo, ukwanda kwesikhutha emkhathini kunganciphisa lezi zingozi zesimo sezulu. Ngempela, i-CO2 iyi-substrate ye-photosynthesis yezitshalo futhi imvamisa ithanda ukubekezelelana kwezitshalo kwisomiso kanye nokuqongelelwa kwezinto eziphilayo emhlabathini.

Kuze kube namuhla, bekungaziwa ukuthi lezi imiphumela ezuzisayo ye-CO2 bangaqhubeka noma bangaqhubeki uma kwenzeka isimo sezulu esibi kakhulu. Ngokokuqala ngqa, kunikezwa impendulo yalo mbuzo ngenxa yokuhlolwa. Amasampula edlelo abhekana nesimo sezulu esinjengaleso esasibikezelwe kusukela ngonyaka ka-2050, sifudumele futhi somile, kanye nokwanda kwenani lomkhathi le-CO2 kuhlangene, noma cha, kushiswa elishisayo nesomiso esibi kakhulu.

Isomiso kanye ne-heatwave

Ngesikhathi sesomiso kanye ne-heatwave, ukucebisa ku I-Atmospheric CO2 inciphisa imiphumela emibi yokuxineka kwamanzi nokushisa, ukugcina ukusebenza komzimba wezitshalo. Kuvusa ukukhula kwezimpande, kuvumela ukufinyelela emanzini amaningi nezakhi emhlabathini, okusheshisa ukukhula kwedlelo kusukela ekugcineni kwesimo sezulu esibi kakhulu.

Kukho konke lokhu kuhlolwa, ukwanda kwe-CO2 esemkhathini kususwe ngokuphelele imiphumela emibi yesomiso kanye ne-heatwave ekwakhiweni kwekhabhoni edlelweni. Lolu cwaningo lukhombisa ukubaluleka kokucabangela isethi yokusebenzisana ocwaningweni lwemithelela yokuguquka kwesimo sezulu.

Kubonisa ukuthi ukwanda kwe-CO2 yasemkhathini kuyanda ukumelana nodaba lomhlabathi, kwemvelo yamadlelo neyezinkomo eziyizinkokhelo zesimo sezulu esibi kakhulu sohlobo lweshisa elishisayo nesomiso, kepha ayikuvumeli ukuphetha ngemiphumela eqoqayo yalokhu kudlondlobala kwesimo sezulu. Le miphumela yokuqoqeka kufanele ihlolwe ngelinye ibhethri lokuhlola.


Okuqukethwe yi-athikili kunamathela ezimisweni zethu ze izimiso zokuhlelela. Ukubika iphutha chofoza lapha.

Yiba ngowokuqala ukuphawula

Shiya umbono wakho

Ikheli lakho le ngeke ishicilelwe.

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  1. Ubhekele imininingwane: Miguel Ángel Gatón
  2. Inhloso yedatha: Lawula Ugaxekile, ukuphathwa kwamazwana.
  3. Ukusemthethweni: Imvume yakho
  4. Ukuxhumana kwemininingwane: Imininingwane ngeke idluliselwe kubantu besithathu ngaphandle kwesibopho esisemthethweni.
  5. Isitoreji sedatha: Idatabase ebanjwe yi-Occentus Networks (EU)
  6. Amalungelo: Nganoma yisiphi isikhathi ungakhawulela, uthole futhi ususe imininingwane yakho.