Xa uthetha nge Isiphepho saseMediteraOku kubhekisa kwenye yezinto ezinokuthi ziphazamise kakhulu imozulu eSpain kwiiyure ezimbalwa. Ayizizo zonke izivuthuvuthu ezifanayo; azenzeki kwiindawo ezifanayo, kwaye azizisi uhlobo olufanayo lwemvula. KwiMeditera, apho ulwandle lunokuqokelelana khona ubushushu obuninzi, iimeko zinokutshintsha ukusuka ekuzoleni ngokupheleleyo ukuya ebusika obugcweleyo obunemvula enkulu, ikhephu, kunye nokwehla okukhulu kwamaqondo obushushu.
Kwiminyaka yakutshanje sibone iziganeko ezidumileyo, ezineemvula ezinkulu, amaza kunye nemvula enkulu, kunye namagama anje ngala: nyota okanye uHarry Ezi ziganeko ziqokelelwe kwinkumbulo yethu sonke. Emva kwezi ziqendu ezininzi kukho izinto eziphindaphindayo: ukufika komoya obandayo kakhulu phezulu, ubukho bomoya ophantsi onqunyulweyo (i-DANA), ukwakheka kwenkqubo yoxinzelelo oluphantsi phakathi koMntla Afrika kunye nentshona yeMeditera, kwaye, ewe, ulwandle, olusebenza njengepetroli. Makhe sihlolisise ngokweenkcukacha indlela ezi zivuthuvuthu zeMeditera ezenzeka ngayo, indlela ezahluke ngayo kwizivuthuvuthu zeAtlantiki, kunye nohlobo lwemozulu ezinokuzisa kwiPeninsula yaseIberia nakwiZiqithi zaseBalearic.
Ukusuka kumaqondo obushushu afana nentwasahlobo ukuya kwiCawa phakathi ebusika
Enye yezona meko ziqhelekileyo iqala ngo umqolo ongaphantsi kwetropiki Ilawula imeko yemozulu eSpain, le nkqubo yoxinzelelo oluphezulu izisa amaqondo obushushu aphezulu ngokungaqhelekanga ngeli xesha lonyaka, kunye neemeko ezifana nezentwasahlobo phakathi kobusika. Nangona kunjalo, le meko izinzileyo ithatha ixesha elifutshane njengoko kusondela ukwehla okukhawulezileyo kwaye i-cyclogeneis iqala ukwenzeka kummandla weMeditera.
Kwenye yezi meko, uqikelelo lwemodeli yaseYurophu lubonisa indlela I-DANA (Uxinzelelo oluQhelekileyo oluManyeneyo kuMazinga aphezulu) Ihamba isiya emantla isuka kwindawo ekufutshane neGulf of Cádiz kunye neCanary Islands. Emva koko, le ndawo ibandayo yomoya inyuka iye kuMntla Afrika, idlula eMorocco naseAlgeria, ngaphambi kokuba ekugqibeleni iphume phezu kweMeditera iye kwiZiqithi zaseBalearic, eCorsica, naseSardinia. Le ndlela ibalulekile kuba ivumela inkqubo yoxinzelelo oluphantsi ukuba iqalise ukusebenzisana nolwandle olufudumeleyo kunye nomoya ovela kwiindawo ezahlukeneyo.
Kwangaxeshanye, ubunzima bomoya obandayo eyondla kwaye iqinise inkqubo. Ukudibana komoya we-polar ofika kumphezulu namanqanaba aphakathi, kunye nomgangatho ophantsi ohamba kuMntla Afrika, kunceda ukwakheka kunye nokuqina kwenkqubo yoxinzelelo oluphantsi kuloo ndawo. Isiphumo sesimo sezulu esinzima kakhulu, kunye nemimoya enamandla evela emantla kwintshona yeMeditera kunye nokwehla okukhulu kwamaqondo obushushu kulo lonke ilizwe.
Kwiimeko ezinjalo, iCawa idla ngokuba lolona suku lunzima kakhulu kwesi siganeko. Emva kweentsuku ezininzi zoxolo, utshintsho lunokuba ngequbuliso: isibhakabhaka esigubungele amafu, iimvula ezingapheliyo kunye nomoya obandayo ocacileyo wobusika, ingakumbi ngaphakathi elizweni nakwiindawo ezineentaba.
Apho lina khona kwaye likhithika kunye nesiphepho esisebenzayo saseMeditera
Xa imvula iphantsi, umngxuma wayo ohambelanayo, kunye neenkqubo zoxinzelelo oluphantsi komhlaba zihambelana, imvula ifikelela kwiindawo ezininzi. Kwenye yezi ziqendu, imvula isasazwa kuzo zonke iindawo. I-Castilla-La Mancha, iAragon, iLa Rioja, iNavarre, impuma ye-Andalusia, i-Valencian Community, i-Balearic Islands, iNgingqi yaseMurcia kunye neCatalonia.Yimeko apho unxweme lweMeditera kunye nenxalenye yesithathu esemantla yelizwe zichaphazeleka kakubi kakhulu.
Imvula elindelekileyo iyonke iphakathi kweelitha ezi-5 nezingama-30 ngemitha yesikwere, kodwa umhlaba udlala indima ebalulekileyo. Kwiindawo zeentaba, apho umoya unyanzelwa ukuba unyuke khona, ubungakanani bunokunyuka kakhulu. EMpuma AndalusiaIngakumbi kwiintaba zaseGranada naseJaén, akuqhelekanga ukubona imvula epheleleyo yeelitha ezingama-30 ukuya kwezingama-40 ngemitha yesikwere kwiiyure ezimbalwa nje. Kumantla eSpain, iPyrenees esembindini (iHuesca neNavarre) kunye neZaragoza esentla nazo zifumana ukuqokelelwa okukhulu kwezi meko.
Ummandla weMeditera usabela ngokukhawuleza kwiipateni zomoya. Ukuba umsinga osemantla okanye emantla-mpuma ufika emva kokuwela ulwandle, umzantsi we IGulf of Valencia Ihlala phantsi kohlobo "lwebhanti yokuhambisa" yamafu agcwele umswakama akhupha umsindo wawo. Iimvula ezinkulu ziyana ngexesha elifutshane, ngamanye amaxesha zihamba neendudumo, kwaye ngamanye amaxesha, nodaka ukuba luhambelana nokufika kothuli lwaseSahara oluqhutywa sisivuthuvuthu ngokwaso. Olu thuli lwaseSahara lunokubangela ukuba kubekho inyani. iimvula zodaka kwiindawo ezivezwe ngaphandle.
Ikhephu liba yinto ebalulekileyo. Ngokufika komoya obandayo kunye nokudlula kwe-DANA (i-isolated high-altitude depression), inqanaba lekhephu kumantla eSpain lisenokuhla liye kufikelela [kwindawo engekhoyo]. 1000 mithaIiPyrenees kunye neIberian System zihlala ziindawo ezixhamla kakhulu kwezi khephu, kunye nokuqokelelana okukhulu kwiindawo eziphakamileyo eziphantsi ngeli xesha lonyaka. Ngamanye amaxesha, ikhephu lingabonakala nakwiiNtaba zaseCantabrian, ingakumbi xa umsinga osuka emantla uzisa umoya obandayo kakhulu nofumileyo ovela kuLwandle lwaseCantabrian.
Okwangoku, imimoya ye-tramontana kunye ne-mistral inokubangela i-real isaqhwithi saselwandle kwintshona yeMeditera. Amaza amakhulu, ulwandle olurhabaxa kunye neemvuthuvuthu ezinamandla kakhulu zenza imeko ibe nzima kunxweme lwaseCatalan, eValencian naseBalearic, kunye nakumantla eAlgeria.
Ukwehla kobushushu: ukusuka phantse ehlotyeni ukuya kwindawo yokukhosela kwiiyure ezimbalwa
Enye yezona zinto zibonakalayo emhlabeni kukungxama ukuhla kwamaqondo obushushuEmva kweentsuku ezininzi zobushushu obuphezulu kakhulu ngeli xesha lonyaka, ukudlula kwe-DANA (i-isolated high-level depression) kunye nokwenziwa kwesiphepho saseMeditera kunokuzisa uvakalelo lwasebusika. Kwisiqingatha esisemantla se-Iberian Peninsula, amaqondo obushushu aphezulu akafiki kangako phakathi kwe-10 kunye ne-15°C, aphantsi kakhulu kune-avareji yangaphambili.
Kunxweme lweMeditera, apho ulwandle ludla ngokuthambisa umahluko, amaqondo obushushu aphezulu aqala kwi-14 ukuya kwi-17 ºC, kodwa amaqondo obushushu aphantsi abonwa ngenxa umoya onamandla Kunye nokufuma okuphezulu. Izixeko ezifana ne-Oviedo zingahlala malunga ne-11ºC, iZaragoza malunga ne-10ºC kunye neMadrid malunga ne-15ºC ngosuku olunokuthi, ngaphandle kwale meko yemozulu, lube shushu kakhulu.
Intlambo yaseGuadalquivir idla ngokuba luhlobo oluthile "Indawo yokutyeba"Nangona ezinye iindawo zeSiqingatha sase-Iberia zipholile, iSeville kunye neCórdoba zinokufikelela kumaqondo obushushu afikelela kwi-21°C, ngenxa yendawo yazo ekhuselekileyo kwimimoya ebandayo yasentla nasempuma-mpuma, kunye nempembelelo yeenkqubo zoxinzelelo oluphezulu ezikufutshane. Nangona kunjalo, umahluko phakathi kweentsuku zangaphambili nawo uyabonakala kwezi ndawo.
Ukuba, emva kokudlula kokuqala komgangatho ophantsi, umoya obandayo ngakumbi ufika uvela kwiindawo eziphezulu, amaqondo obushushu aphantsi ebusuku nawo aya kwehla. Kulapho kuvela khona iqabaka kwiindawo ezingaphakathi, kwaye kunokwenzeka ukuba... inqanaba lekhephu Iyaqhubeka nokuhla, ishiya imiboniso yasebusika kwiindawo apho ingaqhelekanga khona.
Utshintsho olulandelayo: ukusuka kwisaqhwithi ukuya ekubuyeni kwe-anticyclone
Xa isiphepho saseMeditera sifikelele kwincopho yaso, indlela esihamba ngayo itshintsha kwakhona. Ukususela ngoMvulo ukuya phambili, inkqubo yemozulu idla ngokuqala "ukuphinda ihlangane". anticyclone Kumzantsi-ntshona wePeninsula, kutyhala inkqubo yoxinzelelo oluphantsi ngasempuma. Le ntshukumo ikhuthaza ukuzinza kwemozulu kancinci kancinci, nangona ingekho ngoko nangoko: isiqingatha sokuqala sosuku sisenokuba siphawulwe yimvula kunye nesibhakabhaka esinamafu kakhulu kwiindawo ezahlukeneyo.
Kwezi meko, indawo yokudibana phakathi kwe-tramontana kunye nemimoya ye-mistral idla ngokuba phezu kwe- unxweme oluphakathi lwaseCatalan kunye neziqithi zaseBalearicIBarcelona, iGirona kunye neziqithi zinokuqokelelana phakathi kwe-10 kunye ne-20 l/m² kwiiyure ezimbalwa, kunye neemvula ezincipha kancinci kancinci njengoko isaqhwithi sisiya embindini weMeditera.
Okwangoku, emantla nasemantla ntshona e-Iberia Peninsula aziphuncuki kwi-cloud cover. I-Cantabria, i-Basque Country, i-Asturias, kunye ne-Galicia ziyaqhubeka nokubona isibhakabhaka esigubungeleyo kunye nemvula, kunye nomlinganiselo onokufikelela kwi-25 l/m² kwiindawo ezivezwe kunxweme lwase-A Coruña kunye nonxweme lwase-Cantabrian. Iipyrenees Iyaqhubeka nokuwa kwekhephu, ubukhulu bayo bungaphezulu kweesentimitha ezi-5 ukusuka kwiimitha ezili-1000, nto leyo edibanisa ikhephu.
KwiiNtaba zaseCantabrian, kukho ikhephu elincinci elisekhona, kodwa liya lisiba manqaphanqapha njengoko i-anticyclone isanda. Nangona kunjalo, imimoya ephuma emantla okanye emantla-mpuma kunye nolwandle olusarhabaxa kwiMeditera zizikhumbuzo zokuba isivuthuvuthu saseMeditera sidlule apho kutshanje.
I-DANA, i-cyclogenesis eqhumayo kunye neemvula zodaka: "umzuzu walo mzuzu" wemozulu
Kukho iindlela ezimangalisayo apho cyclogenesis eqhumayo Kwingingqi yeAtlantiki okanye kufutshane neIberia Peninsula, idibana ne-cut-off low ephezulu (i-DANA). Kwezi meko, inkqubo yoxinzelelo oluphantsi ephumayo ivelisa imimoya enamandla kunye nokutsala umoya obandayo kakhulu we-polar odibana nomoya opholileyo ohambelana ne-cut-off low. Phakathi kwezi meko zimbini, kwakheka i-front esebenzayo kakhulu, ekwaziyo ukuvelisa imvula enamandla, izivunguvungu, kwaye, ukuba ihambelana nothuli lwaseSahara oluxhonyiweyo, izivunguvungu zokwenyani. iimvula zodaka.
Kule meko, i-cut-off low iya kumzantsi-mpuma ngelixa idibana nomngxuma omkhulu. Ngaphezulu, oku kudibana kuthetha ukuba I-cyclogenesis yeMediteraOko kukuthi, ekwakhiweni nasekuqinisweni kwenkqubo yoxinzelelo oluphantsi phezu kolwandle. Le ndawo intsha isezantsi, ekwimpuma-mpuma yeSiqithi sase-Iberia, isebenza njengepompo, iqhubeka nokuhambisa uthuli lwaseSahara ukuya kwicala elingasempuma leSiqithi sase-Iberia nakwiZiqithi zaseBalearic, rhoqo kakhulu impelaveki yonke.
Isiphumo sisiphumo se-cocktail yemozulu emangalisa kakhulu: isibhakabhaka esiorenjiUdaka oluchithekileyo ezimotweni nakwiindawo eziphezu komhlaba, iishawa ezifana nobisi, kunye nomahluko omkhulu phakathi komoya obandayo wasentla nomoya ofudumeleyo, ogcwele uthuli. Konke oku kuhamba nemimoya enamandla, kwaye kwezinye iindawo, iindudumo ezinemibane. Ngamanye amaxesha, ezi meko ziye zakhokelela kwizilumkiso zemvula enkulu, ezifana nezo zikhutshwe kwiinkqwithela zangaphambili kwiindawo ezikunxweme lolwandle.
Okwangoku, ulwandle luya lusiba nesiphithiphithi ngakumbi ngenxa yomahluko woxinzelelo phakathi kwenkqubo yeMeditera enoxinzelelo oluphantsi kunye nenkqubo yoxinzelelo oluphezulu ekwintshona. Olu xinzelelo lubangela izivuthuvuthu ezinkulu zaselwandle, kunye namaza anokufikelela kwiimitha ezininzi ukuphakama aze anyanzele ukuvalwa kwamazibuko okanye ukumiswa kwezinye iindawo zonxibelelwano lwaselwandle, ingakumbi ezijikeleze iZiqithi zaseBalearic kunye nonxweme olusempuma yeSpain.
Yintoni eyahlula iziphepho zaseMeditera kwiziphepho zaseAtlantiki?
Nangona kulwimi lwemihla ngemihla sisebenzisa nje igama elithi "isiphepho", kwi-meteorology kubalulekile ukwahlula phakathi imvelaphi kunye nendlela yokusebenzaIzivuthuvuthu zaseAtlantiki, njengoko igama lazo lisitsho, zenzeka kwiNorth Atlantic, ngokuqhelekileyo zidibene ne-polar front, apho umoya obandayo we-polar udibana nomoya ofudumeleyo we-subtropical. Umthombo wazo oyintloko wamandla lo mahluko wobushushu phakathi kwe-latitudes.
Ezi nkqwithela zaseAtlantiki zihlala zizinkqubo ezinkulu kakhulu, ezineenxalenye ezibandayo, ezifudumeleyo nezivaliweyo, kunye nesakhiwo esicwangcisiweyo. Xa zifika kwiSiphaluka saseIberia, zihlala zisenza njalo ukusuka entshona okanye emantla ntshona, ziqala ngokudlula kulo lonke eli phondo. IGalicia, unxweme lwaseCantabrian kunye nentshona yelizwe, ngaphambi kokuba ifudukele ngaphakathi elizweni. Iimvula zayo zihlala ziqhubeka kwaye zisasazeka, azinamandla kakhulu kwixesha elifutshane kuneemvula zaseMeditera, kodwa zihlala zikho. Zibangela inxalenye enkulu yexesha elide lemvula egcwalisa amachibi kunye namanzi angaphantsi komhlaba.
Izivuthuvuthu zeMeditera, kwelinye icala, zivela phezu kolwandle ngokwalo. ulwandle lasemediterraneanUlwandle lweAtlantiki, ulwandle oluncinci xa luthelekiswa nolwandle lweAtlantiki, lushushu kakhulu, ingakumbi ekupheleni kwehlobo nasekwindla. Kwimeko enjalo, amandla axhomekeke kancinci kumahluko amakhulu obushushu phakathi kweendawo ezisezantsi kunye neendawo ezishushu, kodwa axhomekeke ngakumbi kubushushu kunye nokufuma okuqokelelene emanzini olwandle.
Xa umoya obandayo uphezulu, njengomoya ophantsi onqunyulweyo, uhlala phezu kolwandle olufudumeleyo, umahluko phakathi komoya obandayo ophezulu nomphezulu wolwandle ofudumeleyo ubangela ukungazinzi. Emva koko iMeditera isebenza njenge fuelIkhupha amanzi amaninzi kakhulu, anyukayo, ajiyile, aze akhuphe ubushushu, omeleza inkqubo yoxinzelelo oluphantsi. Oku kudala uhlobo lwe-feedback loop enokubangela imvula enamandla kakhulu kwiindawo ezincinci.
Ngoko ke, izivuthuvuthu zaseMeditera zihlala zincinci kwaye zihamba kancinci, okanye zingahambi kakhulu kangangeeyure okanye iintsuku. Oku kucotha, kunye nokufumaneka okuphezulu komswakama, kuthetha ukuba izandyondyo zemvula zikufutshane kakhulu, zinokubangela izikhukula ngokukhawuleza, ukugcwala kwemijelo kunye nomonakalo omkhulu kwiindawo ezithile, ngelixa imozulu inokuba noxolo ngakumbi kwiikhilomitha ezimbalwa ukusuka apho.
Iinkqwithela zakutshanje zeMeditera: ukusuka kuGloria ukuya kuHarry
Kutshanje, kubekho iziganeko eziye zaphawula utshintsho olukhulu kwindlela abantu abacinga ngayo ngengozi enxulumene neziphepho zaseMeditera. nyotaUmzekelo, oku kubangele ingxoxo malunga nokuba ibiyeyona nkqwithela inkulu yeMeditera kwiminyaka yakutshanje na. Olu hlobo lweziqhwithi ludibanisa amaza angaqhelekanga, iimvula ezinkulu, imimoya enamandla kakhulu, kwaye, ngamanye amaxesha, ikhephu elikhulu kwiindawo ezingaphakathi nezintaba kufutshane neMeditera.
Omnye umzekelo wakutshanje ungafumaneka kwi Isiphepho saseMeditera esinxulunyaniswa neSiphepho uHarryIsivuthuvuthu Isivuthuvuthu A, esathiywa ngokusemthethweni yi-AEMET, besisisivuthuvuthu sesibhozo esibizwa ngegama lesizini. Ukudlula kwaso kubangele imvula enkulu ngempelaveki kumantla-mpuma eSpain nakwiZiqithi zaseBalearic, apho ikhephu lalimalunga neemitha ezili-1000. Ukususela ngoMvulo nangoLwesibini ukuya phambili, ulwandle oluvuthuzayo kunye nemimoya enamandla yabonakala ngakumbi, kunye neemvuthuvuthu ezinamandla kunye namaza amakhulu kunxweme lweMeditera.
I-arhente yemozulu ilumkisa kwezi meko ngemfuneko yokubeka esweni ngokusondeleyo uqikelelo kunye nezilumkiso yeziganeko zemozulu ezimbi. Utshintsho kwindawo echanekileyo yesiphepho, okanye ekuqineni kwaso, lunokutshintsha kakhulu ukuba zeziphi iindawo ezithwaxwa yiso. Ukutshintsha okuncinci kwenkqubo yoxinzelelo oluphantsi ukuya entshona okanye empuma kwenza umahluko phakathi kwempembelelo enkulu egxile eCatalonia nakwiZiqithi zaseBalearic, okanye ibetha kakhulu iValencian Community, eMurcia, nasempuma yeAndalusia.
Indima yomsinga we-polar jet kunye nomoya obandayo kakhulu phezulu
Uninzi lwezi meko ziqala kwiintsuku ezingaphambili ngotshintsho kwindlela ezimi ngayo izinto. ijethi yepolarUmsinga wejethi ujikajika kwiindawo eziphakamileyo kwiindawo eziphakathi. Xa umsinga wejethi ujikajika kwiindawo ezinkulu, ukhetha ukwehla kwemimoya ebandayo ukuya kwiindawo ezisezantsi, kuquka i-Iberian Peninsula kunye nommandla weMeditera.
Kwezi meko, umqolo we-anticyclonic uphakama ukusuka emazantsi ukuya emantla ujikeleze i-Azores archipelago, ngelixa umzobo we-anticyclonic blocking uzinza entshona yeRashiya. Le patheni ishiya ucango luvulekile ukuze umkhombe ogcwele umoya obandayo kakhulu wehle uye eSpain. Isiphumo kukwehla kobushushu obungakumbi, okuhamba nemvula kwiindawo ezahlukeneyo kunye nomoya we- ebusikanangona ixesha lonyaka liqhubeka.
Ngaphakathi kuloo mgxobhozo, ngamanye amaxesha kubakho intlambo uxinezeleko oluphezulu Xa amaqondo obushushu ehlile kakhulu, malunga ne-30°C okanye angaphantsi nangakumbi kukuphakama okumalunga neemitha ezingama-5400. Le ndawo inomoya obandayo kakhulu iwela i-Iberian Peninsula ukusuka emantla ukuya emazantsi phakathi koMgqibelo noMvulo, ekugqibeleni ihlale kumantla e-Algeria. Iinkqubo zoxinzelelo oluphantsi zinokubonakala kumphezulu, zibonisa oku kungazinzi kwinqanaba eliphezulu, okuthi kamva kuhlengahlengiswe kwaye kungene nzulu phezu kweMeditera.
Ukungaqiniseki kudla ngokuba phezulu kwiintsuku ezimbalwa ngaphambi kwesi siganeko. Iimodeli zemozulu ziyavumelana ukuba kuza kubakho iimvula ezisasazekileyo kwiindawo ezininzi zelizwe, eziza kugxila kamva empuma nakwiZiqithi zaseBalearic, kodwa azivumelani ngobunzulu, ukusasazwa ngokuchanekileyo, kunye nenqanaba lekhephu. Kwimeko eqhelekileyo, inqanaba lekhephu linokuba phakathi 800 kunye ne-1200 yeemitha Kwiindawo ezininzi, nangona ukubakho komoya obandayo kunokubangela ukuwa ngamanye amaxesha kunye nokubonakala kwesichotho okanye ikhephu eliqhekekileyo kwiindawo eziphakamileyo ezisezantsi.
Iimpawu ezinokwenzeka ze-Mediterranean cyclogenesis kunye ne-subtropical
Ukususela ngeCawa ukuya phambili, ingqwalasela idla ngokugxila kwizinto ezinokwenzeka i-cyclogenesis kwiMediteraOko kukuthi, uphuhliso lwenkqubo yoxinzelelo oluphantsi oluphezulu olunxulunyaniswa nomoya obandayo kakhulu phezulu. Ngokuxhomekeke kwindlela ezi modeli eziguquka ngayo, le nkqubo yoxinzelelo oluphantsi inokuqina phakathi kweZiqithi zaseBalearic, emantla eAlgeria, kunye nommandla weCorsica-Sardinia. Indawo yayo yokugqibela kunye nobukhali buya kumisela ubukhulu besiphepho eSpain.
Ukuba isivuthuvuthu sikufutshane ne-Iberian Peninsula kunye neZiqithi zaseBalearic, imvula inokwanda ngamandla. ICatalonia, iAragon, uLuntu lwaseValencian, uMmandla waseMurcia, empuma yeAndalusia kunye neziqithi zaseBalearicKwezi ndawo, ikhephu elikhulu eliwayo kwiindawo eziphakamileyo eziphakathi ukuya kwezisezantsi aliqhelekanga, ukuba umoya obandayo ophakathi uyaqhubeka. Imimoya esentla okanye emantla-mpuma inokuba namandla kakhulu, kunye neenkanyamba ezinkulu zaselwandle kwintshona yeMeditera.
Ngaphezu koko, umoya obandayo unokuqhubeka ungena usuka kwiindawo eziphakamileyo ezisemantla, kwaye kwezinye iimeko, iimodeli zibonisa ukwakheka kwenye inkqubo yoxinzelelo oluphantsi kufutshane nomntla-ntshona wePeninsula yase-Iberia. Olu phazamiseko lutsha luya kuzisa iimvula kunye nekhephu ukuya kweminye imimandla yasentshona nasemantla, kugqityezelwa isiqendu esitshintshatshintshayo kwisikali esidibanisayo.
Kwaneziqithi zaseCanary Islands zisenokutshintsha imozulu enxulumene nale ndlela, ngokufika kwemimoya evela emantla, amaqondo obushushu aphantsi kunesiqhelo, kunye nokungazinzi okwaneleyo okubangela imvula enkulu kwindawo leyo. Ibingayi kuba lixesha lokuqala ukuba imeko elawulwa yinkqubo yoxinzelelo oluphantsi lwaseMeditera kunye nenkqubo yoxinzelelo oluphezulu lwaseAtlantic ibangele imozulu epholileyo neguquguqukayo kwezi ziqithi; eneneni, iziqendu zangaphambili zichaphazele ezi ziqithi, njengoko kuhlalutywe kwiingxelo zesiphango zeCanary Islands, ezirekhoda imvula, umoya, kunye nokudumba.
Ezinye iimodeli, kwiimeko ezigqithisileyo, zide zibonise ukuba isiphepho saseMeditera sinokubangela iimpawu ezithile ezikwi-subtropicalOku kwenzeka xa inkqubo ixhomekeka ngakumbi kubushushu obubonelelwa lulwandle, ibonisa isakhiwo esilinganayo ngakumbi kunye nombindi ofudumeleyo kumanqanaba aphantsi. Asithethi ngesivuthuvuthu esiqhelekileyo, kodwa sithetha ngenkqubo exutyiweyo enokwenza kube nzima ngakumbi ukuqikelela. Ezi meko zinzima, kwaye iimodeli zihlala zingavumelani, yiyo loo nto kugxininiswa ekujongeni ukuguquka kwazo phantse yonke imihla.
Lilonke, izivuthuvuthu zeMeditera ziye zaba yinto ephindaphindayo ebusika nasekwindla kummandla wethu. IiDANA, umoya we-polar, ulwandle olufudumeleyo kakhulu, uthuli lwaseSahara kunye nomsinga we-polar jet Ipeyinta umfanekiso weemeko ezithi, nangona ngamanye amaxesha zimangalisa ngokwembono yemozulu, zikhokelele kwimiphumo emibi kakhulu: izikhukula ezikhawulezileyo, ikhephu elikhulu eliwayo phakathi kokuphakama, imimoya enamandla kakhulu, kunye nezivuthuvuthu ezinkulu zaselwandle. Ukuqonda indlela ezikhula ngayo kunye nesizathu sokuba ziziphatha ngendlela eyoyikekayo kubalulekile ekutolikeni izilumkiso, ukulungiselela izivuthuvuthu, kunye nokuvavanya ngcono okwenzekayo xa sisiva ukuba isivuthuvuthu esitsha saseMeditera siza kufika.
