Kukho iziganeko zemozulu yasebusika ezingaqhelekanga kunezinye. Kule meko siza kuthetha nge-rime kunye neqabaka. Le yimifanekiso yekristale ebonakala ngokukodwa kwiintsasa zasebusika ezibandayo. Kukho ezinkulu umahluko phakathi kweqanda neqabaka edla ngokudida abantu.
Ngesi sizathu, siza kunikezela eli nqaku ekuqaqambiseni umahluko phakathi kwerime kunye neqabaka.
Umahluko phakathi kwerime kunye neqabaka
I-Chiselladas kunye neqabaka zidla ngokuvela ngexesha le-anticyclone, ngeentsuku ezizolileyo nezingenamoya. Ezi meko zenza ukuba ubushushu buphele ngokukhawuleza emhlabeni. Esi siganeko senzeka ebusuku, yaye sidla ngokusifumana ngentsasa elandelayo, ezimotweni nakwizityalo, ezinomaleko womkhenkce osikhumbuza ngekhephu.
Xa ilanga litshona yaye kuba mnyama, ubushushu buyahla yaye umhlaba uqalisa ukuphola. Umoya opholileyo uxinene kwaye ushona kumaleko asezantsi kwaye uqala ukupholisa ngaphezulu. Zombini ukufuma kunye nobushushu zidlala indima ebalulekileyo. Ukufuma komoya okunxulumeneyo kufuneka kungaphezulu kwe-60% kwaye ubushushu bomphezulu kufuneka bube ngaphantsi okanye bulingane no-0ºC. Ngale ndlela, umphunga wamanzi uguqulwa ngokuthe ngqo kwiikristale zomkhenkce, esizibiza ngokuba yiqabaka.
Nangona le nkqubo iyafana, xa kuvuthuza umoya onamandla, inkungu idla ngokuvela. Umsi omhlophe, ovela kwiintsuku ze-anticyclone, uyabanda kwaye uzolile. Le nto yenzeka xa "umbethe" ungaphantsi kwendawo yokukhenkceza, apho kuvela inkungu apho ubushushu bubanda ngakumbi. Amathontsi amancinane amanzi, axhonywe kwinkungu, ayantywiliselwa, kwaye xa zidibana nomphezulu ziyabanjwa, zenze ezo kristale zincinci zimenyezelayo. Apha, umoya uvelele, kwaye xa uvuthuza, uphazamisa ukwakheka ngokuthanda kwaye unokudala uhlobo "lweflegi yomkhenkce", "iintsiba" kunye "nemimoya" enomdla yokufota.
Iphi i-rime eyenziwe
Yinto yemeteorological eyenzeka xa inkungu ingumkhenkce. Xa kukho inkungu ebandayo kwaye eqhubekayo ebangelwa kukufuma okuphezulu, i-rime idla ngokubakho. Abafoti abaninzi basebenzisa olu hlobo lokwenzeka ukwenza iifoto ezinomdla. Ngokuqhelekileyo kwenzeka kwiindawo apho kukho inkungu eshinyeneyo kwaye amaqondo obushushu ehla ngaphantsi kwe-0 degrees. Kwezi xabiso lobushushu indawo yombethe ingaphantsi kweqondo lomkhenkce.
Kungalo mzuzu apho amanqanaba amanzi adada emoyeni aqala ukuba ngumkhenkce kumphezulu wendawo. Siyakhumbula ukuba amanzi adinga umphezulu ukuze akwazi ukuba ngumkhenkce. Ke ngoko, iincinci zesanti ezinobungakanani bemicron ziyafuneka ukuze zisebenze njenge-hygroscopic condensation nucleus. Xa amathontsi amanzi eqalisa ukuba ngumkhenkce phezu komhlaba enza iintsiba okanye iinaliti zomkhenkce othambileyo. Oku kumila kufana nekhephu kodwa akufani ncam.
Indawo ekwenzeke kuyo umsinga ifana kakhulu nenye indawo enekhephu. Nangona kunjalo, ukuba sisondela kumphezulu wamatye, amasebe emithi, amagqabi, njl. Siyakwazi ukubona ezi naliti zincinci kunye nohlobo lwemibhobho yokwakheka komkhenkce ebangelwa yinkungu engumkhenkce. Izixeko kunye needolophu zaseSpain ezinomlambo okufutshane zezona zinokwenzeka ukuba le nto yenzeke. Sesinye sezizathu zokuba i-cencellada yenzeke rhoqo ngexesha lasebusika eValladolid okanye eBurgos.
Kwaye kukuba imilambo isoloko ingumthombo wokufuma kwimekobume. Ukongeza, sibulela ukuhamba kwamanzi rhoqo intyatyambo exinene ngokufanelekileyo iyakhula inceda ukugcina ukufuma kokusingqongileyo. Xa kukho ukungafani kwamaqondo obushushu emini nasebusuku, olu hlobo lwenkungu exineneyo ludla ngokuvela kwaye, ngenxa yezityalo, luhlala lugcinwa. Ukuba ubushushu be-ambient yehla ngaphantsi kwe-0 degrees, ukuvuthuza kwesiphango kunokwenzeka ukuba kwenzeke.
iqabaka phi
Ngobusuku obunesibhakabhaka esicacileyo, imimoya enomoya okanye ezolileyo, kunye nomoya ofumileyo ngandlel’ ithile, uMhlaba uyaphola ngenxa yemitha yemitha, njengoko usenza nomoya ohlala emhlabeni. Umphunga wamanzi ofumaneka kumoya ococekileyo kufutshane nomphezulu uyaphola kwaye uvelise amathontsi ziyajiyana zibe ngamathontsi avela emagqabini, engceni, kwiindiza, njl. Ngoko sinombethe.
Iqondo lobushushu apho umphunga (irhasi) ujika ube lulwelo (amathontsi amanzi) ubizwa ngokuba "yiqondo lombethe." Amathontsi ombethe alingana ngobukhulu kwaye angaphantsi kwemilimitha ububanzi.
Kubusuku obuzolileyo nobunoxolo, umoya unokubanda ngokuphawulekayo, ufikelele kumaqondo obushushu angaphantsi kweqanda; ke umphunga wamanzi uya ngqo kwiikristale zomkhenkce kwaye sineqabaka. Ingca, iindiza, iifoloji zeefolo, iinduli zezindlu, njalo njalo, kwabonakala kumhlophe kwakusasa, kwakubonakala ngathi kunekhephu, kodwa akukho mntu wabhidayo, kuba isibhakabhaka sasicwebile ubusuku bonke. Ngamanye amaxesha amafama abiza ezi qabaka "iiqabaka."
Kukho inkqubo yesithathu apho kwenziwa amathontsi ombethe (iqondo lobushushu elingaphezu kwe-0°) aze la mathontsi abe ngumkhenkce (ubushushu obungaphantsi kwe-0°); Kubizwa ngokuba "umbethe omhlophe". Apha, umphunga (igesi) uba lulwelo (amathontsi) uze umkhenkce (umkhenkce). Yinkqubo efana naleyo ibangela ukuvela kwesichotho, kuphela ukuba esi sichotho senzeka kumafu anamandla akhula ngokuthe nkqo. Xa kukho umbethe, umoya, nangona ubanda, ungaphezu kwe-0 ° (umzekelo, 3 ° ukuya ku-5 ° C); ukuze kubekho iqabaka, umoya kufuneka ube ngaphantsi kwe-0 ° (-2° ukuya ku-4° C).
Umbethe udla ngokubonwa ngexesha leequinox kunye nekwindla, ngelixa iqabaka iyindawo eqhelekileyo yasentwasahlobo nasebusika. Umbethe neqabaka ngokuqhelekileyo zenzeka kwiindawo eziphantsi kunye namathafa, apho ukufuma kudla ngokuba phezulu.
Entwasahlobo, emva kweqabaka enzima okanye umbethe, ekuzeni kokusa, kuba umoya ucace kakhulu, i-condensation ikhawuleza ibe ngumphunga; ukweba ubushushu obuphuma buphuma buphuma kumathupha, amagqabi kunye neentyatyambo, nto leyo ebangela ukwehla okumangalisayo kobushushu. Oku kuchaphazela la malungu esityalo aethe-ethe. Zibizwa ngokuba yi-evaporation frosts kwaye ke ngoko yoyikwa ngamafama akwicala lentwasahlobo.
Ndiyathemba ukuba ngolu lwazi unokufunda ngakumbi malunga nomahluko phakathi kwe-rime kunye neqabaka.