La ICalima kwakhona libali eliphambili kwiZiqithi zaseCanary Ngokutsho kwe-State Meteorological Agency (AEMET), isivuthuvuthu sothuli siza kuqala kancinci kwiindawo eziphakamileyo kwaye ekugqibeleni sichaphazele phantse lonke iqela leziqithi. Uthuli oluxhonyiweyo luya kuhambelana nokunyuka okukhulu kwamaqondo obushushu, iimeko ezomileyo, kunye nomoya onamandla kwiindawo ezibonakala kakhulu.
Emva kweentsuku ezininzi eziphawulwe kukudlula kwezivuthuvuthu, Imeko yemozulu iyatshintsha: isibhakabhaka esicacileyo okanye esinamafu kancinci siyaphumelela, amaqondo obushushu aphezulu ayanyukaUmgangatho womoya uba mandundu ngenxa yokungena kothuli lwaseSahara, kwaye iimeko zolwandle ziba nzima ngakumbi kunxweme oluninzi lweZiqithi zaseCanary.
Ukuguquka kombala womkhenkce: ukusuka ekukhanyeni ukuya kwisiqendu esiqatha
Iimodeli ze-AEMET zibonisa ukuba Ukwanda komoya ongcolileyo kuza kuqala kwiindawo eziphakamileyo ingakumbi kwiphondo lasempuma (eLanzarote naseFuerteventura) naseTenerife. Ekuqaleni, uthuli oluxhonyiweyo luya kuba buthathaka kwaye lubonakale ikakhulu kwiindawo eziphakamileyo, kunye nokuncipha okuncinci kokubonakala kunye nokufiphala esibhakabhakeni.
Njengoko iiyure zihamba, inkungu iya kusasazeka nakwezinye iziqithi. ukufumana amandla kunye nobubanziPhakathi koLwesine noLwesihlanu, uthuli lwaseSahara luza kufikelela kulo lonke iziqithi, lubonakale ngakumbi kwiindawo eziphakathi nakwiincopho zeziqithi eziphakathi nezisempuma, kunye nakwiindawo ezingaphakathi zaseFuerteventura naseLanzarote.
Uqikelelo lubonisa ukuba esi siganeko asizukuba sifutshane: Ubushushu buza kuba qatha ngempelavekiIngakumbi phakathi kobusuku bangoMgqibelo neCawa kusasa, apho kulindeleke ukuba kubekho uthuli oluninzi emoyeni. Oku kuya kubangela ukwehla okukhulu kokubonakala kunye nokuwohloka okuphawulekayo komgangatho womoya kwiindawo ezininzi zeziqithi.
Ngasekupheleni kweCawa, ukungena kothuli kuza kuqala ukuhla kwiziqithi zasentshona, ngelixa Isenokuba ibalulekile kwiziqithi ezikwimpuma njengeLanzarote, iFuerteventura kunye neLa Graciosa, apho umoya unokuhlala unomkhenkce okwethutyana.
Ukunyuka kwamaqondo obushushu: ubushushu ngaphakathi elizweni, emazantsi kunye neencopho
Oku kunxulunyaniswa nokufika komoya ofudumeleyo ovela kwilizwekazi laseAfrika, inkungu iya kuhamba ne ukunyuka kwamaqondo obushushu ngokubanzi KwiZiqithi zaseCanary. Kwiindawo ezininzi ezikunxweme lolwandle, ukwanda kuya kuba kuncinci, kugcina imeko-bume icocekile, kodwa kwiindawo eziphakathi, ezisemantla nasencotsheni ukunyuka kwamaqondo obushushu kuya kubonakala ngakumbi.
Ngokutsho kwe-AEMET, Amaqondo obushushu aphezulu aza kunyuka ngokuphakathi ngaphakathi elizweni Kwiziqithi zasempuma, amaqondo obushushu aza kunyuka ukusuka malunga nama-23°C ukuya kufikelela okanye kudlule ama-27°C kwiindawo ezithile zaseGran Canaria, eFuerteventura, naseLanzarote ngoLwesine. Kwiziqithi zasentshona, ukunyuka kuya kuba phakathi ekuqaleni, kodwa kuya kubonakala nakwiindawo eziphakamileyo.
Njengoko esi siganeko siqhubeka, ukunyuka kwamaqondo obushushu kuya kucaca ngakumbi. Uqikelelo lubonisa ukuba, xa sisondela ngoLwesihlanu ingakumbi ngoMgqibelo, amaqondo obushushu afikelela okanye adlule kwi-30ºC kwiindawo ezinkulu zephondo laseLas Palmas, enempembelelo ethile kumzantsi nasentshona weGran Canaria nakwiindawo ezingaphakathi zeFuerteventura kunye neLanzarote.
ETenerife, utshintsho luza kubonakala ngakumbi: I-AEMET iqikelela ukuba amaqondo obushushu angadlula ama-34°C Kwiindawo ezisemazantsi nasentshona zesiqithi, kunye noomasipala abafana neGuía de Isora kunye neArona phakathi kweendawo apho ubushushu buza kuba bukhulu khona. EGran Canaria, amaqondo obushushu aphezulu kulindeleke ukuba afikelele okanye adlule kwi-30°C kwiindawo ezifana neMogán, Santa Lucía de Tirajana, La Aldea, Tejeda, kunye neSan Mateo.
Ngokwahlukileyo, Izixeko ezinkulu ziya kugcina amaxabiso ethambileyoILas Palmas de Gran Canaria iya kufumaneka malunga ne-17-21ºC kwaye iSanta Cruz de Tenerife ifumaneka malunga ne-18-23ºC, kwaye amaqondo obushushu angaphantsi angatshintshi kangako kwaye ukunyuka okuncinci kumbindi womzantsi.
Uqikelelo oluqhelekileyo lweZiqithi zaseCanary: isibhakabhaka, umoya nolwandle
Kwiintsuku ezimbalwa ezizayo, imozulu kwiCanary Islands iya kuba phantsi kolawulo Isibhakabhaka esicacileyo okanye esinamafu kancinci kwiindawo ezininzi zeziqithiNgamaxesha athile amafu aphantsi emantla eziqithi ezinkulu ngexesha lasekuseni nangokuhlwa kakhulu. Kwezi ndawo, ukukhanya, ukusasazeka, kunye nokuna kwemvula ngamanye amaxesha kunokwenzeka, ingakumbi kwiindawo eziphakathi ezijikeleze umoya.
Kwiindawo eziphakamileyo, amaxesha esibhakabhaka esicacileyo aya kutshintshana amaxesha athile amafu aphezuluIngakumbi emva kwemini, nto leyo eya kwenza isibhakabhaka sibe nolusu olumnyama kancinci. Ukubakho kolusu olumnyama kumanqanaba aphezulu naphakathi kuya kuyiqinisa le mvakalelo yemozulu emhlophe okanye etyheli.
Umoya uya kuba yenye into ebalulekileyo: Imimoya yorhwebo yasempuma-mpuma iya kuba phambili Kwiindawo ezisezantsi, ngokubanzi ngamandla aphakathi kodwa ngamaxesha emvula enamandla kwiindawo ezisemazantsi-mpuma nakumantla-ntshona eziqithi, apho iziphepho zingenakuthintelwa khona. kwiindawo zokuhlala ezinamandla kakhuluingakumbi ngamaxesha okugqibela emini.
Embindini umoya uya kuba mncinci, uvela empuma, ngelixa ezincotsheni kukho ukuhamba kwamanzi. inxalenye esemazantsi eya kuthanda ukufumana amandlaKulindeleke ukuba kubekho imimoya ephakathi ephuma kumzantsi-ntshona kwiindawo ezisemantla eTenerife, apho kukho imimoya enamandla ngamanye amaxesha kwaye kubekho imimoya enamandla kakhulu phakathi emini. Imimoya yolwandle iya kuhlala ixhaphakile kwiziqithi eziphakamileyo kumzantsi-ntshona.
Elwandle, i-AEMET iqikelela imeko ulwandle olulwayo ukuya kulwandle olunamandlaXa umoya wasemntla-mpuma unamandla angama-5 okanye ama-6, ngamanye amaxesha angama-7 elunxwemeni. Ukuphakama okusemantla kuya kuvelisa amaza afikelela kwiimitha ezimbini ukuphakama, kwaye kwiphondo lasentshona, amaza afikelela kwiimitha ezintathu anokufikelelwa ekupheleni kosuku njengoko ukunyuka kutshintshela emantla-ntshona.
Imeko yesiqithi ngesiqithi: inkungu, amaqondo obushushu kunye nomoya
ELanzarote, kukho isibhakabhaka esicacileyo kakhuluKulindeleke ukuba kubekho amafu emantla kusasa nangokuhlwa kakhulu. Ubushushu buya kuba kukhanya kwiindawo eziphakamileyo, kunye nobushushu obuphezulu obunyukayo kunye notshintsho oluncinci kubushushu obuphantsi. E-Arrecife, amaqondo obushushu aphantsi kulindeleke ukuba abe malunga ne-16°C kwaye amaqondo obushushu aphezulu ajikeleze i-26°C, kunye nemimoya ephakathi yasempuma-mpuma kunye nemimoya yorhwebo enamandla kancinci kwisiqingatha esisezantsi ngamanye amaxesha.
I-Fuerteventura iza kubonisa imeko efanayo: Isibhakabhaka esinamafu kancinci kunye namaxesha athile Kumantla nasentshona, kulindeleke inkungu ekhanyayo kwiindawo eziphakamileyo ngexesha lasekuseni nangokuhlwa kakhulu, kunye nobushushu obuphezulu obunyukayo. Imimoya yasempuma-mpuma iya kuba phakathi, kunye nomoya onamandla onokuthi uvuthe phezu kweJandía peninsula ngokuhlwa kakhulu. EPuerto del Rosario, amaqondo obushushu aya kuba malunga ne-15-25°C.
EGran Canaria, imozulu iya kulawulwa isibhakabhaka esinamafu okanye esicacileyoNgaphandle kwasemantla ngaphantsi kweemitha ezingama-600-800, apho kunokubakho amafu aphantsi kunye nokukhanya okuncinci, okunemvula ngamanye amaxesha kusasa. Ubushushu buya kuba bukhulu ekuqaleni kwiindawo eziphakamileyo, kodwa bunokuba bukhulu kamva emini. Amaqondo obushushu aphezulu aya kunyuka kancinci elunxwemeni kwaye aphakathi kwiindawo eziphakathi nakwiincopho, kunye namaqondo obushushu amancinci angatshintshiyo okanye aphakame kancinci kwiindawo eziphakathi ezisezantsi. Imimoya yorhwebo iya kuba phakathi, kunye neemvuthuvuthu ezinamandla kumzantsi-mpuma nakumntla-ntshona kwaye iimvuthuvuthu ezinamandla kakhulu kwindawo ebonakalayo.
ETenerife, kulindeleke oku kulandelayo: isibhakabhaka esicacileyo kakhuluAmafu aza kuba makhulu emantla ngaphantsi kweemitha ezingama-900-1.100 ngexesha lesiqingatha sokuqala sosuku kwaye kwakhona ekupheleni kosuku. Iimvula ezikhaphukhaphu nezizimeleyo zinokwenzeka kwiindawo eziphakathi emantla kusasa. Ubushushu buza kuhlala njengomaleko wokukhanya kwiindawo eziphakamileyo kwiindawo eziphezulu ngeeyure zokugqibela. Amaqondo obushushu aza kunyuka kancinci elunxwemeni kwaye aphakathi kwiindawo eziphakathi nakwiincopho, apho kunokwenzeka ukuba kubekho ukunyuka okukhulu kwiindawo eziphakamileyo.
ILa Gomera iza kubonisa umfanekiso ocacileyo Isibhakabhaka esinamafu kancinci kunye namaxesha athile Kulindeleke amafu aphezulu emva kwemini, kunye namafu emantla kusasa nangokuhlwa kakhulu. Kunokwenzeka ukuba kubekho ukuna kwemvula okuncinci nokungahambelaniyo kwiindawo eziphakathi emantla kusasa kakhulu. Inkungu encinci inokwenzeka kwiindawo eziphakamileyo ngokuhlwa kakhulu. Imimoya yasempuma iya kuba phakathi, kunye nomoya onamandla wasekuhlaleni kumzantsi-mpuma nasentshona, ngelixa umoya uya kuba namandla kumzantsi-ntshona.
ELa Palma, emantla nasempuma yesiqithi kuya kuba Isibhakabhaka esinamafu ngakumbi kunye nethuba lokuna kwemvula Kulindeleke ukukhanya kunye nemvula ngamanye amaxesha kwiindawo eziphakathi kokuphakama, ingakumbi kwisiqingatha sokuqala sosuku. Kwezinye iindawo, isibhakabhaka siya kuba sicacile kakhulu, kunye namafu aphezulu emva kwemini. Inkungu encinci inokwenzeka kwiincopho emva kwemini. Imimoya yasempuma iya kuba phakathi, kunye nomoya onamandla kwiindawo ezisezantsi-mpuma kunye nemathambeka asentshona-ntshona, kunye nemimoya ekhanyayo entshona.
Kwi-El Hierro, iimpawu eziphambili ziya kuba isibhakabhaka ngokuyinxenye Kulindeleke ukuba kubekho amafu emantla ngexesha leeyure zasekuseni, apho kunokwenzeka ukuba kubekho imvula ekhanyayo neyodwa kwiindawo eziphakathi. Inkungu ekhanyayo inokwenzeka kwiindawo eziphakamileyo ekupheleni kosuku. Imimoya yorhwebo iya kuba phakathi, kunye neemvuthuvuthu ezinamandla kumazantsi-mpuma nakwiindawo ezikude ezikumntla-ntshona, kunye nemimoya entshona. IValverde iya kufumana amanye amaqondo obushushu apholileyo kakhulu kwiziqithi, kunye nobushushu obuphantsi obumalunga ne-11°C kunye nobushushu obuphezulu obumalunga ne-15°C.
Impembelelo kwimpilo kunye neengcebiso
Ubukho be ubuninzi bothuli oluxhonyiweyo Inokubachaphazela kakhulu abantu abasengozini enkulu, ingakumbi abantu abaneengxaki zokuphefumla, abantu abadala, kunye nabantwana. Ngexesha lobushushu obukhulu, kuqhelekile ukuba ukudinwa kunyuke xa uzilolonga kwaye iingxaki ezifana ne-asthma okanye i-bronchitis zibe mandundu.
Abasemagunyeni kunye neenkonzo zemozulu bacebisa, ngexesha leeyure zothuli oluphezulu, ukunciphisa umsebenzi womzimba onzima wangaphandleGcina iingcango neefestile zivaliwe kakuhle kwiindawo ezichaphazelekileyo kwaye uhlale unamanzi aneleyo. Kwimeko yokungakhululeki okukhulu kokuphefumla, kuyacetyiswa ukuba ubonane neengcali zempilo.
Kwabo bachitha ixesha elininzi ngaphandle, oku kunokuba luncedo. sebenzisa iimaski ezifanelekileyo ezihluza ezinye zeengceba ezinkulu, nangona isiphumo singesosiso esipheleleyo. Kukwacetyiswa ukuba kuphetshwe ukuhamba ngokungeyomfuneko ezindleleni apho ukubonakala kunciphisa khona uthuli, ingakumbi ngexesha lokukhanya okuphantsi.
Kumacandelo afana nezolimo, ulwakhiwo, okanye ukhenketho olunomdla, olu hlobo lweziganeko lusinyanzela ukuba lungisa iishedyuli kunye namanyathelo okukhuselaukubeka phambili umsebenzi kwiindawo ezinothuli oluphantsi kunye nokuqinisa ukusetyenziswa kweeglasi zokukhusela ukuphefumla xa kuyimfuneko.
Ulwandle olurhabaxa kunye nemisebenzi yangaphandle
Umoya ovela emantla-mpuma kunye nokuvuthuza okuvela emantla kuya kudala ezinye Iintsuku ezinzima kwimisebenzi yokuzonwabisa yaselwandleUkudibana kwamaza arhabaxa okanye anzima kunye namaza anokufikelela kwiimitha ezimbini okanye ezintathu kwenza kube lula ukuthatha amanyathelo okhuseleko aqatha xa uhamba ngeenqanawa ezincinci, usenza imidlalo yasemanzini kwaye udada kwiindawo ezivulekileyo.
Kumanxweme achaphazeleka kakhulu ziinduli ezisemantla nakumantla-ntshona, kuyacetyiswa ukuba musa ukusondela kakhulu kwiindawo zokusefa Nokuba kwiindawo apho amaza anokufikelela khona kwiindawo ezihambahambayo, ematyeni, okanye kwiindawo ezithintela amanzi. Amandla olwandle, kunye nomoya onamandla, anokudala iimeko eziyingozi nakubantu abanamava.
Emhlabeni, imimoya enamandla elindelekileyo kwiincopho nakwiindawo ezithe tyaba ezivulekileyo yenza kube luncedo cwangcisa imisebenzi yasezintabeni ngononopheloUkuhamba ngeenyawo, ukukhwela ibhayisekile ezintabeni, okanye ukukhempisha kunokuchaphazeleka ziimpepho ezinamandla, uthuli emoyeni, kunye nokungabonakali kakuhle, ngoko ke kuyacetyiswa ukuba ujonge uqikelelo oluhlaziyiweyo kwaye ucinge ngeendlela ezahlukeneyo okanye utshintsho kwishedyuli.
Le meko yemozulu, enomoya omninzi, ubushushu, yinxalenye yendlela eqheleke kakhulu kwiziqithi: ukutshintshana kwezivuthuvuthu zeAtlantiki kunye nokungena komoya eSahara eziguqula imbonakalo yesibhakabhaka kunye nobushushu obubonwayo kwiintsuku ezimbalwa nje. Kule siqendu, imihla ezayo iya kuphawulwa zisibhakabhaka ezicacileyo, amaqondo obushushu aphezulu ngaphakathi elizweni, ulwandle olurhabaxa, kunye nomoya omdaka ngenxa yothuli olumiyo, nto leyo efuna amanyathelo okhuseleko olongezelelweyo elunxwemeni nakwiintaba.
