Phakathi kwezimo zezulu zezulu ezibhubhisa kakhulu nezibuhlungu kakhulu emhlabeni wethu sithola izivunguvungu neziphepho. Futhi kungenxa yokuthi lezi zimo zezulu zakhiwa ezindaweni nasezimweni ezithile futhi zingadala umonakalo omkhulu. Noma kunjalo, zikhona umehluko phakathi kweziphepho neziphepho abantu abaningi abakacaci ngokuphelele ngakho.
Kule ndatshana sizokutshela ngomehluko phakathi kweziphepho neziphepho.
Yini isiphepho
Ukwazi ukuthi yini umehluko phakathi kweziphepho neziphepho, kufanele siqale sazi ukuthi siyini isiphepho. Ingabe mayelana isisindo somoya esakhiwa nge-velocity ephezulu ye-angular. Ukweqisa kwesiphepho kutholakala phakathi kobuso bomhlaba nefu elifana ne-cumulonimbus. Yize kuyisimo somkhathi esinamandla, akuhlali isikhathi eside.
Kunezinhlobo eziningi zesiphepho ngokuya nge-morphology yazo nesikhathi esivame ukuzungeza. Kodwa-ke, ngokuvamile abanaso isikhathi eside kakhulu. Zivame ukutholakala phakathi kwemizuzwana embalwa nehora. Azikho iziphepho ezirekhodiwe ezinde kakhulu. Isiphepho morphology esaziwa kakhulu yileso sefeleni. Siyabona ukuthi ekugcineni okuncane kuthinta phansi futhi kuzungezwe ifu elikhukhula lonke uthuli nemfucumfucu evela kulo. Lesi isithombe esidala esisetshenziswa kuma-movie lapho ufuna ukubona ngeso lengqondo isiphepho.
Ijubane elingafinyelelwa yiziphepho liyatholakala phakathi kuka-65 no-180 km / h futhi ingaba ngamamitha angaba ngu-75 ububanzi. Awavamile ukuba sendaweni lapho akhiwa khona, kepha ahamba yonke insimu. Imvamisa bahamba amakhilomitha ambalwa ngaphambi kokunyamalala.
Ukwakhiwa kwesiphepho kwenzeka ushintsho ohlangothini futhi usheshise isivunguvungu. Lezi zinguquko zakha umphumela wokujikeleza ovundlile. Ngale miphumela, kwakhiwa izigaxa eziqondile lapho umoya ukhuphuka ukuphakama njengoba uzungeza ngaphakathi kwesiphepho. Lezi zimo zezulu zixhunyaniswe nezikhathi ezithile zonyaka. Imvamisa zenzeka nge imvamisa ephakeme ngesikhathi sokuwa nesikhathi sentwasahlobo. Ngaphezu kwalokho, zakha izikhathi eziningi emini kunezasebusuku. Imvamisa ephakeme kakhulu yeziphepho ekupheleni kosuku isantambama.
Yini isiphepho
Esinye isimo sezulu esisalele ukuthi sihlaziye yisiphepho. Zilinganiswe njenge- izivunguvungu ezinamandla kakhulu nezinodlame kakhulu ezingaba khona emhlabeni wethu. Ngokuya ngokuthi sikuphi, zingaziwa ngamanye amagama njengeziphepho noma izivunguvungu.
Ekubunjweni kwalolu hlobo lwesimo sezulu, sithola ukuthi kukhona inqwaba yomoya ofudumele noswakeme. Lezi zici zifana nomoya oshisayo. Lesi siphepho sisebenzisa lo moya ofudumele, onomswakama njengophethiloli ukwakha umoya ovunguza ngamandla. Njengoba lo moya ukhuphuka usuka ebusweni bezilwandle, ushiya izindawo ezingezansi zinomoya omncane. Njengoba sazi, ukuqondiswa komoya kujikeleza kusuka ohlangothini kusuka lezo zindawo lapho kunengcindezi ephezulu yomkhathi kuya lapho kukhona ingcindezi ephansi yasemkhathini.
Uma ukukhuphuka komoya oshisayo kushiya izindawo eziphansi zinomoya omncane, umoya uphendukela kuleyo ndawo ukumboza insimu. Lokhu kungenxa yokuthi endaweni enomoya omncane kunengcindezi ephansi yomkhathi. Lapho umoya osuthathe indawo yaleyo ngxenye engezansi ufudunyezwa futhi, uvame ukuphakama futhi ususe enye indawo enomfutho ophansi womkhathi. Lo mjikelezo ukhula ngokuqhubekayo kuze kube yilapho senza lokho esikwaziyo njengesiphepho.
Umoya oshisayo okhuphukile uyaphola futhi, njengoba unomswakama, wakhe amafu. Lawa mafu yiwona ekugcineni enza isiphepho.
Umehluko phakathi kweziphepho neziphepho
Uma siqhathanisa lezi zimo ezimbili zesimo sezulu, umehluko wokuqala wokuqala kulapho ziqala ukwakheka. Ngenkathi iziphepho Kuqubuka iziphepho ezindaweni ezisemhlabeni nezasogwini eduze nomhlaba.Iziphepho zivela olwandle. Akunakwenzeka ukuthi kube nesiphepho emhlabeni.
Ijubane lemimoya ngomunye umehluko omkhulu phakathi kwalezi zimo zezulu. Isivinini umoya ongasiphatha ngaphakathi kwesiphepho siphakeme kakhulu kuneseziphepho. Kodwa-ke, iziphepho, noma ngabe zinezivinini zomoya eziphansi, zihlala isikhathi eside. Ngenkathi iziphepho isivinini somoya singafinyelela amanani we-500 km / h, eziphephweni ezingadluli amakhilomitha angama-250 ngehora.
Kukhona futhi umehluko osayizi ophelele wesimo sezulu. Isiphepho esinosayizi ojwayelekile ngokuvamile siba ngamamitha ayi-400-500 ububanzi. Iziphepho, ngakolunye uhlangothi, zivame ukuba zikhulu kakhulu njengoba ububanzi bazo bufinyelela amabanga we kuze kufike kumakhilomitha ayi-1500. Lezi zinguquko ezilinganisweni zombili zezimo zezulu zingadala imiphumela emibi ehlukene ezindaweni ezenzeka kuzo.
Yize zombili lezi zimo zezulu zithinta kakhulu izindawo lapho zenzeka khona, umonakalo uhluke kakhulu. Iziphepho zivamise ukuhlasela izindawo ezinkulu ezifinyelela ngisho emazweni amaningi, kuyilapho iziphepho zihlasela kakhulu endaweni.
Esikhathini sobabili bezimo zezulu futhi singathola umehluko ocacile. Isiphepho sihlala kancane kakhulu kunesiphepho. Yize isiphepho sibhubhisa kakhulu, isigamu sempilo yaso sihlala imizuzu. Akuvamile ukuthi isiphepho singahlala ngaphezu kwamahora amaningana ubude. Ngokuphambene nalokho, kube neziphepho emlandweni wonke ezisebenze izinsuku ezingaphezu kwezingu-20.
Omunye umehluko endabeni yokubikezela. Lapho izazi zezulu zizama ukubikezela ukwakheka kwanoma iyiphi yalezi zimo zezulu zihlangabezana nezinkinga ezithile. Ngenkathi kwenzeka isiphepho, kulula ukubikezela indlela yokwakheka ngokuhlaziya okuguquguqukayo kwesimo sezulu, kunzima kakhulu ukwazi ukwakheka nendawo yenkanyamba. Ngalesi sizathu, kunabathandi bezimfundamakhwela abaziwa ngokuthi "abazingeli benkanyamba" abaphethe ukufuna nokuhlaziya lezi zenzakalo. Ukubikezela izivunguvungu kalula futhi kusebenza ukukwazi ukuthatha izinyathelo ezinqala zokuvikelwa kwazo kamuva.
Ngiyethemba ukuthi ngalolu lwazi ungafunda kabanzi ngomehluko phakathi kweziphepho neziphepho.