Utshintsho lwemozulu luneziphumo ezahlukeneyo kwiindawo ezahlukeneyo. Ngokwesiqhelo olu tshintsho kwiziphumo luyahluka kwizinga elikhulu okanye ngobude / ngobubanzi emhlabeni. Ngokubanzi, utshintsho lwemozulu lunefuthe lokunyuka kwamaqondo obushushu, kodwa Olu konyuka aluyi kufana kuzo zonke iindawo.
Ngokophononongo, ukonyuka kwamaqondo obushushu kuya kuchaphazela izixeko ngakumbi kunakwimimandla yendalo kwaye, ukuba inqanaba langoku lokunyuka liyaqhubeka, ifuthe lamaza obushushu ezixekweni linokuphindaphindwa ngesine. Ngaba uyafuna ukwazi ngakumbi ngolu phando?
Iziphumo zokunyuka kwamaqondo obushushu
Uphononongo malunga nokuba amaqondo obushushu angazichaphazela njani izixeko kunye nemeko yendalo lwenziwe yiYunivesithi yaseLeuven (eBelgium) kwaye banezigqibo eziqinisekileyo abazenzileyo kwindibano ebibanjelwe yi-European Union ye-Geosciences eVienna.
Omnye wababhali abaphambili bophando ngamaqondo obushushu abiziweyo UHendrik wouters Icacisile into yokuba iziphumo ezibi zokutshintsha kwemozulu ngokubhekisele kumaqondo obushushu ziya kuba zibi ngokuphindwe kabini kwizixeko njengendawo zendalo.
Sele isaziwa kuphando lwangaphambili ukuba isiphumo sobushushu obuphezulu sikhulu ezixekweni kunasezilalini. Ngokukodwa ebusuku kukho "isiqithi sobushushu", kukunyuka komoya oshushu obambeke kwiipavumente kunye neasphalt, kubangela ukwanda kwamaqondo obushushu. Yintoni ebangela ukuba olu phononongo luguquke kukwenza ubalo okokuqala ngqa kwinqanaba apho izixeko ziya kuba namaqondo obushushu aphezulu.
Iziphumo zokunyuka kwamaqondo obushushu ezixekweni
Kukho izifundo ezibonisa ukuba amaza obushushu ayenyuka ezixekweni, kokubini rhoqo kunye nokuqina. Ngobushushu obushushu, ukwamkelwa esibhedlele ngenxa yokonyuka kwamanzi emzimbeni, imveliso iyancipha, ukonakala kweziseko zophuhliso kuyonyuka kwaye kwiimeko ezibi kakhulu, iimeko zokufa ziyanda.
Kolu phando, abaphandi benze uhlalutyo malunga nendlela iimpembelelo zamaza obushushu ezinxibelelana ngayo ezixekweni nakwimeko yendalo. Kule nto, basebenzise imilinganiselo yeqondo lobushushu kule minyaka ingama-35 idlulileyo eBelgium kwaye bayithelekisa nokuhamba rhoqo kunye nokuqina apho kuye kwagqitywa ubushushu. Le mida iphawula umonakalo obangelwe kokubini empilweni nakuyo yonke into ekhankanywe apha ngasentla.
Ngenxa yoko, kunokubonwa ukuba ngeli xesha kufundwayo, amaza obushushu ebeshushu kakhulu ezixekweni kunasemaphandleni. Oku kulindeleke ukuba kubemandundu kwixesha elizayo.
Ixesha elizayo
Nje ukuba bafumane izigqibo zophando, bazinikezele ekwenzeni uqikelelo malunga nento eza kwenzeka kwixesha elizayo. Uqikelelo lusekwe kwimodeli eyenziwe kwiimodeli ezenziwe yikhompyuter. Olu qikelelo lubona kwangaphambili ukuba kwisithuba se-2041-2075 ifuthe lobushushu ezixekweni liphindwe kane kunokusendle.
Abaphandi bacacisa ukuba olu qikelelo luhambelana nemeko esezantsi kwaye bayaqonda ukuba zininzi izinto ezinokuchaphazela ukubala, njengokuhla okukhulu kokukhutshwa kwegesi ekrwada emoyeni okanye ukucothisa ukukhula kwezixeko.
Eyona meko imbi kakhulu kubushushu obugqithisileyo iya kuba kukunyuka amanqanaba olumkiso ukuya kwiidigri ezili-10 kwaye anokuhlala iintsuku ezingama-25 ehlotyeni. Nangona kunjalo, ukuba ukukhutshwa kwegesi yendlu eluhlaza kuncitshisiwe, kuya kufana nanamhlanje.
Ngayo yonke le nto, kwenziwa iinzame zokubhekisa kwimfuno ekhoyo yokuba izixeko ziphinde ziyile ubume bazo kunye nolawulo ngokusekwe kutshintsho lwemozulu. Umzekelo, uyilo olumi nkqo lwedolophu, ukunciphisa ukukhutshwa kwegesi eluhlaza okanye ukusebenzisa iziseko ezingcolisayo. Zizikhokelo zokunciphisa ifuthe lamaza obushushu.