Thundercloud. amafu Storm nemibane

Ukuna - kwizimanga zendalo apho iindleko zombane ibunjwa ngaphakathi emafini okanye phakathi ilifu phezu komhlaba. Xa zemozulu ezifana kukho amafu emvula amnyama. Ngokuqhelekileyo, le siganeko kunye neendudumo, izandyondyo zemvula, isichotho kunye nomoya onamandla.

ukubunjwa

Ukuba ahlasele ilifu, kufuneka ukuba izinto ezininzi ekuphuhliseni ulwazi lwengqiqo ezifana පිළිතුරු iimpendulo. Ezi zithinteli ukufuma ezaneleyo imvula kwaye iziqalelo ze amasuntswana ilifu ikwimeko ulwelo ngumkhenkce.

පිළිතුරු iimpendulo ikhuthaza kuduma kwezi meko zilandelayo:

• zokufudumeza ezimagqagala zezulu kufutshane kumphezulu womhlaba kwaye ngokwemaleko aphezulu. Umzekelo ilizwe ubushushu kunye namanzi kwiindawo ezahlukeneyo;

• ngexesha ukubana zezulu efudumeleyo kwiingcamba abandayo emoyeni;

• ubonakala storm ilifu ezintabeni kwi lift umoya.

Cumulus nganye enjalo linyathelo udlula ilifu, kwaye umbane oqolileyo ukubola yeqonga.

isakhiwo

I intshukumo kunye nokusasazwa kweentlawulo zombane ngeenxa ngaphakathi thundercloud - yinkqubo eqhubekayo narhoqo ukutshintsha. Ubume dipole evelele. intsingiselo yalo kukuba intlawulo ezigxekayo imi emazantsi efini kunye ezakhayo - phezulu. ion esesibhakabhakeni ezihamba phantsi kwempembelelo esigangeni yombane, obuyiyile imida emafini-ebizwa ngokuba uvikele umaleko, uvikele lobume umbane.

Kuxhomekeka kwindawo wejografi inqununu intlawulo ezimbi kulapho ubushushu ngu -5 ukuya -17 ° C. loxinano ophethe indawo 1-10 C / kwiikhilomitha cubic.

Moving thunderclouds

Izinga naziphi na ukulinganiselwa kwamafu, kubandakanywa umbane, kuxhomekeke intshukumo komhlaba. Temp ukubana Chance bodwa badla ufikelela 20 km / h, yaye ngamanye amaxesha onke 65-80 km / h. Isenzeko yokugqibela kwenzeka ebudeni intshukumo ezimbalwa esebenzayo abandayo. Kwiimeko ezininzi, ngexesha ekuweni iiseli uqhwithela yangaphambili kwasekwa elitsha.

Iindudumo amanyathelo ibangela amandla. Ikhoyo nokubakho bubushushu abagxothwa ephuma xa amafu umphunga, ekusekeni kwamathana efini. Uhlolo amandla ngokubanzi, iindudumo zingenziwa ngokusekelwe imali ye kwezulu.

ukwabiwa

Ngelo xesha kwiplanethi yethu, kukho amawakawaka amafu emvula apho avareji yenani umbane ifikelela nekhulu enye ngomzuzwana. Oko hhayi lonke isasazwe phezu komhlaba. Kule elwandle imozulu kukho izihlandlo ezilishumi ngaphantsi kwe kwi ukuhlasela. amafu Storm ngokuqhelekileyo zifumaneka kwiindawo amahlathi kunye sezulu. khupha umbane obukhulu bebekelwa Central Afrika.

Kwiindawo ezinjalo njengoko Antarctic kunye Arctic, nesiphango ayikho kukulawula. Kwelinye icala, kwiindawo intaba enjalo njengoko Cordillera kunye malayas ke ngengingqi eziqhelekileyo ukuze ezifana nesenzeko umbane nje thundercloud. Maxa wambi, imozulu oku kuyenzeka ixesha elininzi ehlotyeni ngexesha lasemini, yaye abafane ngokuhlwa kunye kusasa.

Iindudumo kwezinye izenzakalo zemvelo

Thundercloud lidla zikhatshwe imvula-kuvulelwa. Ngokomlinganiselo, kwimozulu enjalo 2 tsakisi amawaka. Kwezulu cubic. Xa izaqhwithi ezinkulu - izihlandlo ezilishumi kwangangoko.

Isaqhwithi (kwakunye nkanyamba) - a omtsha okudala thundercloud. Yena uya ezantsi, rhoqo kumgangatho osezantsi. It has indlela isiqu, lithatyathwe ilifu amakhulu iimitha ubukhulu. Ubukhulu be ifanele umenzi imalunga eziimitha ezine.

Ukongeza kwezi ngezenzeko zendalo thundercloud kunegalelo inkangeleko undizela nasekuh-. Le yokugqibela kuvela kwintaba ephakame apho ubushushu umoya ngaphantsi ngakumbi kokusingqongileyo. I-flow uba awubandi naxa linyibilike ice amasuntswana imvula ukuba idliwa amathontsi efini.

Zandise ehla umlambo yenza umahluko icace ngebala phakathi emoyeni kweshushu athi ndijonge. Movement ithala phambi kube lula ingqalelo yi nokwehla okukhulu lobushushu - degrees ezintlanu Celsius okanye ngaphezulu - yaye umoya onamandla (bakwazi ukufikelela kwi-50 m / s).

Intshabalalo inkanyamba ibe imilo setyhula, kunye downflow - line. Zombini ngezenzeko kungakhokelela ekugqibeleni kukhokelela imvula. Kwiimeko ezinqabe kakhulu, imvula ngokomphushu ngexesha lokuwa. Le nto ibizwa ngokuba 'isiphango owomileyo. " Kwezinye iimeko kwenzeka imvula, isichotho, uze emva koko ngomkhukula.

uthintelo ingozi

Kukho inani lwemithetho yokuziphatha ngexesha imozulu, nto leyo sikhatshwa iindudumo nemibane. amafu Storm iyingozi kakhulu ubomi kubo bonke abantu, hayi nje kuphela kweli ezitratweni (nangona oku umngcipheko omkhulu), kodwa kwakhona kufuphi window ngaphakathi. Kubalulekile ukwazi ukuba yamanzi umbane andibethe izakhiwo ubude. Oku kungenxa yokuba amasuntswana zombane balandela umendo ezilu-.

Xa kukho isiphango, zama ukuba abe kufutshane izikhululo zamandla kunye neentambo zothumelo, phantsi emide, imithi eyedwa kuyo kwindawo evulekileyo (ezifana intsimi okanye engcotyeni intlambo). Eyingozi kukuba siqubha emlanjeni, amachibi kunye namanye amaqumrhu zamanzi, kuba amanzi a conductivity elungileyo zombane.

Lo moya, nto leyo ephaphazela ngayo ilifu cumulonimbus, yeyela kwizowuni-gingxi. Kulapho kwezo zihlandlo, ukuthuthwa uqengqa kuzo zonke izalathiso phantsi yintshukumo ukugeleza efini. Abakhweli va Abokuhlunguzelelwa ngamandla, kwaye moya - ubunzima, leyo ayinqweneleki kakhulu kuye.

Kuye emngciphekweni omkhulu ukusetyenziswa izithuthuthu, iibhayisekile okanye ezinye izinto ezenziwe ngentsimbi. Kuyingozi kwakhona ukuba ubomi sibe nayiphi endulini, ezifana kophahla yezindlu, ezo thunderclouds basondeleyo. Iifoto kwezi ngezenzeko zendalo bacinge lobuhle kunye nokusebenza, kodwa esweni umngcipheko sezulu esitalatweni zinokubiza umntu ubomi bakhe.