Umoya wolwandle

Umoya wolwandle entwasahlobo

Ngokuqinisekileyo ukhe wayiphawula impepho yolwandle kulusu lwakho kwaye uye wazibuza ukuba yenziwa njani kwaye kutheni. Zombini uMhlaba kunye namanzi ziyaqhubeka nokufudumeza nokupholisa kunikwa umahluko kumaqondo obushushu athi abekho phakathi kwemini nobusuku. Xa umoya osemoyeni ushushu nangaphezulu kunesiqhelo emini, imimoya ephezulu yomoya yenzeka, yenze umoya wolwandle.

Ngaba uyafuna ukwazi ngakumbi malunga nomoya opholileyo wolwandle?

Yenziwa njani?

Ukuyilwa komoya waselwandle

Umoya wolwandle ubizwa ngokuba yi-virazón. Ngenxa yomahluko wobushushu phakathi kwemini nobusuku, umphezulu wobushushu uyaphola ngokujikeleza. Oku kubangela umphezulu woMhlaba, xa ushushu ngaphezulu kwesiqhelo kwaye wenza njalo phambi komphezulu wolwandle, Yenza ishushu, inyuke imisinga yomoya.

Xa kunyuka umoya oshushu, kuba ushushu kunendawo engaphezulu yolwandle, ushiya umsantsa ophantsi woxinzelelo. Umoya uphakama ngokunyuka xa usiya ushushu kwaye umoya obandayo osondeleyo kumphezulu wolwandle ushiya indawo enoxinzelelo oluphezulu, olwenza ukuba ufuna ukuthatha indawo eshiywe ngumoya ophakamileyo. Ke ngoko, ubunzima bomoya kunye noxinzelelo oluphezulu ngaphezulu kolwandle buhlala buhamba ngaphezulu kwendawo yoxinzelelo esezantsi ekumhlaba.

Oku kubangela ukuba umoya ovela kumphezulu wolwandle ungene elunxwemeni kwaye upholile kuhlala kumnandi ehlotyeni, kodwa kubanda ebusika.

Zenziwa nini?

Umoya wolwandle

Imimoya yomoya elwandle nangaliphi na ixesha. Kuyimfuneko kuphela ukuba ilanga lifudumeze umphezulu kubushushu obuphezulu kunomoya ojikeleze umphezulu wolwandle. Iintsuku ezinomoya omncinci ngokubanzi, kungabakho impepho yaselwandle engaphezulu, kuba umphezulu womhlaba ushushu ngakumbi.

Eyona mpepho imnandi ukuyiva yakhiwa entwasahlobo nasehlotyeni ngenxa yento yokuba ilanga lifudumeza ngaphezulu komhlaba kwaye amanzi asabanda ebusika. Kude kube kunyuka amaqondo obushushu elwandle ngenxa yempembelelo yolwakhiwo, umoya wolwandle uya kuqhubeka ngakumbi.

Amandla omoya aveliswa ngumoya waselwandle axhomekeke kumahluko wobushushu. Umahluko omkhulu phakathi kweqondo lobushushu kwindawo zombini, isantya somoya siphezulu, kuba kukho umoya omninzi ofuna ukubuyisela umsantsa ophantsi oshiyekileyo ngokunyuka komoya oshushu.

Iimpawu zempepho yolwandle

Umoya wolwandle ubaleka

Umoya wolwandle uthanda ukubetha ngokungxama kunxweme kwaye uyakwazi ukufikelela Iikhilomitha ezingama-20 ukuya elwandle. Kuba umahluko wobushushu obomeleleyo uyimfuneko phakathi komhlaba kunye nolwandle umphezulu, amandla aphezulu omoya wolwandle afezekiswa emva kwemini, xa ilanga lishushu ngamandla. Isantya somoya sikwaxhomekeke kubume bendawo. Nangona imimoya evuthuza nethandekayo, ukuba ubume bomhlaba buzinzile, umoya unokufikelela kumaqhina angama-25.

Ngamanye amaxesha, ukuhanjiswa okwenzeka ngaphezulu kweqondo lobushushu bomhlaba kunye nokufuma okunamandla okuziswe ngumoya ojikeleze ulwandle, kwenza amafu aphuma ngokuthe nkqo (abizwa ngokuba yi-cumulonimbus) anokubangela iimeko zokungazinzi komoya kwaye avelise izivunguvungu zombane imvula enkulu ngexesha elifutshane. Le yimvelaphi yezaqhwithi ezaziwayo zasehlotyeni: ezo zithi kwimizuzu nje engama-20, zishiye impompo yamanzi enokudala umonakalo omkhulu.

Iziqithi kunye neemonons

ngokuthe nkqo ukukhula kwamafu

Iziqithi zikwanempembelelo yempepho yolwandle kunxweme lonke. Ngokwesiqhelo, bakwaphakama nasemva kwemini. Oku kuthetha ukuba zonke ezona ndawo zifanelekileyo zokumisa izikhephe zisezantsi kwaye kunzima ngakumbi ukufumana enye apho umoya wolwandle ungavuthuzi okanye ubuthathaka.

Ngempembelelo efanayo enika umoya wolwandle, ezinye zeemonco ziyenziwa. Esi siphumo sokuhlala komoya obandayo kwindawo yoxinzelelo oluphantsi eshiywe ngumoya oshushu okhulayo, inyuswe iye kwinqanaba elikhulu, yenza imimoya ibe namandla ngakumbi kwaye yenze uxinano olukhulu kwaye ibe yingozi ngokuthe nkqo ekuphuhliseni amafu. La mafu ashiya imvula eninzi njengoko injalo iimvula kwiindawo ezikufutshane neHimalaya.

Ehlotyeni, izihlwele zomoya zoMzantsi-mpuma weAsia ziyafudumeza kwaye ziphakame, zishiya indawo yoxinzelelo oluphantsi emhlabeni. Le ndawo ithathelwa indawo ngumoya obandayo ovela elwandle opholileyo ovela kuLwandlekazi lwaseIndiya. Xa lo moya udibana nendawo efudumeleyo, ufikelela kwiintaba eziphakamileyo kwaye uqalise ukunyuka kwawo de ufike kwiindawo eziphakamileyo kwaye uphole, unike imvula enkulu kakhulu.

Ingingqi

Unxweme

Sayibiza ngokuba yi-terral kuba inxulumene nomoya wolwandle, nangona imeko kunye nefuthe lazo zichasene ngokupheleleyo. Ebusuku, umphezulu womhlaba uyaphola kuba ilanga alisebenzi. Nangona kunjalo, umphezulu wolwandle ugcina ngcono ubushushu obufunxwe imini yonke ngeeyure zokukhanya kwelanga. Le meko ibangela ukuba umoya uvuthuze ujonge kwelinye icala, oko kukuthi, ukusuka emhlabeni ukuya elwandle. Oku kwenzeka ngenxa yokuba iqondo lobushushu lomoya kufutshane nomphezulu wolwandle liphezulu kunelo lomhlaba kwaye ivelisa indawo enoxinzelelo olusezantsi lomoya. Ke ngoko, umoya obanda kakhulu emhlabeni ufuna ukugubungela lo mmandla woxinzelelo oluphantsi kwaye uvelise umoya wolwandle kwicala lomhlaba wolwandle.

Xa umoya obanda kakhulu emhlabeni udibana nomoya ofudumeleyo ovela elwandle, kuyenziwa yintoni eyaziwa ngokuba yi-terral. Umoya oshushu uvuthuza ubhekisa elwandle.

Ngolu lwazi, kuyacaca ukuba icace gca ukuba kutheni kubetha impepho yaselwandle.


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  1. Uxanduva lwedatha: UMiguel Ángel Gatón
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