Ngokuqinisekileyo wakhe wazibona iindudumo kunye nombane kwaye ungomnye weentlobo ezimbini zabantu abajamelene nezi ziganeko zemozulu: ungabazonda okanye uyabathanda. Iindudumo nemibane Ngokwesiqhelo zizinto ezimangalisayo ezifanele ukubanjwa kunye neekhamera kunye nevidiyo. Ukuba zenzeka ebusuku, zinomtsalane ngakumbi kwaye zintle ngokumangalisayo.
Nangona kunjalo, uyazi ukuba kutheni zisenzeka kwaye yeyiphi eyona ndlela yokuzikhusela kuyo? Ukuba ufuna ukufunda ngakumbi malunga neenkqwithela nombane, le yiposti yakho 🙂
Inkcazo yesiphepho
Uqhwithela aluyonto ngaphandle kokuphazamiseka kogonyamelo kubume bomoya obonakala ngokuba imvula enkulu, umoya ovuthuzayo, imibane neendudumo, kwanesichotho ngamaxesha athile. Ngokubanzi, ziziganeko zemozulu ezihlala ixesha elifutshane (malunga nemizuzu engama-20 okanye iyure enye) kwaye zichaphazela indawo ethile kuphela.
Ezi zivunguvungu zenzeka rhoqo kwiindawo apho ubushushu buphantsi okanye buphakathi. Ingxelo yehlabathi yommandla onezona nkqwithela zinkulu ithathwa sisiqithi saseJava, ngaphezulu kweentsuku ezingama-225 zesaqhwithi nemibane ngonyaka.
Usenza njani isaqhwithi?
Kuyathakazelisa ukubona isaqhwithi sombane okanye, ngokuchaseneyo, into eyingozi kakhulu ukuba ukwiindawo ezingathandekiyo. Izaqhwithi zenzeka xa umoya usenzeka umoya okhoyo phezulu onamandla.
Xa umoya oshushu womphezulu unyuka, ubalekela kumaleko omoya opholileyo phezulu kwaye ujikeleze uye kuma kumafama asakhulayo athe nkqo. La mafu aqala njenge i-cumulus humilis Kwaye bajike kuloo mbonakalo yomqhaphu ocolekileyo. Njengokuba ukungazinzi komoya okukhoyo okubangelwa ngumoya womoya okhulayo phezulu kukhula, ngokuthe nkqo amafu asakhulayo aguquka abe icumulus congestus.
Xa ilifu likhulu kakhulu, kuyabizwa cumulonimbus kwaye ukhuphe onke amanzi agciniweyo.
Ukwenziwa kwesiphango sahlulwe sangamanqanaba amathathu:
Isigaba sokuqala
Amaza omoya anyukayo abangela ilifu lamafu ukuba lenze. ukuya kuthi ga kwi-7.500 yeemitha zokuphakama. Ilifu liqokelela amathontsi amanzi lize lenze imilo.
Inqanaba lesibini
Xa ilifu likhula nangaphezulu, lifikelela kubude obuyi-12.000 yeemitha, ngokuhlala phantse kuwo wonke ummandla wetroposphere. Ngenxa yomahluko wamaqondo obushushu awenzekayo phakathi komaleko ongezantsi womoya okhulayo kunye nomaleko kubude apho ilifu lenza khona, ngaphakathi ngaphakathi banokurekhodwa ukuya kumaqondo obushushu angama -40 kunye nama-50 degrees.
Uhlaziyo lunokufikelela kwisantya ukuya kuthi ga kwiikhilomitha ezili-100 ngeyure. Xa zingqubana nelifu, amathontsi omoya ngaphakathi kuwo ayajiya kwaye agcinwe kumathontsi amanzi anomkhenkce, iikristali zekhephu kunye nakwiikhephu, ngokuxhomekeke kumaqondo obushushu asezantsi.
Xa bewela phantsi kobunzima babo, bapholisa umoya oshushu kumanqanaba asezantsi kwaye, ngenxa yoko, bawenze ube nzima. Kulapho xa umoya owehlayo wenziwa ngesantya esimalunga neekhilomitha ezingama-50 ngeyure ethwala yonke imvula kunye / okanye ikhephu elijongise kumphezulu womhlaba. Esi sizathu sokuba uninzi lwamathontsi emvula akho kwisaqhwithi makhulu.
Isigaba sesithathu
Xa ilifu ligcwaliswe ngokupheleleyo ngamathontsi amanzi kwaye kukho umoya okhoyo ezantsi, ukhuphelo olupheleleyo kwimizuzu.
Njengoko ilifu liphulukana namanzi kunye nomthamo, umoya ophantsi uyayeka kunye nelifu, elona nxalenye liphezulu, lisasazwa ngumoya. Esi sesona sizathu sokuba izaqhwithi zihlala ixesha elifutshane kodwa zinamandla kakhulu.
Izaqhwithi nemibane
Enye yezinto ezenzeka ngexesha lesiphango ngumbane. Imitha ayikho enye into ngaphandle umothuko omfutshane wombane ezenzeka ngaphakathi kwilifu, phakathi kwelifu kunye nelifu okanye ukusuka kwilifu ukuya kwinqanaba emhlabeni. Ukuze umqadi ubethe emhlabeni, kufuneka uphakanyiswe kwaye kufuneka kubekho into ebonakalayo ngaphandle kwabanye.
Amandla ombane aphindwe kaliwaka kunale ikhoyo ngoku ekhaya. Ukuba siyakwazi ukubanjwa ngumbane ngokuphuma kwiplagi, cinga ukuba umbane unokwenza ntoni. Nangona kunjalo, zininzi iimeko apho abantu babethwe ngumbane, basindile. Kungenxa yokuba ubude bomqadi bufutshane kakhulu, ngoko ke ubukhulu bayo abubulali.
Ziyimitha ekwazi ukusasaza malunga neekhilomitha ezili-15.000 ngeyure kwaye ulinganise ubude malunga nekhilomitha enye. Ukuya kuthi ga kwiikhilomitha ezintlanu imibane ebhalileyo ebhaliswe kwisaqhwithi esikhulu kakhulu.
Kwelinye icala, siyaduduma. Iindudumo kukudubula okubangela ukukhutshwa kombane okwaziyo ukuduma ixesha elide ngenxa ye-echoes eyenzeka phakathi kwamafu, umhlaba kunye neentaba. Ubukhulu kunye nokuxinana kwamafu, kokukhona isandi senzeka phakathi kwawo.
Ngenxa yokuba umbane uhamba ngokukhawuleza ngenxa yesantya sokukhanya, sibona umbane ngaphambi kokuba sive iindudumo. Nangona kunjalo, oku kwenzeka ngaxeshanye.
Uveliswa njani umbane
Umbane unokumelwa ngokugqibeleleyo sisenzeko esenzeka ekhayeni lethu xa sidibanisa ngokungafanelekanga iipali ezintle zombane. Xa sisenza oku, sifutshane ukujikeleza isikhokelo.
Olo hlaselo lufutshane silibonayo xa sibangela isekethe emfutshane sisebenza umbane kodwa ngezinga elincinci. Le nto yenzeka phakathi kwamafu anegunya elichasene nombane. Ngaphakathi kwilifu kukho iipali ezichaseneyo eziphelweni ezijolise kwityala elilungileyo nelingalunganga naphakathi kwamafu nomhlaba.
Xa oku kusenzeka, umbane uvela phakathi kwelifu, phakathi kwelifu kunye nelifu, naphakathi kwelifu nomhlaba. Ukukhutshwa ngakunye kuhlala isiqingatha somzuzwana kwaye, nangona kunika umbono wokuba ngumbane kuphela, kukho amawakawaka okhuphelo.
Ngolu lwazi uya kuba nakho ukwazi okungakumbi malunga nokwenziwa kwezaqhwithi kunye nesizathu sokubakho kwazo.