Ingxenye enkulu yogu lwaseMedithera, ikakhulukazi I-Barcelona kanye nendawo yayo yedolobhaIdolobha livele ezinsukwini zamuva ngaphansi kolwandle olukhulu lwamafu, ladala izigcawu ezimangalisayo nezingavamile. Kusukela ekuboneni kweCollserola, eVallvidrera, kanye nendawo ezungeze iFabra Observatory, idolobha libonakala sengathi linyamalala ngaphansi kwekhaphethi elimhlophe, kunezindawo ezimbalwa eziphakeme ezibonakalayo ngaphezu kwalo.
Lesi siqephu se inkungu eningi kakhulu Akuzange kudonsele ukunaka kuphela ngemibono emihle, kodwa futhi nokuphazamiseka okubangelwa ukungabonakali kahle emigwaqweni, ogwini lolwandle, nakwezinye izikhumulo zezindiza eMedithera yaseSpain. Nakuba ababukeli abaningi basebenzisa leli thuba ukuthatha izithombe zokuphuma kwelanga, abanye bahlangabezane nokubambezeleka, izindlela eziphambukayo, kanye nezinye izinkinga zokuhamba kanye nokuphazamiseka. izexwayiso zesimo sezulu.
Ulwandle lwamafu olumboze iBarcelona neMedithera
Lesi simo sisakazeke kulo lonke Ugu lweMedithera, ukusuka e-Empordà kuya eJáveabedlula endaweni yaseBarcelona futhi befika naseziQhingini zasePitiusas. Ezindaweni eziningi zogu lolwandle, inkungu yahlala amahora amaningi, inika umbono wokuthi ulwandle kanye nedolobha kwakucashe ngaphansi kwengqimba enkulu yenkungu.
Endabeni yaseBarcelona, izithombe ezihlaba umxhwele kakhulu zitholakale ezindaweni eziphakeme zezintaba zaseCollserola. Kusukela eVallvidrera, ekuseni kakhulu, ulwandle lwamafu phezu kweBarcelona Yanwebeka ngaseMedithera, ilanga liphuma phezu komkhathizwe futhi likhanyisa kancane ubuso benkungu, njengokungathi ulwandle olumhlophe oluhamba kancane.
Ku-timelapse ethathwe eduze kwase Indawo Yokubuka Izinto eFabraUngabona indlela inkungu ejikeleza ngayo ngaphansi kwesakhiwo sokubuka ngenkathi idolobha licwiliswe cishe. Ungqimba olunenkungu luhamba kancane, lugcwalisa izigodi kanye nengxenye engezansi yendawo yasemadolobheni kuyilapho iziqongo nezakhiwo ezinde kakhulu zibonakala zinamahloni.
Lezi zinhlobo zezimo azigcini nje endaweni yaseBarcelona. Izigameko ezifanayo ziqoshwe ogwini lwaseCatalan naseBalearic. izinkungu zolwandle ezihlala isikhathi eside, eziye zamboza izindawo ezinkulu zogu futhi zangena endaweni engakagudli ugu, zithandwa umoya ozinzile kanye nokungabikho komoya ngokuphelele.
Izithombe eziyisithonjana: I-Sagrada Família ne-Montjuïc zimbozwe yinkungu
Izithombe ezithathwe ngabantu abasafufusa abavela eVallvidrera zibonisa IBarcelona cishe ayibonakaliKwesinye sezithombe, isithunzi seSagrada Família singabonakala ngenkungu, sibonakala phansi kwesobunxele sohlaka, singabonakali kahle ngaphansi kwengubo enkulu yenkungu emboze idolobha.
Kwesinye isithombe, okugxilwe kakhulu entabeni ye- I-Montjuïc ivela ngaphezu kolwandle lwamafuUkuhlanganiswa kwenkungu evela olwandle, inkungu yasemadolobheni, kanye nesimo sendawo kudala indawo eyingqayizivele kakhulu: izingxenye eziphakeme zigqama njengeziqhingi kuyilapho yonke indawo imbozwe ungqimba olumhlophe.
Isikhathi sosuku sinezela nokumangalisa okwengeziwe. Izithombe ezithathwe ku- ukusa, ngokukhanya okufudumele, okuphansiZakha isimo esifana nephupho. Imibala yegolide yelanga eliphumayo ihlangana nombala ompunga othambile kanye nomhlophe wenkungu, okuholela endaweni abaningi abayichaza njengemilingo, kodwa empeleni okubangelwa izindlela zomkhathi ezaziwa kakhulu ngababikezeli bezulu.
Lolu hlobo lwamafu alugcini nje ngokuba yingozi enkulu noma ezimweni ezimbi kakhulu. Eqinisweni, luyingxenye ye izenzakalo ezivamile zasebusika kanye nasekuqaleni kwentwasahlobo ogwini lwaseMedithera, nakuba kungahlali kumangalisa noma kuhlanganiswe nezimo ze-photogenic njengakulesi simo.
Kungani ulwandle lwamafu lwakheka phezu kweBarcelona?
Isihluthulelo salokho okuye kwabonwa kulezi zinsuku eBarcelona nakwezinye izindawo zaseMedithera yi- Inkungu yolwandle yokuhlaselaLesi simo senzeka lapho umoya omanzi, ovela olwandle, uhamba kancane ubheke ogwini futhi uthinta indawo ebandayo, njengomhlaba ebusuku noma ekuseni kakhulu.
Uma lowo moya ogcwele umswakama uphola ngokwanele ukufinyelela iphuzu lamazoloUmhwamuko wamanzi uhlangana ube amaconsi amancane alengayo. Lokhu kwakha amabhange enkungu angamboza izindawo ezinkulu zogu futhi angene ngaphakathi ezweni, ikakhulukazi ezigodini nasemathafeni avulekele ulwandle.
Lezi zinkungu zivela kaningi ezimweni zokuphazamiseka kwengqondo. i-anticyclone kanye nokuzinza komoyaIsimo sezulu esizolile, esinemimoya elula kakhulu, sivimbela umswakama ukuthi ungahlangani futhi unyamalale ngokushesha. Ngaphezu kwalokho, kusiza ukwakheka kokuguqulwa kwezinga lokushisa: ungqimba lomoya obandayo eduze komhlabathi nomoya ofudumele ngaphezulu, osebenza njengesivikelo futhi ubambe inkungu ezingqimbeni ezingezansi.
Ngalesi sikhathi sonyaka, umehluko phakathi kwezinga lokushisa lasebusuku kanye nezinga lokushisa lomhlabathi Lokhu kwanele ukuqinisa ukupholisa emazingeni aseduze nobuso. Yingakho inkungu ingaqhubeka futhi idlulele ngale kwamahora okuqala osuku, njengoba kwenzekile ezindaweni eziningi ogwini lwaseCatalan naseValencian.
Inkungu iqala ukunyamalala njengoba ilanga likhuphuka, izinga lokushisa lomhlabathi likhuphuka kancane, nomoya uphazamisa ukushintsha kwezinga lokushisa. Kusukela ngaleso sikhathi kuqhubeke, amaconsi amanzi amile kancane kancane ayanyamalala, futhi ulwandle lwamafu ekugcineni luyanyamalala, lunikeze indawo isibhakabhaka esibuswa yilanga kanye namafu ambalwa aphezulu ahlakazekile.
Inkungu yolwandle, ukubonakala kanye nezinye izinto ezihlobene nayo
Ngale kwemibono emihle evela emibonweni yeBarcelona, lesi sigameko sibe nemiphumela engokoqobo. ukwehla okungazelelwe kokubonakala Kuthinte ukuhamba kwezimoto zasolwandle kanye nezomhlaba ezingxenyeni ezahlukene zogu lwaseMedithera, ikakhulukazi okwenza kube nzima ukuhamba kwezimoto ekuseni kakhulu.
Kwezinye izikhumulo zezindiza zasogwini, njenge-IbizaInkungu enkulu iphoqelele izinguquko zokusebenza. Okungenani icala elilodwa libikiwe lapho indiza kwadingeka iyeke ukufika kwayo yabe isibuyela emuva ngenxa yokungabonakali kahle emzileni wendiza. Imigwaqo eCatalonia naseziQhingini zaseBalearic nayo ibhekane nezindawo ezimbozwe inkungu enkulu amahora amaningi, okudinga ukuqaphela okukhulu.
Amabhange we inkungu yolwandle Zivame kakhulu phakathi kokuphela kobusika kanye nokuqala kwentwasahlobo entshonalanga yeMedithera. Zakheka ngenxa yokungafani kwezinga lokushisa phakathi kwamanzi, asabanda ngemva kwezinyanga zasebusika, kanye nomoya ofudumele kancane, onomswakama okhuphuka ngaphezu kwawo. Umphumela uba ukuminyana okudala umhwamuko oqinile, ongaguquki phezu kolwandle kuze kube yilapho umoya, ngokuvamile ovela empumalanga, ulusunduzela ogwini.
Eceleni kwalolu lwandle lwamafu, isimo se-anticyclonic esibusa i-peninsula senza kube nezinye izenzakalo ezibonakalayo nezomkhathiPhakathi kwazo kukhona okuthiwa "izinsika zelanga", izinsika zokukhanya eziqondile ezivezwa esibhakabhakeni lapho imisebe yelanga iboniswa ngamakristalu eqhwa akhona emafwini aphezulu, ngokuvamile i-cirrostratus.
Ukuzinza nakho kusiza ukuvela kwe- ungqimba olunsundu lokungcola Emadolobheni amakhulu, kubonakala ezindaweni eziphakeme. Ukucindezela okuphezulu kanye nokuntuleka komoya kuvimbela ukusabalala kwezinhlayiya, okwenza kube kubi kakhulu ikhwalithi yomoya kanye nokubonakala okuvundlile, ikakhulukazi ezindaweni zasemadolobheni ezinabantu abaningi njengeBarcelona.
Indima ye-anticyclone kanye nesibikezelo sezinsuku ezizayo
Isimo sezulu kulezi zinsuku sibonakala nge- i-anticyclone eqinile Lolu hlelo lugcina isimo sezulu sizinzile engxenyeni enkulu yeCatalonia nakwezinye izingxenye zeMedithera. Umphumela oqondile uwukuhlanganiswa kokukhanya kwelanga, inkungu, amafu aphansi, kanye nokushintshashintsha kwezinga lokushisa, nezinsuku ezibonakala zizolile kodwa futhi nezenzakalo ezimangalisayo ekuseni kakhulu nasebusuku.
NgoLwesithathu, amamodeli akhomba usuku oluvame ukuba nelanga, kanye Amafu aphezulu entshonalanga yeCataloniaIkakhulukazi ezifundeni zaseLleida naseTarragona, kanye nokuba khona kwamafu aphansi kanye nenkungu yolwandle e-Empordà naseTerres de l'Ebre. Ulwandle lwamafu lungaphinde luvele ezindaweni ezithile ezisogwini kanye nangaphambi kogu uma izimo ezifanayo zokuthula nomswakama ziqhubeka.
Kulindeleke ukuthi umoya ube lula, usuke empumalanga uye eningizimu-mpumalanga, okusho ukuthi ukwanda kokungena komswakama okuvela eMeditheraLesi simo sizovame ukwenza ukubonakala kube kubi kakhulu kwezinye izindawo ngenxa yokuhlanganiswa kwenkungu ephansi kanye nokungcola komoya, ikakhulukazi endaweni yedolobha laseBarcelona nakwamanye amadolobha amakhulu.
Ngokuphathelene namazinga okushisa, ukwehla okuncane kwamazinga okushisa aphezulu kulindeleke ogwini nasezindaweni zangaphambi kogu, kanti kwezinye izindawo zaseCatalonia, amanani azofana kakhulu nalawo ezinsuku zakamuva. Kodwa-ke, ubusuku buzobanda kakhulu ngenxa yokuguquguquka kwamazinga okushisa. amazinga okushisa aphansi aseduze no-0ºC-5ºC engxenyeni esenyakatho nasemaphethelweni ezigodi.
Uma sibheka phambili ezinsukwini ezimbalwa ezizayo, kulindeleke ukuthi ukuqinisa i-anticyclone Ngisho nangaphezulu ngoLwesine, okungaba usuku lokugcina olucacile ukuthi lugcwele ilanga. Akukho ukumbozwa kwamafu okukhulu okulindelekile, kodwa inkungu yolwandle izoqhubeka ogwini lwaseCatalan, igcine kungenzeka ukuthi kube nezinye iziqephu zokumbozwa kwamafu ezindaweni ezifana neBarcelona uma izimo zilungile.
Uthuli lwaseSahara, ukushintsha kwesimo sezulu kanye nokuphela kokuzinza
Kusukela ngoLwesihlanu, amamephu abonisa ukufika kwe Amafu okuqala avela entshonalanga ephelezelwa ngu Uthuli lwaseSahara olumisiweLokhu kungena komoya ogcwele izinhlayiya ezincane kungafiphaza isibhakabhaka, kudale umbala omhlophe noma o-orenji futhi kwandise ubumnyama ogwini kanye nangaphakathi kwe-peninsula.
Empeleni, akukho mvula enkulu elindelekile esikhathini esifushane, futhi amazinga okushisa azohlala efana. ithambile futhi ifana naleyo yezinsuku zangaphambiliniKodwa-ke, umkhathi uzoqala ukukhombisa izimpawu zokushintsha njengoba impelasonto iqhubeka, njengoba isibhakabhaka siba namafu kakhulu ngenxa yokuhlanganiswa kwamafu aphakathi nendawo aphezulu kanye nothuli lwaseSahara.
ISonto lingase libe namafu kancane, kodwa lokhu akusho ukuthi kuzoshintsha kakhulu isimo sezulu esingazinzile. Kuzoba ngesikhathi isonto lokuqala likaMashi lapho i-anticyclone iqala ukuncipha, ivumela iziphepho ezizosondela zivela endaweni ezungeze iPortugal futhi ezingavuselela imvula e-Iberian Peninsula.
Uma lesi simo siqinisekiswa, Imvula ingabuya Ngesonto elizayo, isimo sezulu samanje, esibonakala ngezimo ezizinzile, inkungu yasekuseni, kanye nezikhathi zokumbozwa kwamafu phezu kweBarcelona nezinye izingxenye zeMedithera, kulindeleke ukuthi siphele. Kodwa-ke, uma nje i-anticyclone isekhona, kungenzeka ukuthi sizobona idolobha liphuma ezingqimbeni zenkungu ekuntweleni kokusa maduze nje.
Lesi siqephu sakamuva se- ulwandle lwamafu phezu kweBarcelona Kucacisa izinga isimo esibonakala sizolile, esiphawulwa yi-anticyclone eqhubekayo, esingadala ngalo izinto eziphawulekayo njengenkungu yolwandle, ukuphuma kwelanga nedolobha elicishe lifihleke, kanye neminye imiphumela yokukhanya ehlobene nayo; ngesikhathi esifanayo, kugcizelela ukubaluleka kokuthi qapha ngokucophelela isibikezelo sezulu, kokubili ngenxa yomthelela wayo ekuhambeni nasekubonakaleni kanye nangenxa yezinguquko ezilindelekile ngokufika kothuli lwaseSahara kanye nobuthakathaka obuqhubekayo bokuzinza komoya entshonalanga yeMedithera.