Esikhathini sethu, abaningi bahlushwa ukwesaba ukuhamba emoyeni - ukuqhuma kwamabhomu . Abanye abantu babangela ukuhlaselwa kwe-panic, beka futhi befika, abanye besaba ukuthi izinjini zizohluleka ngokuzumayo, kuyilapho abanye besaba ukuhlasela kwamaphekula. Futhi esinye sezizathu ezenza abanye abantu besabe ukushayela kungukungqubuzana. Imele ukuzamazama okuqinile phakathi nendiza. Lokhu kungethusa wena, ikakhulukazi uma uhamba ngendiza okokuqala. Abagibeli bangase babe nomuzwa wokuthi kunezinkinga ezinkampanini yendiza, futhi abashayeli bezindiza abahlangabezane nokulawula. Kodwa empeleni, ukuhlukunyezwa kuyinto evamile, yendalo yemvelo. Ukuze unqobe ukwesaba kwakho, kwanele ukwazi ukuthi kungani kunezingxabano kule ndege, futhi kuyingozi kangakanani.
Izimbangela ze-turbulence
I-phenomenon of turbulence yatholakala ngokuhlolwa ngo-1883 ngu-Reynolds, onguNgisi onjiniyela. Wabonisa ukuthi ngokukhuphuka kwezinga lokugeleza kwamanzi noma umoya emkhatsini owenziwe, amagagasi anezikhukhula kanye nama-vortices akhiwa. Ngakho-ke, umoya yiyona "eyinhloko" yezingxabano. Ezingxenyeni ezahlukene zemvelo, ama-molecule ayo anenani elihlukile kanye nobukhulu. Ngaphezu kwalokho, ukuguqulwa kokushisa nomfutho womoya, kanye nejubane lomoya (umoya). Njengoba sidlula endaweni yokuqhuma ngesivinini esikhulu, indiza "iyawela" emigodini yomoya, isidumbu sayo sidonsela ngokufutheka, futhi salon kukhona okuthiwa "i-blubber". Ngokuvamile, izindawo ezinjalo zomoya zokungazinzi zikhona emoyeni phezulu kwezintaba nolwandle, kanye nasezihlanganisweni zezilwandle namazwekazi. Izingxenye ezinamandla kunazo zonke zengxubevange zingaphezu kolwandle lwasePacific Ocean. Futhi, ngokuqinisekile uyozizwa ukuthi yikuphi ukukhathazeka, uma indiza ingena ekudumazeni kwezulu.
Ingabe i-turbulence iyingozi yindiza?
Ngokwezibalo, izindiza zibhekene nezingxabano ngo-85-90% wezindiza. Ngesikhathi esifanayo, "i-bolt" ayikho ekusongeni okuncane okusongelayo. Izici zokwakhiwa kwezindiza zanamuhla zifana nokuthi umzimba we "nenyoni yensimbi" uyenzwa ucabangela ukuvunguza okukhulu. Ngaphezu kwalokho, lo mklamo uhlinzeka ngama-flaps akhethekile, okwandisa ukumelana nomfutho wezulu. Izitsha ezintsha kakhulu ezifakwe ebhodini usizo lwezindiza zokusiza ukuze zibone ngaphambi kwendawo ye-turbulence engenzeka futhi zigweme, zihluke kancane kulo mkhakha.
Into enhle kunazo zonke esongela umgibeli ngesikhathi sokuhamba kwendiza ngengozi yokulimala ingozi yokulimala uma, ngesikhathi eshaqhazelayo, eshiya isihlalo sakhe, akayikubopha noma awele emithwalweni engalungile esuka eshalofini eliphezulu. Uma kungenjalo, akukho isizathu sokuthuthumela. Amaqiniso azikhulumela wona: kusukela emvuthwandaba endizeni, akusikho indiza eyodwa eyaphazamiseka phakathi neminyaka engu-25 edlule.
Ukuhlukunyezwa kungabonakala kubi uma ukhona kulo mzuzu ekamelweni lendiza esikhundleni somgibeli. Uma siqhathanisa