Ukuguquka kobushushu

Kwi-troposphere, amaqondo obushushu ayancipha njengoko sikhula kubude. Ngenxa yoko, kuyinto eqhelekileyo ukuba kubanda kwiindawo ezisezintabeni kunasemanzini. Nangona kunjalo, kukho izinto ezithile zemozulu ezenza utshintsho kule gradient ezibangela ukuba zibuyiselwe umva. Yaziwa njenge Ukuguquka kobushushu. Yinkqubo apho ubushushu bukhuphukela phezulu.

Kweli nqaku siza kukuxelela ukuba yintoni inversion ye-thermal, ivela phi kwaye inxulumene njani nongcoliseko lomoya.

Yintoni inversion ye thermal

Yinkqubo apho ubushushu bonyusa ukuphakama. Oko kukuthi, kwezona ndawo ziphantsi esixekweni, umzekelo kwinqanaba lolwandle, sifumana amaqondo obushushu asezantsi kunokuba sinyuka intaba. Kuyinto eyahlukileyo koko kuqhele ukwenzeka.

Oku kuguqulwa kwe-thermal kungenxa yeemeko ezithile ezikhethekileyo apho kuhla khona umoya obandayo kwaye uhlale uzinzile. Masikhumbule ezinye iikhonsepthi ezisisiseko zeemeko zemozulu. Xa kukho ii-anticyclone umoya uyehla uye kwiindawo eziphezulu kwaye kwisaqhwithi senza okwahlukileyo. Sebenza indlela yakho ukuya kwiindawo eziphezulu. Inversion ye-Thermal yenzeka phantsi kweemeko ze-anticyclone kunye nozinzo olukhulu lomoya.

Kwi-inversion ye-thermal sinokubona ukuba umoya obandayo ovela kumaleko aphezulu wehlela njani kwimiqolo esezantsi kufutshane nomphezulu womhlaba. Oku kuhamba ezantsi komoya obandayo kwaziwa njenge-Subsidence. Kukho konke oku kwehla, umoya ucinezelwe ngakumbi nangakumbi, ukwandisa uxinzelelo kunye nokunyusa iqondo lobushushu. Ukongeza, ilahla ukufuma ngenxa yoko akukho mafu. Siyayibona indlela, xa ifikelela ngaphezulu, iyanda kwaye iyahluka. Oku kuyenza ukuba isasazeke ngaphezulu kobuso bonke budala ubeko lozinzo.

Yenziwa njani inversion ye thermal

Amafu okuguqula ubushushu

Ukunyuka okuphezulu kobunzima bomoya ngenxa yokufudumala kwehlabathi kuthintelwe kwaye kunye nokubakho kokungazinzi. Ukungabikho kwezi ntshukumo zomoya kuthintela ubunzima bomoya bamaqondo obushushu ohlukileyo ekuxubeni. Xa ubusuku buza, umhlaba uphulukana nobushushu obufikelele emini ngenxa yemitha yelanga ngokukhawuleza. Obu bushushu budluliselwa emoyeni onxibelelana nomhlaba. Umoya obandayo unzima kakhulu kwaye ubekwa emazantsi entlambo kwaye ke, ngexesha lakusasa amaqondo obushushu ayabanda.

Kufuneka kukhunjulwe ukuba kwezi meko ze-inversion ye-thermal umoya wehla ukusuka kumanqanaba aphezulu kwaye ufudumale phezulu ukuze umoya ofudumeleyo uhlale ngaphezulu komoya obandayo. Oku kubangela iplagi okanye isiciko sokwenza. Kuba ukushukuma okuphezulu komoya kuthintelwe ngokupheleleyo kuba akukho moya unikwe uzinzo olukhulu, ezi zimpawu zeempawu ezahlukileyo azixubeki kwaye ke ngenxa yoko inversion ye-thermal yenzeka.

Into eqhelekileyo kukuba ubushushu bomoya buyancipha ngobude, kodwa kule meko kukho inversion ye-thermal.

Kutheni le nto isenzeka

Ukuze inversion ye-thermal yenzeke, iimeko ezahlukeneyo kufuneka zenzeke. Ebusuku, umhlaba uphola ngokukhawuleza, ulahlekelwe bubushushu obuqokelelwe emini. Lo maleko womoya unobushushu obuphantsi kunalowo uphakamileyo kwangoko. Oku kuthetha ukuba umoya unexinano ezahlukeneyo, ezibathintela ekuxubeni. Njengoko ilanga livela kwakhona liqala ukulungisa inversion ye-thermal kwaye inuka ukufudumeza umhlaba, ubuyisele iimeko eziqhelekileyo.

Le nto yenzeka kakhulu kwimimandla yeentlambo njengoko ukupholisa ngemitha kukhulu. Ukuba kukho umahluko omkhulu phakathi kobushushu bemini nobusuku, kunokwenzeka ukuba kukho inversion ye-thermal. Xa kukho inversion ye-thermal iyabonakala ngokulula. Oku kungenxa yokuba inkungu okanye umsi udla ngokugxila kufutshane nomphezulu womhlaba. kwaye yandisa ngokuthe tye. Kuqheleke kakhulu ukwenzeka kwiindawo zolwandle nakwiingingqi zentlambo. Ngokwesiqhelo kwenzeka kwiindawo apho, ngenxa ye-morphology yayo, ukujikeleza komoya kwesiqhelo kunzima.

Inversion Iluchaphazela njani ungcoliseko

Ukuguquka komhlaba

Sikhankanyile ukuba ngexesha lenkqubo yokuguqula ubushushu umaleko lokuzinza komoya kuveliswa kumphezulu womhlaba. Olu luhlu lwenziwe ngumoya opholileyo oxineneyo kwaye uhlala kumaleko asezantsi. Oku kwenza ukuba kungabikho ukuxubeka kwamanqanaba amabini omoya anoxinano olwahlukileyo xa enobushushu obahlukeneyo. Ke ngoko, kulula kakhulu ukugqiba kwelokuba enye yezona zinto ziphambili zinokubangelwa kukungena kwe-thermal yile nto ungcoliseko lubambekile kumphezulu womhlaba ngaphandle kokuphazeka lusasaze emoyeni.

Ngokwesiqhelo, umoya uthanda ukunyuka kwaye usivumele ukuba sisasaze ungcoliseko lomoya ovela kwiindawo ezisezantsi. Nangona kunjalo, kwi-inversion ye-thermal, ubushushu obuphezulu obuphezulu busebenza njengokugubungela umoya obandayo odibene nomphezulu womhlaba. Kulapho kugcinwa khona isixa esikhulu sezingcolisi. Esinye seziphumo kwangoko kukutshaya. Lo maleko ungcoliseko unokubonwa ukusuka kwiikhilomitha ezininzi kwaye uhlala ukhokelela ekwehleni kwinqanaba lomgangatho womoya.

Iziphumo kwimpilo yabantu yale nto ziguqulelwa kukonyuka kokubonisana kwezonyango ngenxa yeengxaki zokuphefumla kunye neentliziyo. Kufuneka kuthathelwe ingqalelo ukuba umoya ophefumlayo ongcolileyo uhlasela ngakumbi amaqela anobungozi afana nabantu abagulayo, abantu abadala okanye abantwana. Kwaye amanqanaba e-nitrogen dioxide kunye nesulfure dioxide agcinwa ngamaxesha e-inversion ye-thermal. Ngaphaya koko, i-10 kunye ne-2.5 micron ubukhulu bamasuntswana agxilwe kwaye angena kwi-alveoli yemiphunga.

Ndiyathemba ukuba olu lwazi ungafunda ngakumbi malunga nokwenzeka kokungena kwe-thermal.


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