Amafu eentente

Uninzi lwabantu luye lwaphazama ngelifu ngenxa yeUFO. Wonke umntu ozibonileyo ezi iintlobo zamafu Bacinge ukuba indalo iyahleka ngobukho bobomi ngaphandle kweplanethi yethu. Nangona kunjalo, oku akunjalo. Ezi zinto zisesibhakabhakeni zibangelwe bubukho be amafu elensi. Luhlobo lwamafu olunemilo yesososo okanye iilensi eziguqukayo ezihlala zivela kwiindawo zeentaba.

Kweli nqaku siza kukuxelela ukuba yintoni la mafu obumnyama kunye nokuba akhiwe njani. Ukuba unomdla kwaye ufuna ukutyhila ezi mfihlakalo, nantsi iposti yakho 🙂

Yintoni amafu edibeneyo?

Njengoko besesitshilo, Luhlobo lwamafu anesoso okanye imilo yeUFO kwaye oko kubonakala kwiindawo zeentaba. Sele inyani yokuba ibonakala kuphela kwiindawo ezisezintabeni ingasinika imikhondo yeemeko zoqeqesho ekufuneka zibonakale ngoluhlobo. Ngamafu enza kwi-troposphere, oko kukuthi, kweyona iphantsi Ubume beatmosfera.

Iimpawu zeli lifu zezo ze-altocumulus. Ngokungafaniyo neAltocumulus yesiqhelo, yi uhlobo lokuma kunye nelombala (ebizwa ngokuba zizazinzulu i-altocumulus lenticularis). Inokuthatha iifom ze-lenticular cirrocumulus okanye i-lenticular stratocumulus. Olu lwakhiwo luxhomekeke kwimeko-bume nokusingqongileyo njengolawulo lomoya Uxinzelelo lomoya, la ukufuma okanye amaqondo obushushu kukho ngelo xesha.

Olona phawu lubalaseleyo kula mafu kukuba anika indawo entle kwaye adidekile amaxesha amaninzi kunye nokubonwa kweUFO.

Inkqubo yoqeqesho

Ukuze sikwazi ukucacisa konke okungaziwayo malunga nokunqaba okukhethekileyo kwala mafu, siza kuchaza imvelaphi yokwakheka kwawo. Njengoko besesitshilo ngaphambili, ifuna iimeko ezahlukeneyo zemozulu nezendalo ukuba zenzeke. Into yokuqala yile ukuhamba ngamandla okuza ngamandla kunye nokudibana nokubuyela umva emoyeni. Ezi meko kunokwenzeka ukuba zenzeke kwiindawo ezisezintabeni, apho umoya, wakube ungqubene nokwakheka kwamatye, kunyanzeleka ukuba unyuke.

Iintaba ziyimiqobo ethintela ukuhamba komoya emoyeni kwaye siyabulela kuzo ngeziganeko ezinje nge Isiphumo seFoëhn. Xa uhamba emoyeni kwicala elingaphezulu kunye ne-inversion ye-thermal, iziphithiphithi zenziwe zahlelwa njengophazamiseko. Umoya ekugqibeleni ufikelela encotsheni ngeqondo lobushushu elingaphantsi kakhulu kunokuba lalinjalo ngaphezulu okanye kufuphi nomphezulu.

Njengoko iqhubeka nokuhambela phezulu nangaphezulu emoyeni, iqondo lobushushu liyaqhubeka ukwehla ngokuqhubekayo nangakumbi ngenxa yokuguquka kwe-thermal. Ukuba umoya ophakamise intaba ufumile, oko kukuthi, ulayishwe ngamathontsi amanzi, ukufuma kuyancipha njengoko iqondo lobushushu lincipha kwindawo ephezulu, kuba ifikelela kwindawo yombethe. Njengoko ukunyuka komoya kuhlangana, Sifumana ukuyilwa kobunzima belifu obukhulela encotsheni yentaba Kwaye ukuba, xa uhlangabezana nokuguqulweyo kobushushu, kuya kubakho amafu enzala.

Iimeko eziyimfuneko kuqeqesho lwabo

Ngokuqinisekileyo ucinga ukuba kuhlala kukho inversion ye-thermal kwaye, njengoko sikhuphuka phezulu, kuyabanda. Ke ngoko, amafu eententiki kufuneka ahlala esenza. Kuyinyani ukuba, amacala aphezulu e-atmosfera ayabanda kunalawo angezantsi. Ezi ezisezantsi zondliwa bubushushu obukhutshwa emhlabeni xa imitha yelanga phezu komhlaba.

Kodwa oku akufuneki kube njalo. Kukho amaxesha apho umhlaba ubanda ngakumbi ngenxa yokwehla kobungakanani belanga eliwela phezu komhlaba okanye kumbala womphezulu othethiweyo (khumbula ukuba imibala emnyama imisa ubushushu kwaye abamhlophe bayakubonakalisa. ibizwa ngokuba albedo). Kwimeko apho umhlaba ubanda, umhlaba ngokwawo unako ukufunxa bonke ubushushu obujikeleze umoya, ukwenza iileya zomoya ezisezantsi zikubushushu obuphezulu kunobo bangaphezulu. Kule meko sifumana inversion ye-thermal.

Imimandla ene-inversion ye-thermal ihlala izinzile ngokuhamba kwexesha, ukuze umoya, xa uzama ukunyuka intaba, uyakususa umoya oshushu ongasentla oya kubuyela umva udale iindawo ezime ukuba zibamba ukufuma okuxineneyo kwaye zinike ilifu ubume obudibeneyo. Esi sizathu sokuba la mafu abukeke ngathi zi-UFOs kwaye aziphosakele izihlandlo ezininzi.

Kutheni uphepha ukubhabha kufutshane namafu ale lentiki?

Bekusoloko kusithiwa abaqhubi beenqwelo moya bayazama ngazo zonke iindlela ukunqanda ukubhabha kwiindawo ezikufutshane namafu eentlanzi. Makhe sibone ukuba kutheni kusenzeka oku. Njengamafu e lenticular enza xa kuvuthuza umoya yomelele kwaye iza ilayishwe ngomswakama, ukunyuka intaba kunye nokubanda njengoko unyuka kuyakhawuleza. Ngokuba nomaleko ophezulu wokumisa inversion ye-thermal, yenza ukuba umoya ujikeleze ixesha elide kwindawo ephezulu.

Ukwakheka kwala mafu kungafunyanwa xa ukungqubana kwemikhosi emibini yomoya kungqubana kwaye kubangela elona candelo lishushu ukuba liphume kwaye umoya obandayo uthatha indima yesithintelo somatshini. Isizathu sokuba abaqhubi beenqwelomoya bangafuni ukubhabha kwezi ndawo kungenxa yokuba iimpawu zomoya ezinxulumene nala mafu zinamandla kakhulu kwaye zijonge phezulu kwaye zinokubangela uzinzo olukhulu kwindiza.

Kwelinye icala, olu hlobo lomoya lufunwa kakhulu kwezo nqwelo moya zingasebenzisi injini kuba imisinga yomoya isetyenziselwa ukucwangcisa ngcono nokugcina inqwelomoya ixesha elide. Umnqweno kukuba irekhodi lehlabathi lokubaleka kuye kwafezekiswa ukubulela kwimisinga yomoya enika amafu e-lenticular.

Ndiyathemba ukuba olu lwazi luyakunceda ufunde ngakumbi malunga nolu hlobo lwelifu kunye nokwakheka kwalo.