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?
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. Ukuba ufuna ukufunda ngakumbi malunga nezi ziganeko, unokufunda malunga nazo amaza square.
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 ophuma phezu kolwandle usondele kufutshane nonxweme, yaye ekubeni kupholile, kudla ngokuba mnandi ehlotyeni, kodwa kubanda ebusika. Ukuba ufuna ukufunda ngakumbi malunga nefuthe lobushushu kwizinto ezinje, ungafunda malunga ne ICanelula.
Zenziwa nini?
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, njengoko umphezulu woMhlaba ufudumala ngakumbi. Ukuba ufuna ukwazi ngakumbi malunga nokuba ezi zintlukwano zichaphazela njani iimeko zemozulu, bona inqaku abalawuli bemozulu.
Eyona mimoya imnandi yenziwa entlakohlaza nasehlotyeni kuba ilanga liwufudumeza ngakumbi umhlaba kwaye namanzi asabanda ebusika. De amaqondo obushushu olwandle anyuke ngenxa yesiphumo sokuqhelaniswa, impepho yolwandle iya kuqhubeka ngakumbi. Lo mphumo unokufana neemeko ekuxutyushwe ngazo kwinqaku elithi ihlobo elishushu kummandla weMeditera.
Amandla omoya aveliswa ngumoya waselwandle axhomekeke kumahluko wobushushu. Umahluko omkhulu phakathi kweqondo lobushushu kwindawo zombini, isantya somoya siphezulu, ekubeni kukho umoya omninzi ofuna ukutshintshela umsantsa woxinzelelo oluphantsi oshiywe kukunyuka komoya ofudumeleyo. Le nto inxulumene ne-, eyenzeka ngenxa yentsebenziswano phakathi kwemida yomoya eyahlukeneyo.
Iimpawu zempepho yolwandle
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.
Ngamathub’ athile, i-convection eyenzeka phezu kobushushu bomhlaba kunye nokufuma okuqinileyo okuziswe ngumoya ojikelezileyo ukusuka elwandle kwakheka amafu akhula ngokuthe nkqo (abizwa ngokuba ngamafu e-cumulonimbus) anokukhokelela ekungazinzini kwe-atmospheric kunye nokuvelisa iindudumo ezinamandla kunye nemvula enkulu ngexesha elifutshane. Le yimvelaphi yezinye zezona mvula zidumileyo zasehlotyeni: ezo, ezithatha nje imizuzu engama-20, zishiye ngasemva umsinga wamanzi onokubangela umonakalo omkhulu. Ukuba unomdla wokufunda ngakumbi malunga neziganeko ezifanayo, ndincoma ukufunda malunga iinkanyamba eSpain.
Iziqithi kunye neemonons
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. Ukuba ufuna ukwazi ngakumbi ngolu hlobo lweziganeko zemozulu, unokujongana nenqaku amafu ozuko lwasekuseni.
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
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 obandayo ophuma emhlabeni udibana nomoya ofudumeleyo osuka phezu kolwandle, kubakho inkanyamba. yintoni eyaziwa ngokuba yi-terral. Umoya oshushu uvuthuza ubhekisa elwandle.
Ngolu lwazi, kuyacaca ukuba icace gca ukuba kutheni kubetha impepho yaselwandle.
