Amafu entente

Abantu abaningi bake baphutha ifu nge-UFO. Wonke umuntu okubonile lokhu izinhlobo zamafu Bacabange ukuthi imvelo ihleka ubukhona bokuphila ngaphandle kweplanethi yethu. Noma kunjalo, akunjalo. Lezi zakhiwo esibhakabhakeni kungenxa yokuba khona kwe- amafu lenticular. Luhlobo lwefu olunokuma kwesosisi noma ilensi eguqukayo evame ukuvela ezindaweni ezinezintaba.

Kulesi sihloko sizokutshela ukuthi ayini lawa mafu angumbumbulu nokuthi akhiwa kanjani. Uma unelukuluku futhi ufuna ukwembula lezi zimfihlakalo, lokhu okuthunyelwe kwakho 🙂

Ayini amafu edonsa?

Njengoba sishilo, ziwuhlobo lwamafu anesoso noma umumo weUFO futhi lokho kuvela ezindaweni ezisezintabeni. Kakade iqiniso lokuthi livela kuphela ezintabeni lingasinikeza izinkomba zezimo zokuqeqeshwa elidinga ukuvela kanjena. Bangamafu akha i-troposphere, okungukuthi, endaweni ephansi kakhulu ye- izingqimba zomkhathi.

Izici zaleli fu yilezo ze-altocumulus. Ngokungafani ne-Altocumulus ejwayelekile, iyi- uhlobo olumile nolwe-lenticular (ebizwa ososayensi i-altocumulus lenticularis). Kungathatha futhi izinhlobo ze-lenticular cirrocumulus noma i-lenticular stratocumulus emile. Lezi zakhiwo zincike ezimweni zemvelo nezomkhathi ezifana nombuso womoya, i- ingcindezi yasemkhathini, lo umswakama noma i amazinga okushisa kukhona ngaleso sikhathi.

Isici esivelele kakhulu kulawa mafu ukuthi aletha indawo ebabazekayo futhi adideke kaningi nokubukwa kweUFO.

Inqubo yokuqeqesha

Ukuze sikwazi ukusula konke okungaziwa mayelana nokutholakala okungajwayelekile kwalawa mafu, sizochaza umsuka wokwakheka kwawo. Njengoba sishilo phambilini, kudinga izimo ezahlukahlukene zomkhathi nezemvelo ukuthi zenzeke. Into yokuqala ukuthi ukugeleza okunamandla okuqhamuka phezulu nokuhlangabezana noshintsho emkhathini. Lezi zimo kungenzeka ukuthi zenzeke ezindaweni ezisezintabeni, lapho umoya, uma usushayisene nokwakheka kwamatshe, uphoqeleka ukuba ukhuphuke.

Izintaba ziyizithiyo zokuhamba komoya emkhathini futhi ngenxa yazo eminye imicimbi efana ne- Umphumela we-Foëhn. Lapho uhamba emoyeni ubheke phezulu futhi uguqukela ezishisayo, izivunguvungu zenziwa ezihlukaniswa njengeziyaluyalu zemishini. Umoya ekugcineni ufinyelela phezulu ngezinga lokushisa eliphansi kakhulu kunalapho wawukhona noma eduze kobuso.

Njengoba uqhubeka nokunyukela phezulu naphezulu emkhathini, izinga lokushisa liyaqhubeka ukwehla ngokuya phambili ngenxa yokuguquka. Uma umoya okhuphuke eduze kwentaba unomswakama, okungukuthi, ulayishwe ngamaconsi amanzi, umswakama uyaqina njengoba izinga lokushisa lincipha phezulu, ngoba lifinyelela endaweni yamazolo. Njengoba umoya okhulayo ujiya, sithola ukwakheka kwesisindo samafu esikhula sifike esiqongweni sentaba nokuthi, lapho kuhlangatshezwana nokushintshwa okushisayo, amafu e-lenticular azokwakhiwa.

Izimo ezidingekayo zokuqeqeshwa kwabo

Impela ucabanga ukuthi kuhlale kunemfudumalo eshisayo nokuthi, njengoba sikhuphuka phezulu, kuyabanda. Ngakho-ke, amafu e-lenticular kufanele akhe njalo. Kuyiqiniso ukuthi, izingqimba ezingenhla zomkhathi zibanda kakhulu kunezingezansi. Lawa aphansi ondliwa ukushisa okukhishwa emhlabathini lapho i- imisebe yelanga ebusweni bomhlaba.

Kepha lokhu akudingeki kube njalo. Kunezikhathi lapho umhlabathi ubanda kakhulu ngenxa yokwehla kwenani lokukhanya kwelanga okuwela ngaphezulu noma ngisho nombala waleyo ndawo eshiwo (khumbula ukuthi imibala emnyama imunca ukushisa futhi abamhlophe bayakubonakalisa. ibizwa ngokuthi albedo). Uma kwenzeka umhlaba ubanda kakhulu, umhlabathi ngokwawo ungamunca konke ukushisa okuvela emoyeni ozungezile, okwenza izingqimba ezingezansi zomoya zisezingeni lokushisa eliphakeme kunalezo ezingenhla. Kukulesi simo lapho sithola ukuguqulwa okushisayo.

Izindawo ezinokushintshwa okushisayo zivame ukuzinza ngokuhamba kwesikhathi, ukuze umoya, lapho uzama ukukhuphuka intaba, uzobe ususa umoya oshisayo ophezulu ozohlehlela phansi udale izindawo ezimile babamba umswakama ojiyile futhi banikeze ifu isimo se-lenticular. Lesi yisizathu esenza ukuthi lawa mafu abukeke njengama-UFO futhi aphuthelwe wona kaningi.

Kungani kufanele ugweme ukundiza eduze kwamafu edwala?

Bekuhlale kushiwo ukuthi abashayeli bezindiza bazama ukugwema ukundiza ezindaweni eziseduze kwamafu adonsa ngazo zonke izindlela. Ake sibone ukuthi kungani lokhu kwenzeka. Njengamafu e-lenticular akha lapho umoya inamandla futhi iza ilayishwe umswakama, ukwenyuka intaba nokuncipha njengoba ukhuphuka kushesha impela. Ngokuba nesendlalelo esiphakeme esimile sokuguquguquka okushisayo, kwenza umoya ujikeleze isikhathi eside endaweni ephezulu.

Ukwakheka kwalawa mafu kungatholakala futhi lapho izidudla zomoya ezimbili eziphikisanayo zishayisana futhi zibangele ukuthi ingxenye eshisa kakhulu inyuke futhi umoya obandayo uthatha indima yesithiyo semishini. Isizathu esenza abashayeli bezindiza bangafuni ukundiza kulezi zindawo kungenxa yokuthi izici zomoya ezihambisana nalawa mafutha zinamandla amakhulu futhi ziqonde phezulu futhi zingadala ukonakala okukhulu endizeni.

Ngakolunye uhlangothi, lolu hlobo lomoya lufunwa kakhulu kulezo zindiza ezingayisebenzisi injini kwazise imisinga yomoya isetshenziselwa ukuhlela kangcono nokugcina indiza isikhathi eside. Ilukuluku ukuthi irekhodi lomhlaba lokundiza kufinyelelwe ngokubonga imisinga yomoya eyenza amafu lenticular.

Ngiyethemba lolu lwazi lusiza ukuthi ufunde kabanzi ngalolu hlobo lwefu nokwakheka kwalo.