Iindawo zentlambo.
Abasebenzi bokucima umlilo kummandla wentlambo yomlilo weentaba, kufuneka sinikele ingqalelo okokuqala ngumlilo oveliswa ngumlilo ophaphazelayo kulula ukuvutha intsimi yentaba ekufuphi, ejikelezwe ngabasebenzi bokulwa nomlilo;Okwesibini, xa umlilo uvutha, isixa esikhulu. Ioksijini iyatshatyalaliswa, ukuze umoya weoksijini osemoyeni osemazantsi entlambo wehle, ukuze isicima-mlilo sifuthaniseleke sife.
Indawo yeCanyon.
Xa umoya uvuthuza kubude bentlambo nobubanzi bentlambo buyahluka ngokweendawo ngeendawo, isantya somoya siyanda kwindawo emxinwa.Oku kubizwa ngokuba yicanyon wind, okanye canyon effect.Umlilo wawuvutha kulo mwonyo, yaye wawukhawuleza kangangokuba kwakuyingozi ukulwa nawo kulo mwonyo.
Indawo yomsele.
Ukuba umsele oyintloko kwinduli yomlilo uyatsha, umlilo uya kuphambukiswa xa udibana nesebe.Isebe ekutshisweni, kodwa akukho lula ukuya kwicala eliphambili lomsele wophuhliso, ngoko ke, ukuba umsele omkhulu womlilo, abasebenzi bokucima umlilo. ukusuka kumsele oyintloko ukuya kwintshukumo ephambili yomsele ayikhuselekanga.
Indawo yesali.
Xa umoya uwela intsimi yesali yenduli yentaba (oko kukuthi, umgama phakathi kweenduli ezimbini zeentaba kunye nokuphakama kwentlambo kunye nentlambo yentaba ayikude kakhulu), idla ngokwenza izivunguvungu ezithe tye nezithe nkqo, ezinokubangela umonakalo kubacimi-mlilo.
Uluhlu lweentaba olunyuka ngokulandelelanayo.Xa kukho iintaba eziphakamileyo ngokulandelelanayo phambi komlilo, umlilo ukhula ngokukhawuleza ngaphambili, kwaye iintaba ezininzi ziya kutshiswa zonke ngaxeshanye.Akukhuselekanga ukwakha imigca yomlilo kwiinduli eziphambi komlilo.
Ixesha lokuposa: Mar-03-2021