Ukuthuthukiswa kwe- amafu Ngokusobala kuba kancane uma inqubo ebangela ukuthi iyeke ukwenzeka. Nokho, izici ezihlukahlukene zingangenela bangela ukunyamalala wamaconsi amanzi noma amakristalu eqhwa akha amafu, njengokufudumala komoya, ukuba khona kwemvula nokuxubana nomoya ozungezile, ovame ukomisa. Ngaphezu kwalokho, umcimbi we Amafu esiphepho iye yathintwa ukungcola, okungaba nomthelela ekubunjweni nasekuhlakazweni kwayo.
Ifu lingathola ukushisa ngokumuncwa kwemisebe yelanga noma yasemhlabeni, nakuba zombili lezi zenzakalo zibuthakathaka uma kuqhathaniswa Ukushisa kwe-adiabatic. Lokhu kwenzeka lapho umoya ifu elikuwo ungaphansi kokuncipha. Njengoba izinga lokushisa lomoya likhuphuka, umswakama wawo ohlobene uyancipha, okubangela ukuthi umoya ungabe usagcwala; Ngenxa yalokho, izinhlayiya zamafu ziyahwamuka futhi ziguquke zibe umhwamuko ongabonakali wamanzi.
La ilanga Ngokuvamile kubangela ukuhlakazeka kwamafu akheke ngenxa yokunyakaza komoya. Lapho imisebe yelanga eyanele ifika phansi futhi ifudumeza umoya oseduze nendawo engaphezulu, izinga lokujiya okuxubile liyakhuphuka, ngaleyo ndlela kukhuphule isisekelo samafu eStratus noma eStratocumulus. Lesi simo sehlisa ukujiya kwefu okukhawulelwe ukuguquguquka kwesiphithiphithi, okuholela ekunyamaleni kwalo ekugcineni.
I-Los I-cumulus enhle yesimo sezulu, ezakheka ezindaweni ezisemhlabeni ngaphansi kwethonya lokukhanya kwelanga, isenzakalo esivame ukuvela phakathi nezinsuku. Lawa mafu ngokuvamile avela ekuseni, afinyelele izinga eliphezulu lokukhula kwawo ntambama, futhi ashabalala ngokushesha njengoba amazinga okushisa aphansi ehla ekupheleni kosuku. Kulo mongo, kuyathakazelisa ukubona indlela la mafu, ngokungafani iziphepho ezinkulu, ezibonakala ngezimo zezulu ezimbi kakhulu.
Kubalulekile ukuqaphela ukuthi umoya ozungeze ifu ngokuvamile awugcwali ngokuphelele. Ukuxutshwa kwamafu nalo moya kungaholela kumswakama ongaphansi kuka-100%, okungaheha okunye ukuhwamuka efwini ngokwalo, okubangela ukuguguleka kwalo nokushabalala ekugcineni.
Ulwazi olwengeziwe mayelana ne- RH y ifu elithi 'Morning Glory', isenzakalo semeteorological esihlaba umxhwele.
Izinto Ezibalulekile Ekuhlakazweni Kwamafu
I-cloud dissipation inqubo yesimo sezulu engathinteka yizici eziningi. Ikakhulukazi okulandelayo:
- Ukushintsha kwezinga lokushisa: Lapho izinga lokushisa lomoya likhuphuka, umswakama ungase unciphe, okubangele ukuhwamuka kwamaconsi amanzi.
- Umoya: Imimoya ingahlakaza umswakama efwini, ibangele ukuthi uhlangane nomoya owomile futhi ngaleyo ndlela usheshise ukushabalala kwawo. Lesi simo sibalulekile kumongo we imithelela yokuduma kwezulu.
- Imvula: Uma ifu liqala ukukhiqiza imvula, ukukhishwa kwamanzi kungaholela ekulahlekelweni kwesisindo sawo futhi, ekugcineni, ukuchithwa kwawo.
- Imisebe yelanga: Ukuchayeka emisebeni yelanga kushisa umoya ozungezile, okungabangela ukunyuka kwezinga lokushisa nokuhwamuka okulandelayo kwamafu.
Ngaphezu kwalezi zici, ukwakheka nokwakheka kwefu ngokwalo kudlala indima ebalulekile esikhathini salo sokuphila. Amafu akhiwe ngamaconsi amancane ngokuvamile awahlali azinzile ngakho-ke avame ukushabalala ngokushesha, okuye kwaxhunyaniswa nokwenzeka isithwathwa nesithwathwa, izenzakalo ezithinta ukuzinza komkhathi.
Imininingwane Yenqubo Yokuhlakazwa
Amafu azohlala emkhathini inqobo nje uma kunezimo ezifanele zokubunjwa nokuthuthuka kwawo. Le nqubo ingahlukaniswa ngezigaba eziningana:
- Ukwakhiwa Kwefu: Lesi isinyathelo sokuqala, lapho amaconsi amanzi ehlangana khona ezungeze izinhlayiya ezisemkhathini, njengothuli noma usawoti.
- Ukulungiswa kwamafu: Uma nje kunokugeleza njalo komoya oswakeme nezimo zokushisa zivuma, ifu lingakwazi ukuhlala lihamba emoyeni.
- I-Cloud Dissipation: Lapho izimo zishintsha, njengokwenyuka kwezinga lokushisa noma ukwehla komswakama, ifu liqala ukuncibilika.
Ubude besikhathi befu bungahluka kusukela emahoreni ambalwa kuya ezinsukwini ezimbalwa, kuye ngokuzinza kwezimo zomkhathi kanye nemvelo yefu ngokwalo. Ngalo mqondo, kuyathakazelisa ukuhlola ukuthi i- imikhono yasolwandle ingaxhuma amaphethini athile okuhlakazeka.
Ukubaluleka Kwamafu Esimeni Sezulu
Amafu awabalulekile nje kuphela ekuqondeni umjikelezo wamanzi, kodwa futhi adlala indima ebalulekile ekulawuleni isimo sezulu soMhlaba. Zisebenza njengesibuko esibonisa ukukhanya kwelanga, zisiza ukupholisa ubuso boMhlaba, kuyilapho zibamba ukushisa emkhathini, okunomthelela kumphumela we-greenhouse.
Izazi zesimo sezulu ziye zahlola ukuziphatha kwamafu ukuze zibikezele izimo zesimo sezulu esibi kakhulu, njengeziphepho neziphepho. Ukuhlukahluka kokwakheka kwamafu nokuhlakazeka kunganikeza izinkomba ezinguqukweni zamaphethini wezulu womhlaba kanye nomthelela wawo endaweni ezungezile. Ulwazi mayelana ne- izenzakalo zesiphepho kuyafaneleka futhi kulo mongo.
I-Artificial Cloud Dissipation: Ingabe Kungenzeka?
Umqondo wokukhohlisa komkhathi, ikakhulukazi i imbewu yefu, iye yanakwa eminyakeni yamuva. Le nqubo ihilela ukufaka amakhemikhali emafwini ukuze abangele imvula futhi, kwezinye izimo, nokunciphisa ubukhulu besichotho. Enye yezinto ezisetshenziswa kakhulu iodide yesiliva, esebenza njenge-nucleus yokufingqa.
El iodide yesiliva Inokwakheka kwekristalu efana neqhwa futhi ingahlakazwa emafwini isuka ezindizeni. Ngokwenza lokhu, inani lemvula eliwa kulawa mafu lingakhuphuka. Kodwa-ke, ukusebenza kahle kwalolu hlelo kanye nemiphumela yayo yesikhathi eside esimweni sezulu kuseyindaba-mpikiswano.
Imbewu yamafu isetshenziswe emazweni amaningana, okuhlanganisa i-Australia ne-United States, ukuzama ukukhulisa imvula ezindaweni ezikhahlanyezwe yisomiso. Nakuba ezinye izifundo ziye zaphakamisa ukuthi imbewu yamafu ingaba nomthelela omuhle, abanye baxwayisa ngokuthi abukho ubufakazi obanele bokuqinisekisa ukuthi kuyisixazululo esisebenzayo ezinkingeni zesomiso.
Nakuba le ndlela ingase ibonakale ithembisa, kuye kwaphakama ukukhathazeka mayelana nemiphumela yayo engemihle kanye nezimiso zokuziphatha zokuxhaphaza isimo sezulu ngale ndlela. Ukuhlukahluka kwemvelo kwemvula kwenza kube nzima ukucacisa ukusebenza kahle kokutshala kwamafu.
Umbuzo wokuthi ukulawulwa kwesimo sezulu kungasebenza yini kusewumbuzo ovulekile futhi uyindawo yocwaningo olusebenzayo phakathi kwezazi zezulu kanye nososayensi bomkhathi.
Ucwaningo Lwakamuva Lokuhlakazeka Kwamafu
Ucwaningo lwakamuva lufune ukuqonda kangcono izinqubo eziholela ekwakhekeni kwamafu nokushabalala. Abacwaningi besimo sezulu basebenzise ubuchwepheshe obuthuthukisiwe njengamasathelayithi namamodeli asemoyeni ukuze baqoqe imininingwane yokuphila kwamafu nokuthi aziphatha kanjani ngaphansi kwezimo zezulu ezihlukene.
Le datha inike amandla ukulingisa okunembe kakhudlwana nokubikezeleka kokuziphatha kwamafu nokusebenzisana kwawo nesimo sezulu, okubalulekile ekuthuthukiseni ukunemba kwezibikezelo zesimo sezulu.
- Ikhono lokubikezela izivunguvungu nezehlakalo zesimo sezulu esibi lithuthuke kakhulu ngenxa yale ntuthuko yezobuchwepheshe.
- Ulwazi mayelana nokuguquguquka kwamafu luyasebenza kwezolimo, lapho lubalulekile ekulawuleni ukuchelela nokuvuna.
- Ukutadisha ukwakheka kwamakhemikhali amafu kungasisiza siqonde ithonya lawo kumakhemikhali asemoyeni nokushintsha kwesimo sezulu.
- Amafu anethonya elikhulu ekulinganiseni kwamandla omhlaba futhi abalulekile ekuqondeni ukuguquka kwesimo sezulu.
Imithelela amafu anayo esimweni sezulu nendlela asabela ngayo ekushintsheni kwezinga lokushisa nokuswakama iyaqhubeka nokuba yindawo ethokozisayo yokufunda, enethuba lokuvula izindlela ezintsha zokubhekana nenkinga yesimo sezulu.
Ucwaningo lwamafu, kokubili ukwakheka nokuhlakazeka kwawo, luyingxenye ebalulekile yesayensi yesimo sezulu esizosiza ukuthuthukisa izinqubo zethu zokuphatha imithombo yemvelo futhi sibhekane nezinselele zokushintsha kwesimo sezulu esikhathini esizayo. Ukuthuthukiswa okuqhubekayo kwe ubuchwepheshe kanye nenqubekelaphambili ekuqondeni kwalezi zenzakalo zomkhathi kubalulekile ukuze siqhubeke sithuthukisa yethu amasu yokujwayela isimo sezulu esishintshayo.
