Emva komnye we IiVeki eziNgcwele ezishushu nezizinzileyo kakhulu ezirekhodiweyo kwiindawo ezininzi zaseAndalusia, ngokutsho Uqikelelo luka-Aemet lwePasikaImozulu iyatshintsha kwakhona. Imozulu ephantse ibe yehlobo, enamaqondo aphezulu afikelela kuma-31 degrees kwiindawo ezithile zaseHuelva kunye nama-30 degrees eSeville, eCordoba, eGranada, naseJaen, inika indawo imeko eqhelekileyo kakhulu entwasahlobo: ukwanda kwamafu, iimvula, udaka, kunye nokwehla okukhulu kwamaqondo obushushu.
Kwimihla ezayo, uluntu lwase-Andalusia lujongene utshintsho olucacileyo oluya ekungazinziniNgokufika kwezaqhwithi ezininzi kunye nomoya obandayo ovela kwiAtlantiki nakwiGulf of Cádiz, uqikelelo oluvela kwi-Spanish State Meteorological Agency (Aemet) kunye neemodeli ezahlukeneyo zaseYurophu ziyavumelana ngengcamango ngokubanzi: imvula iya kubuya, ngamanye amaxesha ngamandla, ihamba neendudumo, uthuli olumileyo, kunye nomoya onamandla, ingakumbi kwiStrait of Gibraltar.
Ukususela kubushushu bePasika ukuya kutshintsho kwindlela esiphila ngayo isimo sezulu
Ukuza kuthi ga ngoku, imozulu e-Andalusia ibilawulwa yi- iimeko eziphawuleka kakhulu ze-anticyclonicInxulunyaniswa ne-Azores High kunye nomoya ofudumeleyo, amaqondo obushushu anyuka. Ubuninzi bafikelela okanye badlula ama-30 degrees Celsius kwizixeko ezininzi ezinkulu, kunye nesibhakabhaka esicacileyo kunye nobusuku obupholileyo, okudala iimeko ezifanelekileyo zemibhiyozo kunye nemisebenzi yangaphandle.
Loo meko inomhla wokuphelelwa. Ukususela ngoMvulo, isibhakabhaka siqalile ukugutyungelwa ukusuka entshona ukuya empuma ngokufika kwesigqubuthelo samafuEkuqaleni, bekungekho mvula ingako, ngaphandle kwemvula encinci kwinxalenye yesithathu esentshona yommandla kunye nobushushu obuvela eMntla Afrika. Yayilusuku lotshintsho, lusenamaqondo obushushu aphezulu, nangona amaqondo obushushu ehla kancinci kwintshona ekude.
Isitshixo sotshintsho lwemozulu sisekubunjweni kwe- inkqubo ebandayo exineneyo ekwintshona yeSiphaluka sase-IberiaLe nkqubo, enxulunyaniswa nomsele weAtlantiki kunye nomoya obandayo ofikelela kwiGulf of Cádiz, iya kuhamba kancinci ize ihlale kufutshane nomzantsi-ntshona weIberian Peninsula kangangeentsuku ezininzi, izisa imingcele kunye nemida yemvula eAndalusia.
Iimodeli zibonisa ukuba, ngolu qwalaselo, ummandla uya kuba phantsi kwempembelelo ethe ngqo yesaqhwithi kangangexesha elininzi leveki, kunye nesinye isihlandlo semvula esinokuthatha ixesha elide ukususela phakathi evekini ukuya kwimpelaveki, nangona kukho ukunyuka nokwehla kobushushu kunye nokusasazwa kweemvula.
Utshintsho lokuqala: amafu, imimoya enamandla yasempuma kunye nemvula evela entshona
Uphawu lokuqala olucacileyo lokuba imozulu itshintshile luboniswa apha. Ukuqala kweveki, kunye nemimoya enamandla kakhulu yasempuma eCadiz kunye nokwanda kancinci kancinci kokugquma kwamafu. I-Aemet igcine izilumkiso zomoya kwiphondo laseCádiz, kunye neemvuthuvuthu ezinokufikelela kwi-70 km/h emaphandleni nasemanxwemeni, kunye ne-80 km/h kwindawo yeStrait, ukongeza kwiziganeko zonxweme zamandla 7 entshona yeTarifa kunye nolwandle olusemazantsi eTrafalgar.
Ngokuphathelele amaqondo obushushu, ngoMvulo kuya kuba njalo imozulu efudumeleyo kwiidolophu ezinkulu zaseAndalusiaAmaqondo obushushu aza kufikelela kufutshane nama-29-30°C eCórdoba, eGranada, naseSeville, kwaye amanqanaba aphezulu angama-26-27°C eJerez, eHuelva, naseJaén. Kuphela entshona ekude apho kubonwa khona ukwehla okuncinci, oku kusandula ukufika komoya opholileyo kwiintsuku ezizayo.
Kuyo yonke imini nobusuku, amafu ayaphuma kwiAtlantiki aze aqale ukuhamba imvula encinci kwisithathu sasentshonaIngakumbi kwiindawo zaseHuelva naseCádiz, kunye nasentshona yeSeville. Nangona esi ingesosiqendu siphambili, sisebenza njengesilumkiso sento eza kwenzeka ngoLwesibini, kwaye ngaphezu kwako konke, ngoLwesithathu.
Imeko iya kuba nzima ngakumbi ngoLwesibini, njengoko Isibhakabhaka esinamafu okanye esinamafu kakhulu kunye neemvula ezisasazeka ukusuka entshona ukuya empuma Kuyo yonke imini, imvula iya kuba nkulu kwaye ibe nzima entshona yeAndalusia, ngelixa iya kuba isasazeke ngakumbi empuma. Okwangoku, amaqondo obushushu aphantsi aya kunyuka kancinci, kodwa amaqondo obushushu aphezulu aya kuqala ukwehla, kunye nokwehla okukhulu kwindawo yesithathu entshona yommandla.
NgoLwesithathu, usuku olubalulekileyo: imvula enkulu, udaka, kunye nokwehla kobushushu
Incopho yotshintsho lwemozulu iya kufika ngomhla NgoLwesithathu, kulindeleke ukuba ibe lolona suku lubanda kakhulu nolungazinzanga lweveki kwiindawo ezininzi zaseAndalusia. Ngaloo mini, i-Aemet iqikelela ukuba isibhakabhaka siza kuba namafu okanye sibe namafu kakhulu kunye nemvula engapheliyo, ngamanye amaxesha enzima, ehamba neentsalela zemvula. barro ngenxa yokubakho kothuli lwaseSahara oluxhonyiweyo.
Isivuthuvuthu seAtlantiki, esikwintshona yePeninsula okanye kufutshane neGulf of Cadiz, siza kujika siye kuluntu iibhendi zemvula ezicwangciswe kakuhle nto leyo eza kuchaphazela ngakumbi i-Andalusia esembindini. Amaphondo afana neMalaga neCordoba, kunye nentshona yeJaen neGranada, kulindeleke ukuba abe neemvula eziqhubekayo nezinamandla, kunye nokuba kukho iindudumo. Kwimimandla yaseMalaga efana neRonda, iAntequera, iGuadalhorce Valley, iCosta del Sol kunye ne AxarquíaImvula isenokuqhubeka imvula.
I-Aemet iyasebenza Izilumkiso ezimthubi zemvula kunye nezivuthuvuthu ubuncinane kumaphondo amathathuISeville, iMalaga, kunye neCordoba. Kwezi ndawo, imvula iqokelelana ukuya kuthi ga kwiilitha ezili-15 ngemitha yesikwere ngeyure inokwenzeka, kunye neendudumo ezinxulumene nazo kwiindawo ezifana neSierra Sur yaseSeville, ummandla waseSubbética waseCordoba, kunye nezithili zaseMalaga eziquka iRonda, iAntequera, iGuadalhorce Valley, iCosta del Sol, kunye neAxarquía. Izilumkiso ezimthubi ngemvula ukuze ufumane iinkcukacha ngendawo nexesha.
Ukongeza kwimvula, ubukho bothuli oluxhonyiweyo oluvela eMntla Afrika buya kunceda eyaziwa ngokuba “ziimvula zodaka” kwiindawo ezinkulu zoluntuNgokutsho komthunywa wengingqi ye-Aemet e-Andalusia, ezi mvula zodaka ziya kubonakala ukususela ngoLwesibini entshona ye-Andalusia kwaye ziya kuba nzima ngoLwesithathu kwiindawo eziphakathi, kunye notshintsho olungalinganiyo kuxhomekeke kubuninzi bothuli kunye nobungakanani bamanzi awela kwindawo nganye.
Omnye umlinganiswa ophambili ngoLwesithathu uza kuba ngu ukuhla okubukhali kwamaqondo obushushuIzibikezelo ezahlukeneyo ziyavumelana ukuba amaqondo obushushu aza kwehla ukuya kuthi ga kwi-10-12 degrees Celsius xa kuthelekiswa neentsuku zangaphambili kwizixeko ezifana neSeville, iCordoba, neGranada. Kwezinye iindawo zasentshona yeSpain, amazinga obushushu aphezulu aza kufikelela kwi-18-20°C, into eyahlukileyo kakhulu kuma-30°C abonwa ngeVeki eNgcwele.
Apho kuza kuna khona kakhulu imvula: unxweme lweAtlantiki kunye neAndalusia esembindini, zezona zixhamle kakhulu
Iimodeli eziphambili zokuqikelela, kuquka ne-European Centre for Meteorology, zibonisa ukuba esi siganeko siza kuhamba ezona mvula zibalulekileyo zizonke kunxweme lwaseAndalusia eAtlanticIHuelva, iCádiz kunye nentshona yeSeville zibonakala njengeephondo ezineengxelo ezibalulekileyo, ingakumbi kwiindawo zeentaba.
Kwiindawo ezifana ISierra de Grazalema Kwaye kwindawo yaseStrait, iimvula zinokuba shushu kwaye ziphindaphindeke, apho ukuqokelelana kwamanzi kudlula iilitha ezingama-70 ngemitha yesikwere kwaye kudlule ne-100 l/m² kwindawo ephakamileyo. Ezi zixa ziya kufikelelwa kwiintsuku ezininzi zemvula, phakathi koLwesithathu nangempelaveki.
Ngaphakathi, amaphondo afana eSeville, eCórdoba naseJaén Zikwaphakathi kweendawo eziza kuxhamla kakhulu ekubuyeni kwemvula. Kwezinye iimeko, iimodeli ziye zabonisa ukuba imvula ingaphinda idlule kwi-40 l/m² kwiiyure ezingama-24 kuphela kwiindawo ezithile, ingakumbi ngoLwesibini nangoLwesithathu, ngendlela yemvula kunye neendudumo.
Ngokuchasene noko, kwifayile ye- empuma Andalusia (empuma Granada kunye Almería) Imvula ayizukuba ninzi rhoqo, kwaye ngokubanzi, ayizukuba ninzi kangako. Nangona kunjalo, ukuqhubeka kolu ngcola kunye nokuba nokwenzeka kwemvula yodaka kangangeentsuku ezininzi kuya kuthetha ukuba imeko yemozulu iya kuvakala nakula maphondo, ingakumbi ukusukela ngoLwesine ukuya phambili ukuya kuthi ga ngempelaveki.
Esi siganeko sitsha semvula siza emva kweeveki ezininzi ezilawulwa yimozulu ezinzileyo, nangona kufanelekile ukukhumbula ukuba, Ekuqaleni kukaMatshi, iimvula ezinkulu ezifana noRegina okanye uTherese Sele zishiye iingqokelela ezinkulu, ingakumbi eCampo de Gibraltar nakwiindawo ezithile kunxweme lwaseAndalusia eAtlantic. Ukubuya kwemvula okwangoku kwandisa olu hlobo, kodwa emva kwemvula eyomileyo ehambelana nePasika. Jonga uhlalutyo malunga nendlela iinkqwithela ezifana noRegina iziqendu zangaphambili ezilungisiweyo.
Udaka, uthuli lwaseSahara, kunye nobude bexesha leziganeko ezingazinzanga
Uphawu olucacileyo lwesi siqendu kukuba asikuko nje kuphela imvula, kodwa sikwathetha nangemvula. uthuli nodaka oluxhonyiweyoEsi sivuthuvuthu, esikwintshona okanye kumzantsi-ntshona wePeninsula, sikhuthaza ukuvela komoya ozele ziisuntswana ezivela eMntla Afrika, ezixubana namafu kwaye zibangele ezo mvula zimdaka.
Ngokutsho kuka-Aemet, Imvula yodaka iza kuqhubeka ukususela ngoLwesibini ukuya ngoLwesihlanu Kulindeleke udaka kulo lonke elaseAndalusia, ngakumbi ngoLwesithathu nangoLwesine kumbindi wommandla. Ukususela ngoko, udaka luya kuhlala lukho kodwa imvula incinci, nto leyo enokushiya umoya uluthuli kwaye kubekho uthuli kwiimoto, kwiitreyi, nakwifenitshala yesitalato.
Xa sijonge phambili kwimpelaveki, uqikelelo lubonisa ukuba Iimvula zodaka ziza kugxila kakhulu kwimimandla esempumaOko kukuthi, kwiindawo zaseGranada naseAlmería. NgoMgqibelo, kulindeleke ukuba iimvula zichaphazele phantse kuphela eli candelo lisempuma, ngelixa ngeCawa imeko ifanele ukuba ihambe kakuhle xa kuphuma imvula ecacileyo.
Nokuba kunjalo, ixesha elichanekileyo lokungazinzi liya kuxhomekeka Ukuguquka kwe-cold front ezimeleyo kunye nokuba ingaba igqibela ngokuba yi-DANA (Isolated High-Level Depression). incinci ngakumbi kwiSithili sase-Iberia esisemazantsi. Okwangoku, ezi modeli zibonisa imeko apho imvula ecwangcisiweyo kakhulu iya kuba phakathi koLwesithathu noLwesihlanu, apho imvula isakhona, kodwa ingaqhelekanga, ngempelaveki.
Iingcali zigxininisa ukuba, ngenxa yokutshintsha kwentwasahlobo, ezi nkcukacha zinokulungiswa njengoko ixesha lokuqikelela lifinyela, ngoko ke zicebisa ukuba kulandelwe Uhlaziyo lwemihla ngemihla oluvela kwi-Aemet kunye neenkonzo ezikhethekileyo zemozuluingakumbi malunga nezilumkiso zemvula kunye neziphepho.
Amaqondo obushushu aphantsi kunye nokuguquguquka kobushushu kwiintsuku ezimbalwa
Ngaphaya kwemvula, enye yezona ziphumo zicacileyo zolu tshintsho kwimozulu iya kuba ukwehla okuphawulekayo kumaqondo obushushu aphezuluEmva kweentsuku zemozulu efana neyasehlotyeni, kunye namaqondo obushushu aphantsi kunye nemini efudumeleyo kakhulu, ukufika komoya opholileyo kuya kubangela ukuba ii-thermometers zehle ngokukhawuleza kwiiyure ezingama-24 ukuya kuma-48.
Uqikelelo lubonisa ukuba NgoLwesithathu isenokuba lolona suku lubanda kakhulu Kuyo yonke le nxalenye, kulindeleke ukuba amaqondo obushushu ehle aye kuthi ga kwi-10°C kwiindawo ezininzi aze afikelele kwi-12°C kwiindawo ezithile zesiqingatha esisentshona yelizwe. Kwizixeko ezifana neSeville, iCordoba, neGranada, apho amaqondo obushushu afikelele okanye adlule kwi-30°C ngexesha leVeki eNgcwele, amazinga aphezulu anokuhlala malunga ne-18-20°C.
Kumaphondo afana neHuelva, iCádiz, kunye neJaén, ukwehla kuya kuba kukhulu, apho amaqondo obushushu aphakathi kwe-16 kunye ne-20 degrees Celsius phakathi emini. Amaqondo obushushu aphantsi, okwangoku, aya kunyuka kancinci ngaphambi kokufika kombindi ophambili, ngaphambi kokuba azinze ngamaxabiso aqhelekileyo entwasahlobo.
Olu tshintsho lobushushu aluyi kuba lolwe-linear. Iimodeli zibonisa ukuba, Ukususela ngoLwesine, ukufika komoya oshushu kancinci Oku kunokubangela ukuba amaqondo obushushu aphezulu anyuke kwakhona aye kuma-degrees angama-7-8, ikhefu elifutshane eliya kunika ithuba lokwehla okuncinci ngempelaveki, okuhlala kuxhomekeka kwindawo yesaqhwithi kunye nokwakheka okunokwenzeka kwe-DANA (uxinzelelo oluzimeleyo kumanqanaba aphezulu).
Nokuba kunjalo, esi siqendu siza kusebenza phula umkhwa wobushushu ongaqhelekanga weentsuku ezimbalwa ezidlulileyo kwaye kubuyiselwe amaqondo obushushu kumanqanaba aqhelekileyo ngeli xesha lonyaka, into eza kubonakala ngaphakathi nangaselunxwemeni. Umahluko phakathi kweVeki eNgcwele, enye yezona zishushu kakhulu kwiminyaka yakutshanje eAndalusia, uza kuba nomtsalane kakhulu.
Kwiintsuku ezimbalwa ezizayo, iAndalusia iza kutshintsha ukusuka kwimeko yesibhakabhaka esicacileyo kunye nobushushu obuphantse bube sehlotyeni ukuya kwimeko ephawulwe yi imvula, udaka, iziphepho kunye nemozulu epholileyoUnxweme oluphakathi nolweAtlantiki lwalo mmandla luza kuchaphazeleka kakhulu. Indawo ebandayo ethe tyaba, eqiniswe ngumoya ongazinzile kunye nothuli lwaseSahara, iza kuzisa iimvula ezingapheliyo, ukwehla okukhulu kobushushu obuphezulu, kunye nezilumkiso zemozulu kumaphondo aliqela. Nangona ukungazinzi kungayi kufana kulo lonke ummandla kwaye kulindeleke ukuba kunciphe ngempelaveki, ukubuya kwemvula kuqinisekisa utshintsho kwindlela yemozulu eAndalusia emva kweVeki eNgcwele elawulwa lilanga kunye nobushushu obuphezulu.