Isitatimende Sobumfihlo: Ubumfihlo bakho bubaluleke kakhulu kithina. Inkampani yethu ithembisa ukungadaluli imininingwane yakho kunoma yikuphi ukuveza izimvume zakho ezicacile.
1. UCumolus
Amafu akha lapho umoya uphothula khona amazolo, izinga lokushisa lapho umoya ungasakwazi ukubamba wonke umphunga wawo wamanzi. Kuleli lokushisa, ama-vapor wamanzi ama-condenses ukwakha amaconsi amanzi awuketshezi, esiwabona njengefu.
Ukuze le nqubo yenzeka, sidinga ukuthi umoya uphoqeleke ukuthi akhuphuke emkhathini, noma emoyeni omanzi ongahlangana naye endaweni ebandayo.
Ngosuku olunelanga, imisebe yelanga ishisa umhlaba, okuvuthayo umoya ngaphezu kwawo. Lo moya ofudumele ukhuphuka nge-convection futhi amafomu uCumolus. Lezi "isimo sezulu esilungile" amafu "abukeka njengoboya bekotoni.
Uma ubheka isibhakabhaka esigcwele i-CUMULUS, ungabona ukuthi banezisekelo ezifuywayo, zonke zilala ezingeni elifanayo. Kulokhu kuphakama, umoya ovela ezingeni lomhlabathi usupholile kwiphuzu lamazolo. Amafu we-Cumulus awavamisile imvula - ususe yisimo sezulu esihle.
2. Cumonimbus
Ngenkathi i-cumulus encane ingana, uma ubona i-cumulus iba nkulu futhi yandiswa iphakeme emkhathini, kuwuphawu lokuthi imvula enkulu isendleleni. Lokhu kujwayelekile ehlobo, ngokusuka ekuseni uCumulus athuthukela ku-Cumonimbus ejulile (ukuduma kwezulu) ntambama.
Eduze komhlaba, iCumonikhumbus ichazwa kahle, kepha iyakhuphuka baqala ukubukeka ehlakaniphile emaphethelweni. Lokhu kuguqulwa kukhombisa ukuthi ifu alisasenziwa ngamaconsi amanzi, kepha amakristalu eqhwa. Lapho kuvunguza umoya wamaconsi wamanzi angaphandle kwefu, asheshe aphuma endaweni enyaka, enikeza amafu wamanzi umphetho obukhali kakhulu.
Ngakolunye uhlangothi, amakristalu eqhwa athwalwa ngaphandle kwefu awashintshi ngokushesha, anikeze ukubukeka okuphikisanayo.
I-Cumonimbus imvamisa ifakwe phezulu. Ngaphakathi kweCumonikhumbus, umoya ofudumele ukhuphuka nge-convection. Ngokwenza kanjalo, kancane kancane kuyaphola kuze kube yilapho kulincane okufanayo njengomoya ozungezile.
Kuleli zinga, umoya awesekho ukudlala ngakho ngeke kufinyeleleke ngokwengeziwe. Esikhundleni salokho kusakazeka, kwakha ukwakheka kwesimo se-anvil.
3. I-Cirrus
I-Cirrus yakha phezulu kakhulu emkhathini. Bahlakaniphile, bahlanganiswa ngokuphelele ngamakristalu eqhwa awela emkhathini. Uma i-cirrus ithwalwa ngokuvundlile ngemimoya ehamba ngejubane elihlukile, ithatha isimo esinezimpawu zobunye.
Kuphela ezindaweni eziphakeme kakhulu noma ama-latitus akhiqiza i-cirrus kuthela imvula ezingeni lomhlabathi.
Kepha uma uqaphela ukuthi i-cirrus iqala ukumboza okwengeziwe kwesibhakabhaka, futhi iphansi futhi ibe mkhulu, lokhu kuyinkomba enhle yokuthi ingaphambili elifudumele lisondela. Ngaphambili ngokufudumele, umoya ofudumele nowubandayo uhlangane. Umoya ofudumele olula uphoqeleka ukuthi ukhuphuke ngaphezu kwesisindo somoya obandayo, okuholela ekwakhekeni kwamafu.
Amafu aphansi akhombisa ukuthi ingaphambili lisondela, linikeza isikhathi semvula emahoreni ayi-12 alandelayo.
4. Stratus
I-Stratus iyiphepha le-Cloud eliphansi eliqhubekayo elimboza isibhakabhaka. Ama-Stratus alungisa umoya okhuphukayo ngobumnene, noma ngomoya omnene aletha umoya omanzi ngaphezu komhlaba obandayo noma indawo yolwandle. I-Stratus Cloud inciphile, ngakho-ke ngenkathi izimo zingazizwa zimnyama, kungenakulindeleka, futhi okungenani kuzoba yi-drizzle ekhanyayo.
I-Stratus iyafana nenkungu, ngakho-ke uma ngabe wake wahamba ezintabeni ngoSuku lwenkungu, ubukade uhamba emafwini.
5. I-Leticular
Izinhlobo zethu ezimbili zokugcina zefu ngeke zikusize ubikezele isimo sezulu esizayo, kepha zinikeza amazwibela ezikhulumweni eziyinkimbinkimbi ngokwejwayelekile zomkhathi.
Ifomu elibushelelezi, le-lens enomumo le-lensAred Clouds njengoba umoya ushaywa phezulu nangaphezulu kwebanga lentaba.
Lapho nje esedlule entabeni, umoya ungena emuva ezingeni lawo langaphambilini. Njengoba icwila, ifudumale futhi ifu liyahwamuka. Kepha kungaserhshoot, lapho i-Air Mass Bobs isipele ngenye ifu le-lenticular lakha.
Lokhu kungaholela enhlanganisweni yamafu, ukunwebeka ngendlela engaphezu kwebanga lentaba. Ukuxhumana komoya nezintaba nezinye izici ezingaphezulu kungenye yemininingwane eminingi okufanele imelwe kuma-simulators amakhompyutha ukuthola izibikezelo zesimo sezulu.
6. UKelvin-Helmholtz
Ifu leKelvin-Helmholtz lifana negagasi lokuphuka kolwandle.
Lapho ama-wor mastes ezindaweni eziphakeme ezihlukile zihamba ngokuvundlile ngejubane elihlukile, isimo siba yinto engazinzi. Umngcele phakathi kwezixuku zomoya uqala ukuklebhula, ekugcineni kwakheka amaza amakhulu.
Amafu we-Kelvin-Helphoholtz avelakancane, ngoba singabona kuphela le nqubo eyenzeka emkhathini uma isisindo somoya esiphansi siqukethe ifu.
Ifu lingabe selilandele amaza aphula umthetho, embula ubuhlakani bezinyathelo ezingabonakali ngenye indlela amakhanda ethu.
Ngaphezu kwalokho, uma unentshisekelo ephepheni lesikebhe lesikebhe e- EVA noma i - EVA SUP Pad & Eva Traction Pad , sicela ukhululeke ukuxhumana nathi.
Iqembu le-Hellors
2018.07. Okuthenyalwayo
I-imeyili: admin@melorsfoam.com
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Isitatimende Sobumfihlo: Ubumfihlo bakho bubaluleke kakhulu kithina. Inkampani yethu ithembisa ukungadaluli imininingwane yakho kunoma yikuphi ukuveza izimvume zakho ezicacile.
Gcwalisa eminye imininingwane ukuze ukwazi ukuxhumana nawe ngokushesha
Isitatimende Sobumfihlo: Ubumfihlo bakho bubaluleke kakhulu kithina. Inkampani yethu ithembisa ukungadaluli imininingwane yakho kunoma yikuphi ukuveza izimvume zakho ezicacile.