Iindidi zenkungu

ukumila kwenkungu

Inkungu luhlobo lwesenzeko semeteorological esivela kwiindawo ezinobumanzi obuphezulu ngokufanelekileyo. Ekuphela komahluko phakathi kwamafu esiwabonayo esibhakabhakeni kunye nenkungu kukuba kwenzeka kumgangatho ophantsi. Kukho ezahlukeneyo iintlobo zenkungu ngokokwakheka kunye neempawu zabo.

Kweli nqaku siza kukuxelela malunga neentlobo ezahlukeneyo zenkungu ekhoyo, zeziphi iimpawu kunye nokwakheka kwazo.

ubukho benkungu

iintlobo zenkungu

Ukubonakala kwenkungu kwindawo ethile kunye nexesha kubonisa ukuba umphunga wamanzi okhoyo emoyeni ufikelele kwimo yokuzaliswa. Umahluko kuphela phakathi kwamafu kunye inkungu esiyibona kumphakamo othile esibhakabhakeni kukuba le yamva ikumphakamo womphezulu womhlaba. (imeko ekhethekileyo yamafu ohlobo lweStratus). Kuzo zombini iimeko, sine-hydrometeor, ebandakanya ukunqunyanyiswa kwamancinci, ngokuqhelekileyo amancinci, amaconsi amanzi. Ngokobuchwephesha, xa ukubonakala okuthe tye kungaphantsi kwekhilomitha, sithetha ngenkungu.

Kukho iindidi ngeendidi zeemeko apho inkungu inokudalwa khona, kodwa zonke zehlela kwiindlela ezimbini eziphambili zokubumba: ukupholisa kunye nokuphuma kwamanzi. Kwimeko yokuqala, xa iqondo lokushisa liwela kwindawo yombethe, utshintsho lwesigaba ukusuka kwigesi ukuya kulwelo lwenzeka kwaye amaconsi enkungu aqala ukwenza, ngeendleko zokuxinana komphunga wamanzi kwindawo engqongileyo. Inkungu yemitha okanye inkungu ye-irradiance kunye nenkungu ye-advection zombini ziinkungu ezipholileyo, nangona zonke zinobunye bazo kunye nefom kwindawo ezahlukeneyo.

Iindidi zenkungu

iintlobo zenkungu zikhona

Inkungu eqhelekileyo ehlala kwiintlambo namathafa angaphakathi kwipeninsula, ngokukhethekileyo ngexesha leenyanga zasebusika, yinkungu eqaqambileyo. Ukupholisa ebusuku kufuphi nomhlaba, apho umoya uzolile kwiatmosfera ezinzileyo, kubangela ukuba ezi nkungu zenze iibhanki ezibanzi, kwaye phantsi kweemeko ezivumayo ngokukodwa (ngaphambili zazizele kukufuma kunye namaqondo obushushu aphantsi okanye aphantsi kakhulu, 0 ukuya ku-5 ºC) omelele ngakumbi. La mafu amile, ngokungafaniyo nenkungu ye-advection, eyenziwa xa izixa ezikhulu zomoya ofudumeleyo nofumileyo zityibilika phezu kolwandle olubandayo okanye emhlabeni. Kule meko, ziinkungu eziqhelekileyo zaselunxwemeni ezingalandeli umjikelo wemini nobusuku kwaye zinokugqabhuka nangaliphi na ixesha lonyaka nangaliphi na ixesha lonyaka.

Iindlela zokuphuma kwamanzi zibe ngumphunga zikwadala inkungu yolwandle, njengenkungu yolwandle, kodwa kule meko inkungu ibakho xa umphunga wamanzi osuka kulwandle olufudumeleyo udibana nomoya opholileyo ongaphezulu kwawo. Le nkungu ixhaphakile kwi-polar yolwandle kwaye yaziwa ngokuba yi "arctic smoke". ukuguquka komphunga ngokunjalo yinkqubo ephambili ekwenziweni kwezinye iinkungu ezingaphambili. Imida efudumeleyo ngamanye amaxesha iyathontsiza kwaye, ngamagama alula, kuqhelekile ukuchonga ezo ziganeko zozibini, ngaphandle kokwahlula phakathi kokuthontsiza, amathontsi emvula amancinci kakhulu kunye nenkungu.

Enyanisweni, akukho mahluko ungako phakathi kwezi ntlobo zimbini zeemeteors (i-drizzle nenkungu) njengoko amathontsi emvula ethu makhulu kancinane kunesiqhelo kule yokugqibela. Ngaphantsi kwamagama ezinkungu ezililayo, iimeona okanye iichorreras, ezo nkungu zifumile kwaye ziphantsi kwemvula ekhanyayo ziyaziwa.

Amagama anikwe kwiindawo ezahlukeneyo

inkungu eLondon

Kukho ishumi-mhlawumbi ikhulu- e-Spain esetyenziselwa ukubhekisa kwingingqi yenkungu okanye inkungu. Kwelinye icala, kukho ukwahluka kwesi sibini samagama, njenga i-nebra, i-niebria, i-nebría, i-niubrina okanye amafu. Amagama anje ngo borrina, borrín okanye burriana aye asetyenziswa kumhlaba waseAsturian. Sikwafumana igama lokugqibela elinefom yegurriana, kunye neCantabrian variant (guarrina), apho ithontsi elixutywe nenkungu libonwa.

Phakathi kwawona magama angaqhelekanga enkungu, kwelinye icala sine taró (okanye tarol). Isuka eFenike, kwiCosta del Sol kunye neCampo de Gibraltar, bayibiza le pateni njengenkungu yolwandle ethe gqolo ukuvela ikakhulu ehlotyeni nasekuqaleni kwekwindla ejikeleze iStrait yaseGibraltar, ngamanye amaxesha isasazeka kuLwandle lweAlberan. evela eAfrika. Imimoya eyomileyo evela emazantsi, ekwazileyo ukukhupha amanzi amaninzi elwandle. Imikhumbi enqumla kumsinga kufuneka ibe nemiqondiso evakalayo ukuthintela ukungqubana okunokwenzeka.

Elinye igama elikwisinye ngudorondón. Bayisebenzisa eAragon ukubhekisa ku-a inkungu engqindilili kwaye ebandayo, ebanda kwiimeko ezininzi. Oku kugqibela kwenzeka kumaqondo obushushu angaphantsi kwe-0 ºC. (indawo yokukhenkceza yamanzi), apho amathontsi enza ifog supercool (kwimo yenguqu yesigaba ebizwa ngokuba yi-subfusion), ngoko ke xa ebetha nantoni na, enjengeepali, iingcingo, imithi okanye amatyholo ayengumkhenkce ngoko nangoko, enze umaleko womkhenkce. , kwaye yathiywa iqhwa. Umphumo uba yinkangeleko emhlophe ekhumbuza ikhephu, okanye imbonakalo-mhlaba ebangela iqabaka eqatha.

Sigqiba uphononongo lwethu olufutshane lwe-nomenclature of fogs kunye namanye amagama, afana ne-macazón, esetyenziswa ngaphakathi eCantabria ukubhekisela kwinkungu ephantsi, evaliweyo, kodwa ehlala kuphela encinci (ithala leencwadi lenkungu), i-boira, i-boirón ephuculweyo ( Ummandla waseSerrablo, eAlto Aragón) kunye ne-boirina yakhe encinci, eCatalonia, bayisebenzisela ukuchonga inkungu, kwaye ekugqibeleni ibufo okanye ibufa, ethatha igama layo kwiintaba ezisezantsi zenkungu ephuma entlanjeni, iqhutywa yimpepho yasemini.

Ezinye iintlobo zenkungu

Inkungu yokupapasha

Inkungu eyenzeka xa umoya ofumileyo udlula phezu komhlaba opholileyo yinkungu ye-advection. Amaqondo obushushu asezantsi akhokelela kumaqondo asezantsi kubushushu bomoya ofumileyo. Oku kwandisa ukufuma kwayo kwaye kubangela ukuba umphunga wamanzi osemoyeni ujiye.

inkungu engumphunga

Inkungu engumphunga, okanye inkungu ebandayo, yenziwa kukuhamba komoya opholileyo, ozinzileyo phezu kwamanzi ashushu kakhulu. Njengoko amanye amanzi ashushu eba ngumphunga, umoya obandayo ongasentla uyahluma uze umphunga wamanzi ujiye ube ngumoya obandayo. Oku kudala into eyaziwa ngokuba inkungu yomphunga, ulwandle lomsi okanye umsi wolwandle lwe-arctic.

inkungu yentaba

Olunye uhlobo lwenkungu yinkungu yentaba, kuba isiseko selifu sisezantsi encotsheni yentaba.

inkungu ngaphambili

Kubakho inkungu engaphambili xa imvula iphuma kumoya oshushu kwaye iwela kumoya obandayo nozinzileyo. Ukuba umoya ukhaphukhaphu, ukuphuphuma kwamathontsi emvula kunokunyakamisa umoya okufutshane nomhlaba, kubangele inkungu.

Ndiyathemba ukuba ngolu lwazi unokufunda ngakumbi malunga neentlobo ezahlukeneyo zenkungu kunye neempawu zazo.


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