Ngokukhula okuqhubekayo komthamo wezinhlelo zamandla kagesi, ukumbozwa kwezintambo zokudlulisa amandla kagesi aphezulu nakho kuyakhula. Ngakho-ke, endaweni ye-micro-terrain, ukuchema komoya kungase kubangele ukuthi iketango lokufakwayo lolayini wokudlulisela litshekele ngasembhoshongweni, ngaleyo ndlela kufinyeze ibanga phakathi kwekhondakta nombhoshongo. Ezindaweni ezivulekile ze-microterrain, imimoya elandelanayo ivame ukuhambisana nokuduma kwezulu nesichotho, okuholela ekukhanyeni kwezulu. Lokhu kubangela umoya onomswakama owengeziwe lapho umoya ucishiwe, kunciphisa amandla okufakwa kwezintambo zikagesi. Ngaphansi kwemimoya enamandla, lapho umugqa wamanzi ophakathi owenziwe yimvula ufana nendlela yokukhishwa kwe-flascent, i-gap discharge voltage izokwehla. Ngokohlaziyo lwezici zesivinini somoya kulayini wokudlulisela, kungabonakala ukuthi ibanga lombhoshongo ngokuvamile lingamamitha angu-3–400. Kodwa ngekhanda lombhoshongo omncane, lapho ukuchezuka komoya kwenzeka, iketango lokufakwa ngaphakathi lingase liphambuke endleleni yomoya, okuholela ekuhlulekeni kwe-trigger. Ngokukhula kobude bombhoshongo, amathuba okuphambuka komoya ayanda. Ukuze kuncishiswe amathuba okuphambuka komoya kwezintambo zokudlulisa amandla kagesi aphezulu, uhlelo lokuklama kufanele lunqunywe ngokuya ngezimo zezulu. Kodwa-ke, ngenxa yokuba seduze kweziteshi zesimo sezulu ezindaweni ezingaphansi kwedolobha, kunzima kakhulu ukuqoqa ulwazi lwezezulu mayelana neziphepho kanye nomoya ohambayo, okuholela ekungabini kwereferensi enembile ekwakhiweni kwezintambo zokudlulisela. Ngakho-ke, uma kuvela inkanyamba, ukunikezwa kwamandla ngeke kukwazi ukusebenza ngokuphepha nangokuzinza.
Ukuhlaziywa kwezinto ezinomthelela wephutha lokuchezuka komoya
1 Isivinini esikhulu somoya esiklanyelwe
Olayini bokudlulisela emihosheni yezintaba, ukuvinjwa kwesigaba esiphambanayo sokugeleza komoya kuncipha kakhulu lapho umoya ungena endaweni evulekile yemihosha, futhi kwenzeka umphumela wokunqamula. Ngenxa yezimo zemvelo, umoya awuqoqi ku-canyon futhi kulokhu, umoya uphuthuma e-canyon, udale imimoya enamandla. Lapho ukugeleza komoya kuhamba eduze kwesigodi, umoya endaweni yokugeleza phakathi kwesigodi uzocindezelwa, futhi isivinini somoya sangempela sizoqiniswa ngokwengeziwe, sibe phezulu kunesivinini somoya oyisicaba, okuholela kumphumela omncane weshubhu. Lapho isigodi sijula, umphumela wokuthuthukisa uba namandla. Kunomehluko othile phakathi kwedatha yesimo sezulu kanye nesivinini esikhulu somoya ekuphumeni kwe-canyon. Kulesi simo, isivinini somoya esiphezulu esiklanyelwe ulayini singase sibe ngaphansi kunesivinini esikhulu somoya esisheshayo esitholwe umugqa wangempela, okuholela ebangeni lokuchezuka elincane kunebanga langempela kanye ne-stroke.

2 Ukukhethwa kombhoshongo
Ngokujula okuqhubekayo kocwaningo, izindlela zobuchwepheshe zivuselelwa njalo, umbhoshongo nawo uyathuthuka. Njengamanje, umklamo ovamile wombhoshongo ususetshenziswe kabanzi, futhi isakhiwo sombhoshongo esisetshenziswa kweminye imigqa emisha sivunyiwe. Ekwakhiweni kwesekethe, naka ukwakheka kokuphambuka komoya, futhi unqume umthamo wangempela wokuphambuka komoya wokuthwala. Ngaphambi kwalokhu, yayingekho indinganiso ehlanganisiwe yokukhethwa kwemibhoshongo ezweni lonke, futhi eminye imigqa emidala enezingalo eziphambanayo ewumngcingo yemibhoshongo edonsa kanzima yayisasetshenziswa. Esimeni sezulu esinomoya, ukuxhumana okuvumelana nezimo kungasonteka ukuze kufinyezwe ibanga phakathi kwezintambo nemibhoshongo. Uma ibanga lilincane kunebanga eliphephile, lingabangela iphakethe lephutha lokuchezuka komoya
3 Ubuchwepheshe Bokwakha
Iphrojekthi yokumisa ulayini wokudlulisa idinga ithimba labakhi, izinga labasebenzi bokwakha, ikhono kanye nesibopho kuhluke kakhulu. Isibonelo, uma imininingwane yokukhiqiza yemigqa yokudonsa amanzi ingekho ezingeni futhi izisebenzi zokwamukela zingaboni inkinga, kungaholela ekusetshenzisweni kwalezi zindlela zokudonsa amanzi ezingajwayelekile, okwandisa amathuba okuphambuka komoya.
Uma umugqa wokudonsa amanzi umkhulu kakhulu futhi intambo evundlile ingafakiwe, izoshwibeka esimweni sezulu esinomoya, okwenza ibanga phakathi kocingo nombhoshongo libe lincane kakhulu, okuholela ekugxumeni okufudukayo: Uma ubude bangempela bomugqa wokudonsa we-jumper buncane. , isikhathi eside kunebanga phakathi komugqa wokudonsa kanye ne-boom, isivikelo esingaphansi singase siphakame, okungase kubangele ukuphuma kwe-boom.