Uphuhliso lwe amafu iyacotha, ngokucacileyo, xa inkqubo evela kubo iyeka ukwenzeka. Kodwa ezinye izinto zinokungenelela kubangele ukunyamalala ukusuka kumathontsi amanzi okanye ziikristale zomkhenkce ezisuka emafini ezifana nokufudumeza umoya, imvula kunye nokudibanisa nomoya owomileyo ojikelezayo.
Ilifu linokufudunyezwa ngokufunxwa kwemitha yelanga okanye yomhlaba, kodwa zombini ezi zinto zibuthathaka ngokuthelekiswa ne Ukufudumeza adiabatic.
Yile nto inokwenzeka ukuba umoya apho ilifu likhoyo uxhaswa. Njengokuba iqondo lobushushu lomoya lisanda, ukufuma okulinganayo kuyahla kwaye umoya unokuzaliswa; emva koko, amasuntswana amafu ayenyuka abe ngumphunga umphunga wamanzi ongabonakaliyo.
La ilanga ihlala ibangela ukusasazeka kwamafu okwenziwe sisiphithiphithi. Ukuba imitha yelanga eyaneleyo ingena emhlabeni, ifudumeza umoya kufutshane nomphezulu womgangatho, inqanaba lokuxinana komxube liyenyuka kwaye, ke, isiseko seStratus okanye iStratocumulus siyenyuka naso. Emva koko, ubukhulu belifu obuthintelwe kukuguqulwa kwesiphithiphithi luyancipha kwaye ilifu ekugqibeleni liyanyamalala ngokupheleleyo.
Los Imozulu elungileyo yecumulus, ezenziwa kumazwe aphantsi kwempembelelo yokunyanzeliswa, zizinto ezinomdla. Ngokuqhelekileyo bavela ngentsasa, bafikelela kuphuhliso oluphezulu ngexesha lasemva kwemini kwaye banyamalale ngokukhawuleza xa umhlaba uphola kwakhona ekupheleni kosuku.
Umoya ojikeleze ilifu uhlala ungafakwanga. Ukuxutywa kwelifu nalo moya kunokubangela ukufuma okungaphantsi kwe-100% kwaye kuvelise okunye ngumphunga efini, ekhukhulayo kwaye inokutshatyalaliswa.
Iinkcukacha ezithe xaxe - RH, Ilifu 'lozuko lwasekuseni', imeko yemozulu enomdla