Ukuduma

Ngokuqinisekileyo ukhe weva ngeendaba kwi isilwanyana. Yimeko yemozulu eyenzeka xa inkungu iqina. Ukuze le nto ibonakale kufuneka kubekho iimpawu ezithile kunye nezinto ezithile. Ngokwesiqhelo ixesha elinamaqondo obushushu asezantsi kunye nenkungu eqhubekayo iyafuneka. Ngaphandle kwento yokuba sisimo sezulu esenzeka kwiindawo ezininzi, asaziwa kakuhle ebantwini.

Ke ngoko, siza kulinikela eli nqaku ukuba likuxelele zonke iimpawu zerim nokuba kutheni isenzeka.

Yintoni irim

Yimeko yemozulu eyenzeka xa inkungu iqina. Xa kukho inkungu ebandayo nengapheliyo ebangelwa kukufuma okuphezulu, isisiqhelo sidla ngokwenzeka. Abafoti abaninzi basebenzisa olu hlobo lwesenzeko ukuthatha iifoto ezinomdla. Ihlala ivela kwiindawo apho kukho inkungu eshinyeneyo kwaye amaqondo obushushu ehla abe ngaphantsi kwe-0 degrees. Kula maxabiso obushushu indawo yombethe ingaphantsi kwengqele.

Ngeli xesha kuxa amanqanaba amanzi ajikelezayo emoyeni eqala ukuba ngumkhenkce kumphezulu wale ndawo. Siyakhumbula ukuba amanzi afuna umphezulu womkhenkce. Ke ngoko, amasuntswana esanti enobukhulu be-micron ayafuneka ukuze asebenze njengombindi we-condensation core. Xa amathontsi amanzi eqala ukuba ngumkhenkce kumphezulu enza iintsiba okanye iinaliti zomkhenkce othambileyo. Ezi zakhiwo ziyafana nekhephu kodwa azifani.

Indawo apho kwenzeke khona ingxolo iyafana kakhulu kwenye indawo apho kukho ikhephu. Nangona kunjalo, ukuba sisondela kwindawo yamatye, amasebe emithi, amagqabi, njl. Siyabona ukuba ezi naliti zincinci kunye nokwakheka okufana neentsiba zomkhenkce kubangelwe yinkungu enomkhenkce. Iidolophu needolophu zaseSpain ezinomlambo okufuphi zezona zigqwesileyo ukuba kwenzeke oku. Sesinye sezizathu zokuba kutheni Umthi wenzeka rhoqo ngexesha lobusika eValladolid okanye eBurgos.

Kwaye imilambo ingumthombo wokufuma rhoqo. Ukongeza, ngenxa yokuhamba rhoqo kwamanzi, kukhula izityalo ezishinyeneyo ezinceda ukugcina ukufuma kwendalo. Xa kukho umahluko kumaqondo obushushu emini nasebusuku, olu hlobo lwenkungu eshinyeneyo luhlala lusenzeka kwaye ngenxa yeentyatyambo zihlala zigcinwa. Ukuba iqondo lobushushu elihleliyo liwela ngaphantsi kweedigri eziyi-0, ixesha lokulima kunokwenzeka ukuba lenzekeke.

Iimpawu eziphambili

Siyabona ukuba xa ingxolo yenzekile inokwenzeka ngeendlela ezimbalwa. Ukuba i-hydrometer yenzeka phezulu kwaye iqondo lobushushu lehla laya kutsho kwi-2 degrees ngezantsi kwe-zero kubukho bomoya, Siyabona ukuba i-rime iba nzima kwaye iikristali zomkhenkce ziyila ngendlela eyahlukileyo. Ezi kristali zomkhenkce azinayo inkqubo yokwakheka efanayo nekhephu eyenzeka xa kukho ikhephu, kodwa endaweni yoko yenza uthotho lweenaliti ezikhula zijonge kwicala lomoya. Ixesha elide ulusu luhlala kunye neemeko ezithandayo, kokukhona umkhenkce uya kuba nakho ukuqokelela.

Into esingafanele siyidibanise nerime yingqele. Yinto eqhelekileyo ukudida neziganeko ezibini ezahlukileyo ngokupheleleyo. Ukuze ingxolo yenzeke, kubalulekile ukuba kubekho inkungu eshinyeneyo kwimeko-bume. Iqabaka livela xa ukufuma kukungcola okusingqongileyo. Kule meko, akukho mfuneko yokuba kubekho inkungu, nangona kuyinyani ukuba ukufuma okuninzi kuyadingeka kwindalo esingqongileyo.

Rime yenzeka xa sele kukho imiphezulu yenkungu ekwaziyo ukugcina ukufuma okusingqongileyo. Ke ngoko, ixhaphake kakhulu kwiindawo apho kukho umlambo kunye neentyatyambo ezinxulumene nayo. Ngokuqinisekileyo, ukuba lixesha lokuqala ubona umphetho, unokumangaliswa kwaye uthi unokufana okuthile neendawo ezinekhephu. Kuyacaca ukuba xa i-rime ibonakala kukuba ikhephu eliweleyo linobunzulu obukhulu. Eli gama laziwa ngokubanzi ngaphakathi kweIberian Peninsula.

Kutheni udini lwenzeka

Ukuze le meko yezulu yenzeke, isibhakabhaka esicacileyo siyafuneka ebusika, amaqondo obushushu asezantsi kunye nendawo apho kugcina ukufuma okwaneleyo. Kuqhelekile kwiindawo zeentaba apho kukho umlambo kunye neentyatyambo ezinxulumene noko. Ibizwa ikakhulu njenge idiphozithi yomkhenkce eyenziwe kukuqhaqha kwamathontsi enkungu okanye amafu asezantsi. Kunokuthiwa inkungu ayikho enye into ngaphandle kwamafu asezantsi kwinqanaba lomgangatho.

Ukuze le nto yenzeke kwiqondo lobushushu elingaphantsi kwengqele iyafuneka. Yile ndlela inkungu yakusasa eveliswa ngayo rhoqo kwiindawo ezisezintlanjeni, ngakumbi. Iziphumo eziphambili zale nto ukuba zenzeke kukupholisa ebusuku. Ngenxa yoku, kufuneka kubekho umahluko omkhulu phakathi kwamaqondo obushushu emini nasebusuku.

Iimeko eziyimfuneko ukuze ingxolo yenzeke sisibhakabhaka esicacileyo, ukungabikho komoya, umahluko omkhulu phakathi kobushushu bemini nobusuku kwaye amaqondo obushushu kusasa aphantsi okanye aphezulu kancinci kune-0 degrees. Ukuba zonke ezi meko zokusingqongileyo ziyafezekiswaMhlawumbi sinenkungu eqhelekileyo yentsasa eya kuguquka. Kuqheleke kakhulu kwimimandla yeentlambo zomlambo ezinomswakama ophezulu kunye namaqondo obushushu asezantsi.

Amaqondo obushushu asebusuku kufuneka abe sezantsi kakhulu kwaye ukufuma okuhambelana noko kuphezulu kakhulu. Ubumanzi obuveliswe lilifu elikhuselweyo kufuneka bubekwe kumgangatho womhlaba, oya kuthi ubangele ukuba ujike ube ngumkhenkce xa ugubungela umphezulu. Umoya obandayo uthanda ukwehla usuka emathambekeni kwaye ube negalelo kwinani elikhulu lokufuma okuququzelela ukuyilwa kwenkungu. Oku kufuma okuphezulu kunceda ekuboneleleni ngamanzi ayimfuneko ekwakhiweni kwenkungu ethi, kamva, ibambe ngaphezulu.

Ndiyathemba ukuba olu lwazi ungafunda ngakumbi malunga nerim.