Sihlale sihumusha umoya njengokuhamba komoya usuka kwenye indawo uye kwenye futhi asikwazi ukuwubona ngaphandle kokuthi uthwele isihlabathi noma izinto zokwakha. Ilukuluku labantu abasemoyeni livela ngokuthi kanjani into esingayiboni ingalinganiswa.
Ngabe bawukala kanjani umoya futhi yiziphi izinhlobo zomoya ezikhona? Ngabe ochwepheshe basuselwa kuphi lapho bebiza umoya ohambayo ngamagama ahlukile?
Kungani umoya wakheka?
Kunezindlela eziningana lapho umoya ungakhiqizwa khona. Imvamisa, okuvame kakhulu ukuthi kunamaphuzu amabili ezindaweni ezihlukene lapho kusungulwa khona phakathi kwabo umehluko ekucindezelekeni noma emazingeni okushisa. Uma kwenzeka ukuthi kunamaphuzu amabili lapho ingcindezi yehluka khona, izixuku zomoya zizojwayela ukusuka lapho kunengcindezi enkulu ziye lapho kuncane khona. Njengalapho sithatha ithubhu lomuthi wokuxubha, siyacindezela ukwenza ukuthi umuthi wokuxubha uphume udala umehluko wengcindezi. IPasta ijwayele ukugeleza isuke lapho kunengcindezi ethe xaxa iye lapho kunokuncane. Lo mehluko wengcindezi ubizwa ngabezimo zezulu umyela.
Ngoba kunobudlelwano obusondelene kakhulu phakathi komoya nengcindezi, amamephu we-isobar. Lawa mabalazwe e-isobar yiwo amele umehluko wengcindezi wona onikeza imininingwane ngejubane nokuhamba komoya. I-isobars yimigqa enengcindezi elinganayo. Ngakho ebalazweni lapho i-isobars isondelene kakhulu, izositshela ukuthi kunomoya omningi, ngoba endaweni encane, ukucindezela kushintsha kakhulu. Ngaphezu kwalokho, kuyathakazelisa ukugqamisa ukuthi kanjani indlela imimoya eziphatha ngayo ezifundeni ezahlukene.
Umthombo: http://sarablogcen.blogspot.com.es/2012/11/mapa-de-isobaras.html
Endabeni lapho umoya wakheke khona ngokwehluka kwamazinga okushisa, kwenzeka okunye futhi. Lapho isisindo somoya sithola izinga lokushisa eliphakeme kunalelo elizungezile, ivolumu yalo iyakhuphuka, okunciphisa ubukhulu bayo. Ngenxa yomphumela we-flotation, ubukhulu bomoya oshisayo buzokhuphuka, futhi indawo yayo izohlala ezinye izindimbane zomoya, ekuhambeni kwabo bazodala umoya. Lokhu kuhamba kwezixuku zomoya oshisayo noma obandayo wona kuwumthombo weziphepho eziningi zasehlobo futhi, ngezinga elikhulu, wemimoya egcwele ezindaweni ezishisayo. Ungabona futhi ukuthi lezi zinguquko zinethonya kanjani izenzakalo zemvelo, njenge Storm Eowyn.
Imiphumela yesiphepho uGaroe ngesinye isibonelo sokuthi umoya ungasithinta kanjani isimo sezulu sezindawo ezithile.
Ulinganiswa kanjani umoya?
Umoya ungalinganiswa ngezindlela ezahlukene nangamayunithi ahlukene. Okusetshenziswa kakhulu yile:
- Ukukala kwejubane lomoya ovundlile: insimbi esetshenziswa kakhulu i-anemometer izinkomishi, lapho ukujikeleza okufanayo kulingana nesivinini somoya. Iyunithi yokukala yi-km / h noma m / s.
- Isilinganiso sokuqondisa: ngoba lokhu kuyasetshenziswa isimo sezulu siyadamba, ekhombisa ukuthi umoya uvelaphi. Sikhuluma ngasenyakatho, empumalanga esenyakatho, eningizimu-ntshonalanga yomoya, njll. kuya ngokuthi ivelaphi.
Ukuze uqonde kangcono ubudlelwano phakathi komoya kanye nesivinini sawo, kubalulekile ukubhekisa ku Isikali seBeaufort, ehlukanisa amandla omoya.
Ezinye izinhlobo ezikhethekile zomoya
Umoya wasolwandle
Ngokuqinisekile ngolunye usuku olushisayo lolwandle uzwe umoya omuhle wasolwandle njengoba usondela ogwini. Imvelaphi yayo imi kanjena: Emini, umhlaba ushisa ngokushesha ukwedlula indawo yolwandle, ukuze umoya wangaphakathi uphume futhi uhlale umoya opholile ovela olwandle. Ebusuku, umhlaba uphola ngokushesha kunamanzi, ngakho-ke umoya ongaphezulu kolwandle ufudumele futhi uvame ukukhuphuka, ubangele ukuhamba komoya kusuka ezweni kuya olwandle. Ngalo mqondo, kuyasiza ukwazi imimoya egcwele eMedithera.
Kushaywa umoya ezintabeni nasezigodini
Kungenzeka ukuthi uye wezwa nomoya opholile okhiqizwa ebusuku ezigodini eziningi. Kulokhu, okwenzekayo yilokhu okulandelayo: Emini, umoya osesigodini ufudumala ngokushesha futhi uvame ukuphakama egqumeni. Ebusuku, umoya opholile uwenza uminyene futhi wehlele esigodini usuka eziqongweni. Lesi simo sihlobene nolunye uhlobo lomoya, njenge umoya katabatic.
Kubalulekile ukucabangela imiphumela yemimoya eyenza izimo ezimbi kakhulu.
Iziphepho
Umphumela odabukisayo ongaba nawo isiphepho waziwa kahle kubo bonke, ikakhulukazi uma uthinta izindawo ezakhiwe lapho izindlu nezakhiwo kungakulungele ukumelana namandla omoya angavela. Isiphepho yisimo sezulu esinobudlova esivela olwandle olushisayo, imvamisa ngasekupheleni kwehlobo noma ekuqaleni kokuwa. Imvelaphi yayo isesisindo esifanayo somoya oshisayo nomswakama okhuphuka ngokushesha. Ingcindezi yomoya isatshalaliswa ngokulandelana maphakathi nohlelo futhi ama-isobar ayimibuthano egxilile kakhulu eduze komunye nomunye. Esivunguvungwini, umoya ungafinyelela finyelela isivinini sama-250 km / h nakuba amanani ajwayeleke kakhulu ezungeze i-119 km/h. Ukuze uthole ukwaziswa okwengeziwe ngeziphepho, bheka isihloko esithi Isiphepho uKirk. Enkabeni yesiphepho kukhona okuthiwa "iso", indawo engenamafu nomoya omncane.
Tornados
Kuyisiphepho semimoya enamandla ehambisana nokwakheka kwamafu anesiphepho sohlobo lwe-cumulonimbus. Izinkanyamba zingaqala phezu komhlaba noma olwandle ukusuka ekukhuphukeni okusheshayo emoyeni ofudumele kakhulu. Ukuhamba komoya ngesimo sokuvunguza, kukunikeza ukubonakala okujwayelekile komphetho noma umkhono. Ukuvakasha kwakho kwezwekazi kungashuba phakathi kuka-1,5 km no-160 km uma kwenzeka kuba nesiphepho esinamandla. Lezo ezikhiqizwa phezu kolwandle zibizwa ngokuthi imikhono yasolwandle. Imimoya ekhiqizwayo icishe ibe ngu-180 km/h, nakuba kunezishingishane ezinesivinini esifinyelela ku-500 km/h. Ukuze uthole imininingwane eyengeziwe, ungabheka ulwazi mayelana izivunguvungu eSpain.
