Uma ubheka esibhakabhakeni, kuyiqiniso elingenakuphikwa ukubona lezo zakhiwo, lapho uqala nje, zibukeka njengoboya bekotini. lezi zinto, Abalutho futhi abalutho ngaphandle kwamafu, ingxenye engokwemvelo ye-ecosystem enomjikelezo wokuphila obalulekile.
Bona ngokwabo, sengathi bantanta nje emoyeni ngaphandle kwesizathu. Nokho, ukubaluleka kwayo nokubamba iqhaza kwayo ngaphakathi kwe-ecosystem, Kubaluleke kakhulu kunalokho ocabanga ngakho.
Ungase futhi ube nentshisekelo esihlokweni sethu: Angakanani amandla adonsela phansi amaplanethi akha isimiso sethu sonozungezilanga?
Zitholele ingemuva elikhona! Ayini amafu?
Uma uwabuka kuqala, amafu abonakala enziwe ngekotini noma into ecijile edala ukungahlaliseki. Nokho, ukuqonda ukuthi amafu ayini, ukuqaphela ubukhulu bokubaluleka kwawo emvelweni.
Njengezinye izakhi eziyingxenye ye-ecosystem, amafu nawo anencazelo yawo kanye nomsebenzi wawo. Bona, kusukela kokulula njengokuhlinzeka ngomthunzi, yizithunywa eziyinhloko zesimo sezulu ngokujwayelekile.
Ngamafuphi, amafu ayinqwaba yomumo nobukhulu obuhlukene ngokohlobo lwawo. Lokhu kuqongelela kuhamba ngezinqubo ezimbili eziqondile, eyodwa eyaziwa kabanzi futhi ebizwa ngokuthi ukufingqa; kuyilapho, enye, i-sublimation.
Umthombo: Imvelo
Ngesikhathi senqubo ye-condensation, umhwamuko okhuphukela emkhathini ngenxa yomjikelezo wamanzi, isebenzisana namazinga okushisa aphansi we-medium. Ngemva kochungechunge lokusabela, umhwamuko wokuqala uguqulwa ube yizinhlayiya zamanzi aminyene.
Ngakolunye uhlangothi, inqubo ye-sublimation iguqula umhwamuko ube yiqoqo leqhwa elinomthamo omkhulu kunowandulelayo. Ngalowo mqondo, amafu angaba amanzi noma iqhwa noma axubene.
Ngokulandelayo, ukuze uqonde kangcono ukuthi amafu ayini, umbono wawo oyiphutha olula kufanele ushiywe. Abagcini nje ngokuhlanganyela emjikelezweni wamanzi, ziyakwazi nokudlulisa ukushisa. Lezi zinto zesibhakabhaka eziyinqaba ziguquguquka kakhulu kunokubonwa ngamehlo.
Wake wazibuza ukuthi amafu nezinhlobo zawo akhiwa kanjani? Yazi yonke inqubo!
Ngaphakathi kwencazelo eyisisekelo, inqubo yokuthi amafu akheka kanjani ekuqaleni izoncika elangeni nasekushiseni elikunikezayo. Izilwandle, amachibi, imifula nemithombo yamanzi emincane, Ayahwamuka akhuphukele ngqo emkhathini.
Kanye ngaleso sikhathi, ukucindezela komoya kwenezela emazingeni okushisa aphansi, kufinya umhwamuko wamanzi kancane kancane. Ngokuhamba kwesikhathi, izinhlayiya zamanzi ziba ziminyene, zize zakhe lokho okungamafu.
Njengoba ifu ligcwala izinhlayiya zamanzi, lezi ziba yizici ezinzima. Esikhathini esithile, amanzi adilika njengemvula evela efwini, kungaba sesimweni salo esiwuketshezi noma esiqinile (isichotho).
Nokho, lena akuyona ukuphela kwendlela yokuqonda ukuthi amafu akheka kanjani. Zivela ekusebenzelaneni phakathi kwezindawo ezibandayo nezifudumele, ngokulandelana. Lapho umoya obandayo ugudla umfudlana oshisayo, uphushela umfudlana oshisayo phezulu.
Isikhathi okwenzeka ngaso, umfudlana oshisayo uyanda futhi wehlise izinga lokushisa. Ngaphezu kwalokho, yengezwe ethonyeni lezendlalelo ezibandayo eziphakeme emkhathini, ikhiqiza izinhlayiya zamanzi zamanje, ukuze zifinyele. Uhlobo ngalunye lokusebenzisana luhlukile futhi kuye ngokuthi lwenzeka kanjani, lungenza noma lungakheki izinhlobo ezithile zamafu.
ukwakheka kwamafu aphezulu
Njengoba igama lazo libonisa, yilezo ezilele phezulu emkhathini, ezibonakala zihlakazekile futhi zifiphele. Phakathi kwazo kukhona i-cirrus, i-cirrocumulus ne-cirrostratus, ngayinye enezici zayo eziyinhloko.
Mayelana namafu e-cirrus, zingamafu ngesimo sezinwele noma izintambo ezinde, esobala futhi ehlakazekile. I-Cirrocumulus inomumo ohlangene kakhudlwana, ohlukaniswe komunye nomunye, kodwa eqenjini futhi akusabonakali ngale. Okokugcina, i-cirrostratus inemiphetho ebukhali kakhulu futhi ngokuvamile ikhiqiza ama-halos elanga noma enyanga.
Ukwakheka kwamafu amaphakathi
Ngenxa yokuma kwawo, amafu aphakathi nendawo aba aminyene futhi afinyele ngokuhlobene nangaphambili. I-Altocumulus ivela kuqala, amafu ahlakazekile amise okwekotini anemiphetho engajwayelekile kanye nesakhiwo.
Okulandelayo, i-altostratus ivela, ukuhlanganiswa kwamafu aminyene ngamafomu afanayo ashiwo ngenhla. Ziyinkomba yamafu amancane futhi, ngokuvamile, amboza ilanga kancane.
ukwakheka kwamafu aphansi
Iwuhlobo lwamafu oluhlotshaniswa kakhulu neziphepho nokushintsha kwesimo sezulu, ne-nimbostratus njengefulegi. Zakha ungqimba lombala ompunga, olandelwayo, ngaphandle kokucaca kanye nokubonakala kwemibimbi noma amamaki alula.
Ngakolunye uhlangothi, iphinde ichaze i i-stratocumulus, afana namafu angenhla ngokubukeka nombala. Umehluko nje wukuthi ziqhelelana kancane. Ezinye zazo, ngenxa yokuphakama kwazo okuphansi, zibangela uhlaka, owaziwa ngokuthi yinkungu.
Ngaphakathi kwalolu hlobo lwamafu, lezo ezikhula mpo, njenge-cumulus ne-cumulonimbus, nazo zifakiwe. Amafu e-Cumulus amafu amakhulu anesiqongo esikhula sibheke phezulu, sisekelwe yiplathifomu evundlile. Ngakolunye uhlangothi, amafu e-cumulonimbus, zibe nokukhula okuguquguqukayo, okubanzi nokuphawulekayo, elibonakala ngethiphu elimise okwekhowe.
Kafushane nje, enziwa ngani ngempela amafu? Sula ukungabaza!
Ukwazi ukuthi zakha kanjani, manje sekuyisikhathi sokuphendula ukuthi amafu enziwe ngani. Njengoba kushiwo ngenhla, zakhiwe izinhlayiya super condensed amanzi ezingeni lokushisa eliphansi.
Umhwamuko wamanzi, kuye ngezinga eliphezulu lokuphakama owufinyelelayo kanye namazinga okushisa aphansi, ungaba uketshezi noma uqine. Ngale ndlela, imvula yakudala noma lezo eziqukethe isichotho ziyakhuphuka.
Umthombo: SuperCurious
Nokho, ukuze uqonde ukuthi amafu enziwa ngani, kubalulekile futhi ukwazi “abaxhasi” bakho. Ngaphandle kwezinga lokushisa kanye nesistimu yokucindezela okuphansi, amafu enziwe ngamanzi ashisayo noma ama-curls abandayo.
Uhlobo ngalunye lwamanje, olubuye lubizwe ngokuthi ama-hot noma abandayo, luhlukaniswa ngendlela efanele ukusuka kwelinye. Futhi, njengoba kushiwo ngenhla, ngokusebenzisana abakwenzayo komunye nomunye kanye ne-ecosystem, bakha amafu nezinhlobo zabo ezithile.