Uninzi lonxweme lweMeditera, ngakumbi IBarcelona kunye nommandla wayo wedolophuEsi sixeko sivele kwiintsuku zakutshanje phantsi kolwandle olukhulu lwamafu, senza imiboniso emangalisayo nengaqhelekanga. Ngokwembono yaseCollserola, eVallvidrera, nakwindawo ejikeleze iFabra Observatory, isixeko sibonakala ngathi siyanyamalala phantsi kwekhaphethi emhlophe, kukho iindawo ezimbalwa eziphakamileyo ezibonakalayo ngaphezulu kwaso.
Esi siqendu se inkungu exineneyo kakhulu Ayikhange itsale ingqalelo kuphela ngenxa yemibono emihle, kodwa kwanokuphazamiseka okubangelwe kukubonakala okungekuhle ezindleleni, elunxwemeni, nakwezinye izikhululo zeenqwelo moya kwiMeditera yaseSpain. Nangona ababukeli abaninzi besebenzise eli thuba ukufota ukuphuma kwelanga, abanye badibana nokulibaziseka, iindlela eziphambukayo, kunye neminye imiba yokuhamba kunye nokuphazamiseka. izilumkiso zemozulu.
Ulwandle lwamafu olugubungela iBarcelona kunye neMeditera
Le nto isasazeke kulo lonke Unxweme lweMeditera, ukusuka e-Empordà ukuya eJáveaudlula kummandla waseBarcelona uze ufikelele nakwiZiqithi zasePitiusas. Kwiindawo ezininzi zonxweme, inkungu yahlala iiyure ezininzi, inika umbono wokuba ulwandle nesixeko zazifihliwe phantsi komaleko omkhulu wenkungu.
Kwimeko yaseBarcelona, ​​​​ezona mifanekiso zibalaseleyo zifunyenwe kwiindawo eziphakamileyo zeentaba zaseCollserola. Ukusuka eVallvidrera, kusasa, ulwandle lwamafu phezu kweBarcelona Yanwebeka yaya ngaseMeditera, ilanga liphuma phezu komphezulu kwaye likhanyisela kancinci umphezulu wenkungu, ngokungathi lulwandle olumhlophe oluhamba kancinci.
Kwi-timelapse ethathwe kufutshane ne Indawo yokujonga izinto eFabraUngayibona indlela inkungu ejikeleza ngayo ngaphantsi kwesakhiwo sokujonga izinto ngelixa isixeko singaphantsi kwamanzi. Umaleko onomphunga uhamba kancinci, ugcwalisa iintlambo kunye nenxalenye esezantsi yendawo yedolophu ngelixa iincochoyi kunye nezakhiwo ezinde zibonakala zisoyika.
Ezi ntlobo zeemeko azipheleli nje kwindawo yaseBarcelona. Iziganeko ezifanayo zirekhodwe kunxweme lwaseCatalan naseBalearic. iinkungu zolwandle ezihlala zihleli, eziye zagubungela iindawo ezinkulu zonxweme zaza zangena kwindawo engaphambi konxweme, zithandwa yimozulu ezinzileyo kakhulu kunye nokungabikho komoya ngokupheleleyo.
Imifanekiso eqingqiweyo: ISagrada FamÃlia kunye neMontjuïc zigqunywe yinkungu
Iifoto ezithathwe ngabantu abangengabo abaphumeleleyo kwiVallvidrera zibonisa IBarcelona ayibonakali kangakoKwenye yeefoto, umfanekiso weSagrada FamÃlia unokubonwa ngenkungu, ubonakala ezantsi ngasekhohlo kwesakhelo, ungabonakali lula phantsi kwengubo enkulu yenkungu egubungela isixeko.
Komnye umfanekiso, ingqwalasela ephambili yintaba ye IMontjuïc ivela ngaphezu kolwandle lwamafuInkungu evela elwandle, inkungu yasezidolophini, kunye nembonakalo yomhlaba kudala umbono owahlukileyo kakhulu: iindawo eziphakamileyo zibonakala njengeziqithi ngelixa ezinye iindawo zomhlaba zigqunywe ngumaleko omhlophe.
Ixesha losuku longeza umbono ongaphezulu wobuhle. Iifoto ezithathwe apha kusasa, ngokukhanya okufudumeleyo nokuphantsiZidala umoya ofana namaphupha. Imibala yegolide yelanga eliphumayo idibana nombala ongwevu othambileyo kunye nomhlophe wenkungu, nto leyo ebangela ukuba kubekho umhlaba ochazwa njengomlingo, kodwa oku kungenxa yeendlela zomoya ezaziwa kakhulu ziingcali zemozulu.
Olu hlobo lwamafu alupheleli nje kwiingqele ezinkulu okanye kwiimeko ezinzima kakhulu. Enyanisweni, luyinxalenye izinto eziqhelekileyo zokuphela kobusika kunye nokuqala kwentwasahlobo kunxweme lweMeditera, nangona ingasoloko inomtsalane okanye idityaniswe neemeko ezifana nezo ze-photogenic njengakule meko.
Kutheni ulwandle lwamafu lwenzeka phezu kweBarcelona?
Isitshixo sento eye yabonwa kule mihla eBarcelona nakwezinye iindawo zaseMeditera kukuba inkungu yolwandleLe nto yenzeka xa umoya ofumileyo, ovela elwandle, uhamba kancinci usiya elunxwemeni uze udibane nomphezulu obandayo, njengomhlaba ebusuku okanye kusasa.
Xa loo moya uzele bumswakama uphola ngokwaneleyo ukufikelela Indawo yombetheUmphunga wamanzi ujika ube ngamathontsi amancinci axhonyiweyo. Oku kwenza iinkungu ezinokugubungela iindawo ezinkulu zonxweme kwaye zihambe ziye ngaphakathi, ingakumbi kwiintlambo nasemathafeni avulekele ulwandle.
Ezi nkungu zibonakala rhoqo kwiimeko i-anticyclone kunye nozinzo lomoyaImozulu ezolileyo, enemimoya ekhaphukhaphu kakhulu, ithintela umswakama ukuba ungaxubeki kwaye unyamalale ngokukhawuleza. Ngaphezu koko, ikhuthaza ukwenziwa kotshintsho lobushushu: umaleko womoya obandayo okufutshane nomhlaba kunye nomoya ofudumeleyo ongaphezulu, osebenza njengomqobo kwaye ubambe inkungu kwiindawo ezisezantsi.
Ngeli xesha lonyaka, umahluko phakathi kobushushu basebusuku kunye nobushushu bomhlaba Oku kwanele ukuqinisa ukupholisa kumanqanaba akufutshane nomphezulu. Yiyo loo nto inkungu inokuthi iqhubeke ize idlulele ngaphaya kweeyure zokuqala zemini, njengoko kwenzekile kwiindawo ezininzi ezikunxweme lwaseCatalan naseValencian.
Inkungu iqala ukunyamalala njengoko ilanga linyuka phezulu, ubushushu bomhlaba bunyuka kancinci, kwaye umoya uphazamisa ukuguquka kobushushu. Ukususela ngelo xesha ukuya phambili, amathontsi amanzi axhonyiweyo ayanyamalala kancinci kancinci, kwaye ulwandle lwamafu ekugqibeleni luyanyamalala, lunika indawo yesibhakabhaka esilawulwa lilanga kunye namafu ambalwa aphezulu asasazekileyo.
Inkungu yolwandle, ukubonakala kunye nezinye izinto ezinxulumene nayo
Ngaphandle kwemibono emihle evela kwimbono yeBarcelona, ​​esi siganeko sibe nemiphumo ebonakalayo. ukuncipha ngequbuliso kokubonakala Ichaphazele izithuthi zaselwandle nezomhlaba kwiindawo ezahlukeneyo zonxweme lweMeditera, ingakumbi ezo zibangela iingxaki kwiiyure zokuqala zosuku.
Kwezinye izikhululo zeenqwelo-moya ezikunxweme, ezifana ne-IbizaInkungu eninzi inyanzelise utshintsho ekusebenzeni. Ubuncinane ityala elinye liye laxelwa apho inqwelo-moya kwafuneka iyeke ukufika kwayo yaza yajika ngenxa yokungabonakali kakuhle kwindlela yokumisa iinqwelo-moya. Iindlela zaseCatalonia nakwiZiqithi zaseBalearic nazo ziye zafumana iindawo ezigutyungelwe yinkungu eninzi kangangeeyure ezininzi, nto leyo efuna ukulumka kakhulu.
Iibhanki ze inkungu yolwandle Ziqhelekile phakathi kobusika basekupheleni nasekuqaleni kwentwasahlobo kwintshona yeMeditera. Zivela ngenxa yomahluko wobushushu phakathi kwamanzi, abandayo emva kweenyanga zasebusika, kunye nomoya ofudumeleyo nofumileyo onyuka ngaphezu kwawo. Isiphumo kukufuma okudala umphunga oxineneyo, ongashukumiyo phezu kolwandle de umoya, odla ngokuvela empuma, ulutyhalele elunxwemeni.
Kunye nolwandle lwamafu, imeko ye-anticyclonic elawula i-peninsula ibangela ezinye izinto ezibonakalayo nezomoyaPhakathi kwazo kukho ezibizwa ngokuba "ziintsika zelanga", iikholamu ezithe nkqo zokukhanya ezibonakala esibhakabhakeni xa imitha yelanga ibonakaliswa kwiikristale zomkhenkce ezikhoyo emafini aphezulu, ngokuqhelekileyo i-cirrostratus.
Uzinzo lukwanceda ukuvela kwe umaleko wongcoliseko omdaka Kwizixeko ezikhulu, zibonakala kwiindawo eziphakamileyo. Uxinzelelo oluphezulu kunye nokungabikho komoya kuyathintela ukusasazeka kwamasuntswana, nto leyo ebangela ukuba umgangatho womoya ube mandundu kakhulu kwaye ukubonakala ngokuthe tye kube mandundu, ingakumbi kwiindawo ezinabantu abaninzi ezifana neBarcelona.
Indima ye-anticyclone kunye noqikelelo lweentsuku ezizayo
Imo yezulu kule mihla iphawulwa yi- i-anticyclone enamandla Le nkqubo igcina imozulu izinzile kulo lonke elaseCatalonia nakwezinye iindawo zaseMeditera. Isiphumo esithe ngqo kukudityaniswa kwelanga, inkungu, amafu aphantsi, kunye nokuguquguquka kobushushu, kunye neentsuku ezibonakala zizolile kodwa kunye neziganeko ezimangalisayo kusasa nasebusuku.
NgoLwesithathu, iimodeli zikhomba kwimini enelanga ngokubanzi, kunye Amafu aphezulu entshona yeCataloniaIngakumbi kwimimandla yaseLleida naseTarragona, kunye nokubakho kwamafu aphantsi kunye nenkungu yolwandle e-Empordà naseTerres de l'Ebre. Ulwandle lwamafu lunokuphinda luvele kwiindawo ezithile ezikunxweme nakwiindawo ezingaphambi konxweme ukuba iimeko ezifanayo zoxolo nomswakama ziyaqhubeka.
Kulindeleke ukuba umoya ube lula, usuke empuma uye empuma-mpuma, nto leyo ethetha ukuba ukwanda kokungena komswakama ovela kwiMediteraLe meko iya kwenza ukubonakala kube kubi ngakumbi kwezinye iindawo ngenxa yokudibana kwenkungu ephantsi kunye nongcoliseko lomoya, ingakumbi kummandla wesixeko saseBarcelona nakwezinye izixeko ezikhulu.
Ngokuphathelele amaqondo obushushu, kulindeleke ukwehla okuncinci kwamaqondo obushushu aphezulu kunxweme nakwiindawo ezingaphambi konxweme, ngelixa kwezinye iindawo zaseCatalonia, amaxabiso aya kufana kakhulu nalawo eentsuku zakutshanje. Nangona kunjalo, ubusuku buza kubanda ngenxa yokutshintsha kwamaqondo obushushu. amaqondo obushushu aphantsi asondele kwi-0ºC-5ºC kwisiqingatha esisemantla nakwiindawo ezisezantsi zentlambo.
Ukujonga phambili kwiintsuku ezimbalwa ezizayo, kulindeleke ukuba i-anticyclone iyaqinisa Okungakumbi ngoLwesine, olunokuba lusuku lokugqibela olucacileyo ukuba lulawulwa lilanga. Akukho lifu libalulekileyo elilindelekileyo, kodwa inkungu yolwandle iya kuhlala ihleli kunxweme lwaseCatalan, igcine ithuba lokuba kubekho ezinye iziqephu zelifu kwiindawo ezifana neBarcelona ukuba iimeko zilungile.
Uthuli lwaseSahara, ukutshintsha kweemeko zemozulu kunye nokuphela kozinzo
Ukususela ngoLwesihlanu, iimaphu zibonisa ukufika kwe Amafu okuqala avela entshona ikhatshwa ngu Uthuli lweSahara ekumisweniOku kungena komoya ozele ziisuntswana ezincinci kunokusigubungela isibhakabhaka, kuvelise umbala omhlophe okanye o-orenji kwaye kwandise inkungu elunxwemeni nangaphakathi kwe-peninsula.
Ngokomgaqo, akukho mvula inkulu elindelekileyo kwixesha elifutshane, kwaye amaqondo obushushu aya kuhlala efana. ithambile kwaye ifana neyeentsuku zangaphambiliNangona kunjalo, umoya uza kuqala ukubonisa iimpawu zotshintsho njengoko impelaveki iqhubeka, isibhakabhaka siya kuba namafu amaninzi ngenxa yokudibana kwamafu aphakathi naphezulu kunye nothuli lwaseSahara.
ICawa inokuba namafu kancinci, kodwa oku akuthethi ukuba kuza kubakho utshintsho olukhulu oluya kwimozulu engazinzanga. kwiveki yokuqala kaMatshi xa i-anticyclone iqala ukuncipha, inika ithuba izivuthuvuthu eziza kusondela zivela kummandla ojikeleze iPortugal nezinokuthi zivuselele imvula kwi-Iberian Peninsula.
Ukuba le meko iqinisekisiwe, Imvula ingabuya Kwiveki ezayo, imeko yemozulu yangoku, ebonakaliswa ziimeko ezizinzileyo, inkungu yasekuseni, kunye namaxesha okugquma kwamafu phezu kweBarcelona nakwezinye iindawo zeMeditera, kulindeleke ukuba iphele. Nangona kunjalo, logama nje i-anticyclone isaqhubeka, kunokwenzeka ukuba siza kubona isixeko siphuma kwiingqimba zenkungu ekuzeni kokusa kungekudala.
Esi siqendu sakutshanje se ulwandle lwamafu phezu kweBarcelona Icacisa indlela imeko ebonakala izolile ngayo, ephawulwa yi-anticyclone eqhubekayo, enokubangela ngayo izinto ezimangalisayo ezifana nenkungu yolwandle, ukuphuma kwelanga nesixeko esiphantse singabonakali, kunye nezinye iziphumo ezibonakalayo ezinxulumene noko; kwangaxeshanye, igxininisa ukubaluleka jonga ngokusondeleyo uqikelelo lwemozulu, ngenxa yempembelelo yayo ekuhambekeni nasekubonakaleni nangenxa yotshintsho olulindelekileyo ngokufika kothuli lwaseSahara kunye nokuba buthathaka okuqhubekayo kozinzo lomoya kwintshona yeMeditera.