Wokuduma kwezulu. Namafu emvula nombani

Ukuduma - into yemvelo lapho amacala kagesi akhiwa ngaphakathi amafu noma phakathi ifu kanye ebusweni bomhlaba. Ngo sezulu okunjalo kukhona amnyama namafu emvula. Ngokuvamile, lesi sehlakalo wukuduma, imvula enkulu, isichotho umoya onamandla.

kumiswa

Ukuze umbelesele ifu, kumele ube izici eziningana sokuthuthukisa imiqondo ezifana Ukubika Inkinga YeWindows. Letakhi kukhona umswakama eyanele imvula izakhi izinhlayiya ifu usesimweni ketshezi neqhwa.

Ukubika Inkinga YeWindows ikhuthaza uma kuduma izulu kulezi zimo ezilandelayo:

• Ukushisa engalingani emoyeni eduze komhlaba futhi izingqimba layo elingenhla. Isibonelo salokhu ezahlukene lokushisa bemhlaba nemanti evele;

• ngesikhathi displacement we izikhatha zomoya oshisayo ezingqimbeni abandayo asemkhathini;

• isiphepho ifu livela ezintabeni i-lift emoyeni.

Isinyathelo ngasinye Cumulus enjalo ifu sihamba, futhi umbani ovuthiwe kwamazinyo esiteji.

isakhiwo

Le nhlangano yenkolo yokulwela nokusatshalaliswa amacala kagesi emhlabeni futhi ngaphakathi wokuduma kwezulu - lechubekako kanye ngokuqhubekayo kokushintsha. Isakhiwo dipole kuyinto evelele. ngencazelo yalo ukuthi icala negative itholakala ezansi efwini kanye omuhle - phezulu. ion Atmosphere lihamba ngaphansi kwethonya inkambu kagesi, wadala imingcele amafu okuthiwa avikele izingqimba, sivikele isakhiwo kagesi.

Kuye sendawo of icala uthishanhloko negative yilapho izinga lokushisa -5 ukuba -17 ° C. kwabantu isikhala lokushaja 1-10 C / cubic amakhilomitha.

Ukuhambisa thunderclouds

Izinga kwanoma iyiphi amafu, kuhlanganise umbani, kuncike ukujikeleza komhlaba. Temp ukufuduka Amathuba isehlane ngokuvamile ifinyelela 20 km / h, futhi ngezinye izikhathi yonke 65-80 km / h. Lo mkhuba yokugcina kwenzeka ngesikhathi ukunyakaza izimpi abandayo asebenzayo. Ezimweni eziningi, ngesikhathi kuwa owedlule isiphepho amaseli kwakhiwa ezintsha.

Nokuduma isinyathelo kubangela amandla. It is eziqukethwe ukushisa esicashile okuyinto ikhishwe uma umusi ukufingqa, ukwakha droplet efwini. Kuhlola amandla ngokuvamile, nokuduma zingenziwa esekelwe inani kwezulu.

ukusatshalaliswa

Ngesikhathi esifanayo eplanethini yethu, kunezinkulungwane namafu emvula lapho Inani eliyisilinganiso umbani ifinyelela eziyikhulu namashumi ngomzuzwana. Abenzi lutho ngokulinganayo basakaza phezu kobuso Earth. Eminyakeni izilwandle sezulu kukhona kancane izikhathi eziphindwe kayishumi ezwekazini. Storm amafu ngokuvamile atholakala izindawo ezishisayo sezulu nakwezifudumele. Ubuningi umbani esithweni tibheke eNkabeni Ye-Afrika.

Ezindaweni ezifana ne-Antarctic futhi e-Arctic, umsebenzi nokuduma akuyona ngokuyisisekelo. Ngakolunye uhlangothi, ezindaweni entabeni ezifana Cordillera kanye zaseHimalaya kukhona sezwe ajwayelekile ngoba enjalo umbani imihlola njengoba wokuduma kwezulu. Ngezinye izikhathi, isimo sezulu lokhu kwenzeka esikhathini esiningi ehlobo ngesikhathi sasemini, futhi kuyaqabukela kusihlwa futhi ekuseni.

Nokuduma nezinye izenzakalo zemvelo

Wokuduma kwezulu ngokuvamile uhambisana esindayo imvula-shower. Ngokwesilinganiso, kulesiya simo sezulu 2 sehla ayizinkulungwane. Kwezulu Cubic. Uma kuba nezivunguvungu emikhulu - kayishumi kunamahlathi.

Tornado (kanye kunenkanyamba) - a vortex ukuthi kudala wokuduma kwezulu. Uya phansi, ngokuvamile ezingeni phansi. It has uhlobo ipotimende, kwakhiwa kusuka ifu amakhulu amamitha ngosayizi. I ububanzi we uphondo uqobo mayelana amane amamitha.

Ngaphezu kwalezi zemvelo wokuduma kwezulu kunomthelela ukubukeka Squalls nasezansi. kuphakama Lesi sakamuva endaweni engamamitha lapho izinga lokushisa emoyeni esingaphansi imvelo. Ukugeleza iba ngisho ukubanda uma lincibilike ice kwezulu izinhlayiya ukuthi shabalala ku amaconsana amafu.

Lokusakaza ukwehla ekusakazeni yakha kunomahluko ocacile ngombala phakathi emoyeni ezinomswakama efudumele futhi abandayo. Movement ithala phambi kungenziwa kalula obonwa iconsi elibukhali lokushisa - degrees ezinhlanu Celsius noma ngaphezulu - futhi umoya onamandla (ongafinyelela futhi idlule 50 m / s).

Ukubhujiswa tornado abe ukuma isiyingi, futhi downflow - umugqa. Bobabili imihlola kuholele phambili ekupheleni nemvula. Ezimweni ezingavamile, imvula iyasha ngesikhathi sokuwa. Lesi senzakalo ngokuthi "isiphepho owomile." Kwezinye izimo zenzeka imvula, isichotho, bese kuba nesikhukhula.

zokuvimbela ingozi

Kunezindlela eziningana imithetho yokuziphatha phakathi sezulu, okuyinto kuhambisana ukuduma nokunyazima kombani. Namafu emvula iyingozi kakhulu ngenxa yokuphila kwayo yonke inyama sekufikile, hhayi nje kuphela emigwaqweni (nakuba lena enkulu kunazo zonke), kodwa futhi eduze kwefasitela endlini. Kubalulekile ukwazi ukuthi umbani esithweni ngokuvamile bashaya kwamabhilidi amade. Lokhu kungenxa yokuthi izinhlayiya kagesi silandele indlela okungenani ukumelana.

Phakathi nokuduma, zama hhayi ukuba eduze iziteshi ezikhiqiza amandla zikagesi, ngaphansi ubude, izihlahla oyedwa endaweni evulekile (ezifana ensimini noma edlelweni esigodini). Dangerous is zibhukuda emfuleni, amachibi kanye nezinye machibi, kusukela amanzi has a conductivity ezinhle kagesi.

Indiza, okuyinto izimpukane engale cumulonimbus, iwela indawo ye omawala. Ngezikhathi ezinjalo, ezokuthutha Rolls kuzo zonke izindawo ngaphansi isenzo ukugeleza efwini. Abagibeli uzizwe kuzamazama okunamandla, futhi indiza - ubunzima, okuyinto kakhulu engathandeki ngaye.

It has a ingozi eliphezulu ukusetshenziswa izithuthuthu, amabhayisikili noma ezinye izinto ezenziwe metal. Libuye eyingozi empilweni ukuba kunoma iyiphi egqumeni, ezifana kophahla yezindlu, okuyizinto thunderclouds abaseduze. Izithombe kulezi zinkanyezi zemvelo kunikeze umuzwa ubuhle kanye nempumelelo, kodwa ukuqapha ingozi sezulu emgwaqweni kungadla indoda ukuphila kwakhe.