Ukubona isimo sezulu yinto esiyenza nsuku zonke. Kodwa-ke, kungenzeka singaqondi kahle lapho usokhaya ekhomba ebalazweni. Sibona imephu yaseSpain enemigqa eminingi, izimpawu nezinombolo. Zisho ukuthini zonke lezo zimpawu?
Lapha ungafunda konke odinga ukukwazi funda ibalazwe lesimo sezulu futhi uyiqonde ngokuphelele. Vele uqhubeke ufunda bese ubuza uma unemibuzo
Izimiso eziyisisekelo zebalazwe lesimo sezulu
Amamephu wesimo sezulu ahlinzeka ngokumela okwenziwe lula kwezimo zezulu zamanje noma zesimo sezulu endaweni. Indlela evame kakhulu iwukuhlaziya indawo engaphandle, njengoba kulapho isimo sezulu sisithinta khona. Imiqondo evamile ye-meteorology kulula ukuyiqonda. Abantu abaningi badinga ulwazi mayelana imvula, imimoya, uma kuneziphepho, isichotho, iqhwa, Njll
Lezi zici zibaluleke impela uma kukhulunywa ngesikhathi sokuqonda. Kuthatha ini ukuze line, kungani kwenzeka, futhi kuzoqina kangakanani. Ukuqonda ukusebenza kokuguquguquka okuningi kwesimo sezulu kubaluleke kakhulu ukwazi ingcindezi yasemkhathini. Umfutho we-atmospheric, ezimweni eziningi, unquma isimo sezulu. Ezindaweni lapho umfutho womkhathi uphakeme, isimo sezulu esihle, esomile siyabusa. Ngokuphambene nalokho, uma iphansi, kuyoba nomoya oswakeme kakhulu nesimo sezulu esibi. Ngaphezu kwalokho, ungakwazi uthintane yethu amamephu we-synoptic ukubuka ulwazi lwesimo sezulu ngokucacile.
Ukubaluleka kwengcindezi yasemkhathini
Lapho kunohlelo lokucindezela oluphakeme kungukuthi isisindo somoya ojiyile. Lokhu kungenxa yokuthi umoya upholile futhi womile kunomoya ozungezile. Uma lokhu kwenzeka, umoya osindayo uwela ohlelweni lokucindezela. Ngalesi sikhathi, kulapho unesimo sezulu esihle futhi esinamafu ambalwa.
Ngakolunye uhlangothi, lapho sinesistimu yengcindezi ephansi, kusho ukuthi ubukhulu bomoya bukhulu kakhulu. Lokhu kungenxa yokuthi umoya uswakeme kakhulu noma uyashisa. Ngakho-ke, umoya ozungezile ungena ngaphakathi, uye enkabeni yohlelo, ngenkathi umoya okhanyayo ukhuphukela phezulu. Lapho ukukhanya, umoya ofudumele uphakama futhi uhlangabezana nezendlalelo ezipholile, uhlangana ube ngamafu. Njengoba amafu ekhula amile, amafu emvula adumile akha.
Kuzinhlelo lapho ingcindezi iphansi kakhulu kwakhiwa iziphepho. Lawa mafu azokwakha futhi ahambele esibhakabhakeni. Ukuze lamafu akheke, umoya oshisayo, onomswakama kufanele ukhuphuke ngokwanele ukuze ukhiqize ukukhula okuqondile.
Uma ubona imephu yesimo sezulu zama ukuhlaziya ukuthi bayilinganisa kanjani ingcindezi. Imayelana nokukala lokho okusindwa umoya phansi. Iyunithi yokukala yi-millibar. Lokhu kubalulekile ukwazi ngoba amaphethini amaningi wesimo sezulu ahlotshaniswa nengcindezi yasemkhathini. Inani eliphansi lengcindezi olwandle ngu-1013 mb. Uma sinesistimu yokucindezela okuphezulu, imvamisa ifinyelela kumanani we-1030 mb. Kodwa-ke, lapho uhlelo lunomfutho ophansi, amanani angehla aze afike ku-1000 mb noma ngaphansi. Ukuze uthole ukuqonda okungcono kokuhlukahluka kwesimo sezulu, ungabona interactive sezulu imephu.
Izimpawu ebalazweni lesimo sezulu
Ukuze ufunde izimpawu ezibaluleke kakhulu ebalazweni lesimo sezulu, kufanele unake izimpawu zokucindezela. Ukuze ufunde ingcindezi engaphezulu ye-barometric, hlola isobars. Le yimigqa ekhomba inani elifanayo lengcindezi yasemkhathini yezindawo ezahlukahlukene. Lokho wukuthi, uma sibona imephu lapho imigqa ye-isobar isondelene kakhulu khona, kuzoba nesimo sezulu esibi. Lokhu kungenxa yokuthi ebangeni elifushane, amanani engcindezi ayashintsha. Ngakho-ke, kukhona ukungazinzi komkhathi.
Imigqa ye-isobar imaka ijubane nokuqondisa komoya. Umoya uqondiswa kusuka ezindaweni lapho kunengcindezi enkulu yomkhathi kuya lapho kuncane khona. Ngakho-ke, lolu lwazi singalwazi ngokuhlaziya amanani ama-isobars. Uma sibheka ama-isobars abekwe emibuthanweni emincane, isikhungo sikhombisa isikhungo sengcindezi. Kungaba kokubili ukuphakama, ngophawu A, nangaphansi, ngophawu B.
Kufanele sazi ukuthi umoya awugelezi uye phansi kuma-gradients okucindezela. Ihamba nxazonke ngenxa yomphumela we-Coriolis (wokuzungeza komhlaba). Ngakho-ke, ama-isobars ahamba ngewashi angu-anticyclonic flows kanti okuphambene nawo ukugeleza kwe-cyclonic. I-anticyclone ifana namazinga okushisa aphezulu kanye nesimo sezulu esihle. Isivunguvungu ukungazinzi komkhathi okuholela esiphephweni. Lapho ama-isobars esondelene komunye nomunye, isivinini somoya sizoba namandla. Uma ufuna ulwazi olwengeziwe mayelana nokuthi lezi zenzakalo zilinganiswa kanjani, ungavakashela isigaba sethu kokuthi real-time sezulu izicelo.
Ukuhunyushwa kohlelo lwengcindezi ephansi futhi ephezulu
Lapho kwenzeka isiphepho ngokuvamile sihambisana neziphepho ngokwanda kwamafu, imimoya, amazinga okushisa nemvula. Lokhu kumelelwe ebalazweni lesimo sezulu ngama-isobars asondelene kakhulu. Imicibisholo ihamba ngokuphikisana newashi enyakatho Nenkabazwe futhi eno "T" phakathi isobar.
Izimo zengcindezi ephezulu azimele imvula. Umoya uya woma futhi bamelwe ngu-H phakathi nesobar. Imicibisholo ijikeleza lapho umoya ubheke khona. Ngendlela yewashi enyakatho nenkabazwe. Ungaphinda ubheke kumhlahlandlela wethu ku ama-anticyclone kanye nokucindezeleka ukuqonda okwengeziwe ngalezi zenzakalo.
Izinhlobo zangaphambili
Kumamephu wesimo sezulu asikhombisa kuthelevishini, izingqimba ziyabonakala zikhonjisiwe. Uma imingcele idlula endaweni, kungenzeka kakhulu ukuthi isimo sezulu sizohluka. Izintaba namanzi amakhulu kungaphambukisa indlela yakho.
Kunezinhlobo ezahlukahlukene zezingqimba futhi zimelwe ebalazweni lesimo sezulu ngezimpawu ezahlukahlukene. Eyokuqala ingaphambili elibandayo. Lapho umphambili obandayo udlula endaweni, maningi amathuba okuthi imvula izoba nesikhukhula futhi kube nomoya onamandla. Kumamephu wesimo sezulu amelwe yimigqa eluhlaza okwesibhakabhaka nonxantathu ohlangothini lwendlela yokuhamba esuka ngaphambili.
Uhlobo lwesibili ingaphambili elifudumele. Kusho ukunyuka kwamazinga okushisa njengoba kusondela. Isibhakabhaka sicwebezela ngokushesha njengoba ingaphambili lidlula. Uma umoya ofudumele ungazinzile, ukuduma kwezulu kungase kwenzeke. Zimelelwe ebalazweni lesimo sezulu ezinemigqa ebomvu nama-semicircles ohlangothini ezibheke kulo.
Uhlobo lokugcina luyi-front occluded. Kwakhiwa lapho ingaphambili elibandayo lifica elifudumele. Zihlotshaniswa neminye imiphumela yesimo sezulu njengeziphepho. Kungaba nokuvaleka okufudumele noma okubandayo. Lapho ingaphambili elivalekile lingena, umoya uya woma. Zimelelwa ulayini onsomi namasendilinga nonoxantathu lapho kuqondiswa umoya.
Ngethemba ukuthi ngalolu lwazi ungafunda ukuhumusha imephu yesimo sezulu. Uma unemibuzo, yishiye kumazwana. Sizokujabulela ukuphendula
Ngiyabonga kakhulu uchazwe kahle, ngixhunywe ekufundeni ukutolika kahle isikhathi.
Ngiyabonga kakhulu ngevidiyo nangemibhalo. Ngifunde okuningi futhi bengifuna izibonelo eziningi.
Ngalesi siphepho osikhulumile ukuthi sisenyakatho ne-Italy, ubheka ukuholwa ngumoya okuzodalwa yilokhu, lapho umoya uvela ezwenikazi i-Europe, kungaba umoya owomile onamathuba amancane emvula?
Gracias!