Xa imozulu ishushu size sicinge ngeeholide zangaphandle, iintaba ziba yindawo esiyithandayo. iziqendu zotshintsho olukhulu lwemozulu Zingasikhumbuza ukuba iintsuku ezishushu kunye neemvula zasemva kwemini ezintabeni zinokubamba nabani na ongalindelanga ngequbuliso. Isibhakabhaka esicacileyo ekuzeni kokusa, amaqondo obushushu aphantsi, umoya omanzi kancinci emini, uze ngequbuliso, kubekho amafu amnyama, iimvula ezinkulu, kwanezichotho kwimizuzu embalwa.
Kule meko, ukuqonda indlela umoya osebenza ngayo kubalulekile. Usuku olunye lunokutshintsha ukusuka ekubeni yinto ezinzileyo ukuya ekubeni yinto engazinzile kakhulu kwiiyure ezimbalwa nje.Ngenxa yotshintsho olukhawulezileyo lobushushu, ukubonakala okunciphileyo ngenxa yokugquma kwamafu aphantsi, umoya ovuthuzayo ngequbuliso, kunye nemvula eqokelelene kwisiqingatha sesibini sosuku. Ngaphezu koko, ubushushu kwiindawo ezininzi zaseSpain abukabi bukhulu kangako, kunye namaqondo obushushu anyukayo nawahlayo imihla ngemihla, ingakumbi xa kusetyenziswa imisele kunye ne-DANA (uxinzelelo oluzimeleyo kumanqanaba aphezulu).
Ipateni ngokubanzi: iintsuku ezizinzileyo, kodwa ngeziganeko ezingalindelekanga emva kwemini
Kwiimeko ezininzi eziqhelekileyo ekupheleni kwentwasahlobo nasekuqaleni kwehlobo, Sishiya ngasemva iziqendu zemvula enamandla size sifudukele kwindawo ezinzileyo ngokubanzi.Oku akuthethi ukuba isibhakabhaka sicacile ngokupheleleyo, kodwa kuthetha ukuba uninzi lwelizwe lunandipha iintsuku ezingenamvula. Nangona kunjalo, umoya uhlala ushukuma, kwaye iintaba zihlala ziyindawo efanelekileyo yokuzalela iimvula ezinkulu ukususela emini ukuya phambili.
Ngezi ntsuku kuqhelekile ukuba inkqubo yomgxobhozo kunye neyangaphambili Kwindawo ephakamileyo, ihamba emva kweentsalela zomphezulu obandayo. Lo msele udlula isiqithi kwaye usebenza njengentlantsi yokuvuselela iimvula kunye neziphepho.Oku kuyinyani ngakumbi kwiindawo apho umhlaba uvumela ukunyuka komoya ofudumeleyo nofumileyo. Ngoko ke, nangona uqikelelo ngokubanzi luxela kwangaphambili imozulu ezinzileyo, iindawo zeentaba zinokubona amafu akhula ngokuthe nkqo kunye neemvula ezinkulu zasekuhlaleni.
Kwimeko yaseSpain, le meko idla ngokuguqulelwa ekubeni Iindudumo zasemva kwemini kumantla eCatalonia, ngaphakathi kweValencian Community, eMurcia nasempuma yeAndalusiaEzi ziindawo apho umoya wolwandle uzisa umswakama, ilanga lifudumeza umphezulu kangangeeyure, kwaye imbonakalo yomhlaba inceda umoya ukuba unyuke ngokulula. Olu dibaniso lufanelekile ukuba kubekho iziphepho ukususela emva kwemini, zihlala zihamba nombane nesichotho, njengoko ezinye iingcaphephe zibonisa. Iimvula nezivuthuvuthu eSpain.
Nangona ezi zivuthuvuthu zixhaphakile, impelaveki ingathathwa njengezolileyo xa ujonga ilizwe liphela. Akulindelekanga ukuba imvula eninzi iqokelelekekodwa kukho iimvula ezingaqhelekanga nezizimeleyo. Iimephu zemvula zihlala zibonisa ubungakanani obuncinci, obuxineneyo kwiindawo ezithile zeentaba kwaye, ngamanye amaxesha, kwiziqithi zeMeditera neBalearic. Kwiimeko ezininzi, Imozulu iyatshintsha eSpain. ukusuka kolunye usuku ukuya kolunye, kunye namaxesha okungazinzi nokuzola atshintshatshintshanayo.
Emva kokuba umkhombe udlulile, imeko iyatshintsha kwakhona. Imozulu ithambekele ekuzinzeni ngosuku olulandelayoUsuku luya kuba luzolile kwiindawo ezininzi. Nangona kunjalo, ezinye iimvula zasekuseni zinokwenzeka kwiZiqithi zaseBalearic, kwaye kulindeleke imvula eninzi eGalicia ngenxa yokusondela kweAtlantiki. Kwakhona, ezi mvula zihlala ziphakathi kwaye azinazo naziphi na iziganeko ezinkulu. Ngamanye amaxesha, ukuzinza kuhamba kunye ne- i-anticyclone emva kwesiganeko sasebusika nto leyo ekhokelela kwiintsuku ezizolileyo.
Iyiphi indima edlalwa ziiTrows kunye neeDANA kwizaqhwithi zasemva kwemini?
Ukuze uqonde isizathu sokuba unokuba noMgqibelo oneziphepho ezintabeni kunye neCawa ezolileyo ngempelaveki enye, kuya kufuneka ujonge indlela ezitshintsha ngayo izinto xa unyuka. Iimbiza zizinto ezibangela umoya obandayo kumanqanaba aphakathi naphezulu omoya ojikeleze umhlaba. ezirhubuluza phezu kwesiqithi emva kokudlula kwemida okanye ezinye iinkqubo zemozulu. Ngokungenisa umoya obandayo kwindawo ethile ephakamileyo, zonyusa ukungazinzi kwaye zenze kube lula ukuphuhliswa kwamafu esiphepho ngamandla amakhulu.
Ngeentsuku ezinesitya sokuhlambela, umoya okufutshane nomphezulu ufudumele kwaye ufumile, ngelixa ulwimi lomoya obandayo lungena kwiikhilomitha ezimbalwa ngaphezulu. Olu tshintsho lobushushu oluthe nkqo lubangela ukuba umoya oshushu nofumileyo ongaphantsi unyuke ngokukhawuleza.ivelisa amafu ophuhliso olukhulu oluthe nkqo oludla ngokukhupha iimvula ezinkulu, iindudumo, kwaye ngamanye amaxesha, isichotho.
Ukongeza kwiimbiza, I-DANA (Isolated Depressions at High Levels) ngomnye umdlali obalulekileyo Ngexesha leemvula zasemva kwemini ezintabeni, xa i-DANA (isolated high-altitude depression) izimisa kufutshane ne-Iberian Peninsula, inokuzisa iintsuku ezininzi ezilandelelanayo zeemeko ezipholileyo kunesiqhelo, isibhakabhaka esitshintshayo, kunye neemvula ezisasazekileyo, ngakumbi kwiindawo ezineentaba nezingaphakathi. Oku kubangela amaqondo obushushu angaphantsi kwesiqhelo, imeko enxulunyaniswa... uqikelelo lwentwasahlobo kunye nemikhwa yayo yokungazinzi.
Xa i-DANA (i-isolated depression ekwizinga eliphezulu) okanye isitya sidityaniswe nelanga elinamandla eliqheleke phakathi kuJuni, Ukungazinzi kuyanda phakathi kweeyure eziphakathi zosukuIntsasa ingaqala ngamafu aphantsi, inkungu kunye nesibhakabhaka esicacileyo; emini ilanga lifudumeza umphezulu, ukujikeleza kwamanzi kuyanda, emva kwemini, kuqhambuke izivuthuvuthu, ingakumbi kwiintaba nakwiinduli.
Le ndlela ithetha ukuba, nangona uqikelelo ngokubanzi luthetha ngexesha elizinzileyo, abo bangena ezintabeni kufuneka bajonge esibhakabhakeni baze bajonge ezinye izilumkiso zemozulu. Iindudumo zeentaba ezisakhulayo emini zinokukhula ngokukhawuleza, ingakumbi kwisiqingatha sesibini sosuku kwaye kukho uphawu lwendawo oluphawulweyo, nto leyo ngamanye amaxesha eyenza kube nzima ukulungisa uqikelelo oluchanekileyo lwentlambo nganye okanye incopho.
Amaqondo obushushu: i-thermal roller coaster yokwenyani
Ngaphaya kwemvula, enye into ephawulekayo kwezi ziqendu kukuguquguquka kwee-thermometers. Ukudlula komkhombe kudla ngokubangela ukwehla okuphantse kube ngokubanzi kumaqondo obushushu aphezulu.Ingakumbi ngemini apho umoya obandayo uphezulu unamandla kakhulu. Oku kubonakala ngakumbi kwiindawo ezifana nempuma yeCantabria, i-Ebro Valley, emantla eCatalonia, kunye nonxweme lweValencian Community, apho amaqondo obushushu aphezulu anokwehla ukuya kuthi ga kwi-10°C ukusuka kolunye usuku ukuya kolunye.
Emva koko kudilika, Kwiimeko ezininzi, usuku olulandelayo luphinda lufudumale. Kwinxalenye enkulu yelizwe, amaqondo obushushu abuyela kumanqanaba aqhelekileyo okanye ade adlule. Okwangoku, imimandla yeMeditera isenokuphinda ifumane ukwehla okuncinci, okuchatshazelwa lifu, umoya ovuthuzayo wolwandle, kunye nobukho bomoya opholileyo kufutshane nonxweme.
Kwiimeko ezinjalo, ubushushu abuyithathi kakuhle iSpain. Ziindawo ezithile kuphela, ezifana nentlambo yaseGuadalquivir, ezisondela kuma-35°C.Njengoko kulindeleke ukuba amaqondo obushushu afikelele malunga nama-34°C kwizixeko ezifana neCórdoba. Iindawo ezingaphakathi nezingakhuselekanga ziyaziva iziphumo zelanga ngokubonakalayo, ngelixa kwezinye iindawo amaqondo obushushu ehlala emnandi ngeli xesha lonyaka. Kwezinye iimeko, i-a Umoya ovuthuzayo ngobushushu nto leyo egxininisa utshintsho.
Kwi-peninsula esembindini, emazantsi nakwinxalenye enkulu yentlambo yase-Ebro, Amaqondo obushushu aphezulu amalunga nama-30°CNgeentsuku ezishushu kodwa ngaphandle koxinzelelo olukhulu. Ithafa elingasentla lidla ngokubona amaqondo obushushu aphakathi kwama-25°C nama-28°C, ngelixa kummandla waseCantabrian, amazinga aphezulu adla ngokuba shushu ngakumbi, aphakathi kwama-20°C nama-25°C. Kunxweme lonke lweMeditera nakwiziqithi zaseCanary, i-thermometer idla ngokujikeleza malunga nama-25°C, kunye nobushushu obuphakathi nobuhlala buhleli. Nangona kunjalo, ngamanye amaxesha inqanaba lemvula linokwehla kwaye lichaphazele neentaba, njengaxa Inqanaba lekhephu lehla ngaphantsi kweemitha ezili-1.000 kwiziqendu ezibandayo.
Xa bejonga ixesha elifutshane, abaninzi bayazibuza ukuba ubushushu behlobo buza kufika nini. Impendulo ayisoloko ilula, kuba Ubukho beziphepho ezintsha ze-DANA busenokuqhubeka nokugcina amaqondo obushushu engaphantsi kwesiqhelo. kangangeentsuku ezininzi. Kwezinye iimeko, kucetyiswa ukuba kude kube ngoLwesine weveki elandelayo ubushushu bunokuhlala bupholile ngeli xesha lonyaka kwiindawo ezininzi zelizwe, ngelixa iindudumo zasemini ziya kuqhubeka ziyinto ephambili ezintabeni.
Iimeko zesibhakabhaka, ukugquma kwamafu kunye nokubonakala ezintabeni
Ngeli xesha lobushushu obuphakathi kunye neziphepho zasemini, Imeko yesibhakabhaka ingatshintsha amaxesha amaninzi eminiKwiyure zokuqala, isibhakabhaka sidla ngokuba namafu amaninzi okanye sibe namafu amaninzi, ingakumbi xa kukho amafu amaninzi aphantsi. Esi sigqubuthelo samafu sinokunciphisa ukubonakala kwasekuhlaleni, okwenza kube nzima ukuhamba ezintabeni kwaye sifihle iincochoyi ezazibonakala ngokucacileyo kwiiyure ezimbalwa ngaphambili.
Njengoko kusasa kuqhubeka, amafu asezantsi anokunyuka, nto leyo enika ithuba lokuba kubekho amaxesha esibhakabhaka esicacileyo namafu aphakathi. Nangona kunjalo, Imo yezulu ayizinzanga kwaye ixhomekeke ekudalweni kwamafu amatsha akhula ngokuthe nkqo.Oku kuthetha ukuba usuku lunokunika ikhefu elifutshane ukusuka emafini, kodwa kungcono ukungakhathali, njengoko amafu edla ngokwanda emva kwemini, ingakumbi kwiintaba.
Kwisiqingatha sesibini sosuku, imeko eqhelekileyo kukwanda kwesigqubuthelo samafu, kunye nezakhiwo ezincinci nezimnyama ngakumbi. Kungale maxesha apho kulindeleke khona imvula enkulu kunye neemvula ezinkulu.Izivuthuvuthu, ezinokuba nzima kakhulu ezintabeni kwaye zikhatshwe sisichotho, ziyingozi kakhulu kwiindlela ezinamatye okanye kwiindawo ezinamatye agudileyo, njengoko zinyusa kakhulu umngcipheko wokutyibilika nokuwa.
Izivuthuvuthu ezihamba nale mvula zihlala zinamandla kakhulu ngokubhekiselele kumsebenzi wombane. Umbane yenye yezona ngozi zinkulu ezintabeni eziphakamileyoIngakumbi ukuba sibanjwe kwiinduli, iincopho ezivezwe elubala, okanye kwiindawo ezingenandawo yokukhosela ekufutshane. Ngaphezu koko, amakhethini emvula enkulu anokunciphisa ukubonakala okwexeshana ukuya kwiimitha ezimbalwa, okwenza kube nzima ukulandela iindlela okanye ukufumana iimpawu ezibalulekileyo kunye nezinye iimpawu.
Ngoko ke, nangona ingxelo ingachaza usuku "oluzinzileyo kakhulu", Xa ufuna ukunyuka intaba, kufuneka ufunde umzobo omncinci.Isibhakabhaka esinamafu amaninzi, amaxesha okugquma kwamafu aphantsi, kunye nokubonakala okuncinci ngamaxesha athile zizinto ezibalulekileyo xa ucwangcisa indlela, ukhetha ixesha lokuqala, kunye nokulindela iindawo zokubaleka xa isivuthuvuthu siqala ngokukhawuleza kunokuba bekulindelwe.
Imvula, ubunzulu kunye namathuba okuba kubekho iziphepho
Ngezi ntlobo zeentsuku, iimodeli zemozulu kunye neenkonzo zihlala zibonisa Imvula ethe kratya kwisiqingatha sesibini sosukuKulindeleke imvula kunye neemvula, nto leyo ethetha ukuba zingaba nkulu kakhulu kwiindawo ezithile kodwa zingasasazeki kulo lonke eli phondo. Kwabo basezintabeni, oku kuthetha ukuba intlambo ifumana imvula enkulu ngelixa, kwiikhilomitha ezimbalwa ukusuka apho, kukho amathontsi ambalwa kuphela.
Amathuba okuna kwemvula emini yonke adla ngokuba phezulu. Ngamaxesha amaninzi, Amaxabiso amalunga ne-80-90% yamathubaingakumbi emva kwemini. Ngamaxesha athile, uqikelelo lunokubonisa imvula encinci (umzekelo, 0,2 ukuya kwi-0,7 l/m²), ngelixa kwamanye, kulindeleke iimvula eziphakathi ukuya kwezinkulu, kunye nokuqokelelwa kwe-2 ukuya kwi-6 l/m² kwiiyure ezimbalwa nje. Kwiziqendu ezisebenza kakhulu, iirekhodi zinokudlulwa, njengoko kuboniswe kwizifundo malunga iirekhodi zemvula.
Umzekelo oqhelekileyo wexesha lasemini ngulo: ngentsimbi yesi-17:00 emva kwemini, amathuba emvula encinci angama-90% amalunga ne-1 l/m² kunye nobushushu obumalunga ne-13 °C; ngentsimbi yesi-18:00 emva kwemini, Imvula iyanda iye kuthi ga kwi-2,7 l/m² kwaye amathuba aphezulu afanayo kunye ne-12 °C; kwaye, njengoko imini iqhubeka, ubunzulu bunokwehla kancinci kancinci, nge-0,7 l/m² kwi-19:00 kunye nezixa eziphantsi kancinci ukusuka kwi-20:00 ukuya phambili, kusagcinwe amathuba angama-80-70% kwezinye iindawo.
Ukususela ebusuku, umoya ungazinza kancinci kancinci. Amathuba okuna kwemvula ancipha kancinci kancinciAmathuba emvula ehle ukusuka kwi-50% malunga ne-22:00 PM kunye nemvula encinci ye-0,2 l/m² kuphela, ukuya kwi-30% nge-23:00 PM kunye ne-0,3 l/m². Ezinzulwini zobusuku, kwiimeko ezininzi, uqikelelo sele lukhomba isibhakabhaka esinamafu, ngaphandle kwemvula enkulu kunye nobushushu obuqikelelwayo obusondeleyo kubushushu bokwenyani.
Xa kujongwa imvula eqokeleleneyo ixesha elide, iirekhodi zinokubonisa amaxabiso aguquguqukayo kakhulu. Kukho iimeko apho imvula yemihla ngemihla iyonke ingaphezulu kwama-20 mm (umzekelo, i-20,6 mm okanye i-23,8 mm kwiintsuku ezixakekileyo), ixutywe neentsuku ze-1,9 mm okanye i-2,9 mm kuphela, kunye nezinye ezinomlinganiselo ophakathi, njenge-5,3 mm okanye i-10,2 mm. Kuzo zonke, ikhephu lihlala kwi-0 cm, kuba ezi meko zenzeka kwimeko yamaqondo obushushu aphantsi.
Umoya, ukubanda komoya, kunye nezinye izinto ezibalulekileyo
Imimoya yasezintabeni yenye into ephambili edla ngokungaqatshelwa xa uqikelelo lwemozulu lujongwa ngokungakhathaliyo. Kwezi meko, Imimoya ephakathi esezantsi ixhaphakilengemimoya enamandla kwiindawo eziphakamileyo. Kamva, njengoko imini iqhubeka okanye utshintsho lwenzeka ngenxa yokuhamba komsele, umoya usenokutshintshela entshona emva kwemini, ulahlekelwe ngamandla kwezinye iindawo. Kubalulekile ukuthobela izilumkiso ezifana nokuba kunokwenzeka Isilumkiso esiorenji somoya kwiindawo ezivulekileyo.
Ngokukodwa, imimoya evuthuza ukusuka kwi-8 ukuya kwi-11 km/h idla ngokurekhodwa kwiiyure zasekuseni, kunye neemvuthuvuthu ezinokufikelela kwi-13 ukuya kwi-17 km/h. Emini yonke imimoya inokunyuka, ifikelele kwi-20 okanye kwi-30 km/h ngamaxesha athile.ingakumbi kwiindawo eziphakathi kweentaba nakwiincopho. Ngobusuku obuzolileyo, umoya ungahlala ujikeleze i-5 ukuya kwi-9 km/h, kunye nomoya ophakathi.
Amaqondo obushushu ngamaxesha abalulekileyo emini nawo abonakalisa imo epholileyo yomoya. Kwakusasa, umzekelo ngo-08:00, Akuqhelekanga ukufumana amaxabiso aphakathi kwe-4 °C kunye ne-9 °CUkuba nomoya obandayo kwenza kube ngathi kupholile ngeqondo elinye okanye amabini. Umswakama oqhelekileyo uhlala ujikeleze i-88-95%, nto leyo enegalelo ekugubungeni kwamafu aphantsi kunye nomoya ofumileyo nopholileyo.
Phakathi emini, malunga ne-14:00 PM, amaqondo obushushu anyuka aye kwi-10-15 °C kuxhomekeke kukuphakama, kunye neempawu zobushushu ezihlala zifana kakhulu nobushushu bokwenyani ukuba umoya awuvuthuzi ngamandla kakhulu. Isigqubuthelo selifu sinokuba phakathi kwama-64% nama-97%.Oku kubonisa isibhakabhaka esitshintshatshintshayo kakhulu, kunye namaxesha esibhakabhaka esicacileyo phakathi kwamafu kunye namanye amazulu aphantse agubungele.
Emva kwemini nangokuhlwa, malunga nentsimbi yesi-8:00 emva kwemini, amaqondo obushushu aphinda ehle aye kutsho kwi-20-14 °C, apho amaxabiso omoya aphantsi kancinci xa kukho umoya okanye imvula. Umswakama uphinde wanda ngaphezulu kwama-85-90%.nto leyo eyonyusa ukuziva ubanda xa simanzi, into exhaphakileyo emva kokuwela imvula endleleni.
Imitha ye-UV, ukusa, ukutshona kwelanga, kunye nesigaba senyanga
Enye into engafanele ingananzwa kule mihla ezintabeni yimitha yelanga. Nokuba isibhakabhaka sinamafu okanye sigubungele amafu, Amanqanaba emitha ye-UV adla ngokuba maphakathi.Kwiindawo ezininzi zokubeka ixesha, amaxabiso e-UV 3 okanye e-UV 4 avela, ahlelwa njengomngcipheko ophakathi, oko kuthetha ukuba ulusu lunokutsha ngexesha elifutshane kunokuba sicinga ukuba asisebenzisi ukhuseleko.
Ekuseni okanye emva kwemini, i-UV index yehla kakhulu, ide ifikelele kumaxabiso akufutshane ne-0 okanye i-1, ethathwa njengengozi ephantsi. Nangona kunjalo, kwimisebenzi yasezintabeni eyenzeka phakathi eminiKucetyiswa ukuba usebenzise i-sunscreen ene-factor ephezulu yokukhusela, i-cap okanye umnqwazi kunye nee-sunglasses ezifanelekileyo, njengoko ukuphakama kwandisa ukuvezwa kwimitha.
Ngokuphathelele amaxesha okuphuma kwelanga, idatha ibonisa ukuphuma kwelanga phakathi kwentsimbi ye-07:01 kunye nentsimbi ye-07:17, kunye nokushona kwelanga okulibazisekayo ukusuka kwintsimbi ye-21:31 ukuya malunga nentsimbi ye-21:46. Ezi ntsuku zinde zokukhanya kwelanga zivumela ukucwangcisa iindlela ezindeKodwa zikwathetha ukuba izivunguvungu ezininzi ziqala emva kwemini, xa kusekho usuku olude oluzayo kwaye kulula ukungabi naxhala xa kusacacile.
Ezi rekhodi zikhankanya nezigaba zenyanga ezifana I-Waning Gibbous, iKota yokugqibela kunye neNyanga eNcinciNangona inqanaba leNyanga lingachaphazeli ngqo ukwakheka kwezivuthuvuthu ezijikelezayo ezintabeni, lulwazi olusebenzayo kubantu abakhwela iintaba kunye nabafoti basebusuku, njengoko lumisela ubungakanani bokukhanya okufumanekayo ukuba umsebenzi uqhubeka ebusuku okanye wenziwa nge-bivouacking kwindawo ephakamileyo.
Ukudibana kokuphuma kwelanga kwangethuba, ukutshona kwelanga kade, kunye nemitha ye-UV ephakathi kwenza iintsuku zibe mnandi kakhulu, kodwa ikwafuna nolawulo olucokisekileyo lwamaxesha okuhamba nawokubuya. Kudla ngokuba kuhle ukuqala umsebenzi kwangethuba uze wehle kwiindawo eziphakamileyo ngaphambi kokuba kubekho izivunguvungu.Oku kwenzeka rhoqo kwezi meko ziqala malunga nemini kwaye ziqhubeke ngamandla emva kwemini.
Indlela yokwenza uqikelelo kunye nolwazi oza kulujongana nalo
Kuzo zonke ezi meko, iinkonzo zemozulu zibonelela ngolwazi oluninzi kumaphepha azo eengxelo zemozulu. Ulwazi lunikezelwa ngeendlela ezahlukeneyo ukuze kube lula ukubonisanaKwelinye icala, imephu esebenzisana nayo ikuvumela ukuba ukhethe izinto eziguquguqukayo zemozulu ezifana nobushushu, imvula, umoya okanye isigqubuthelo samafu; kwelinye icala, iitheyibhile zibandakanyiwe nezilumkiso zeziganeko ezimbi, imibhalo echazayo yesimo sezulu kunye noluhlu lwamaqondo obushushu aphantsi naphezulu koomasipala abafanelekileyo.
Olu lwazi lufumaneka kumanqanaba ahlukeneyo endawo: ISpain iyonke, uluntu oluzimeleyo okanye izixeko, kunye namaphondo okanye iziqithiNgale ndlela, umntu oya ezintabeni unokujonga zombini ingqikelelo ngokubanzi kunye neenkcukacha ezikufutshane, into ebalulekileyo xa ejongene nezivuthuvuthu ezixhomekeke kakhulu kumhlaba kunye neenguqu ezincinci zengingqi.
Enye ingongoma ebalulekileyo lulwalamano phakathi kwexesha lendawo kunye nedatha ebonisiweyo. Zonke izinto eziguquguqukayo ezikhawulezayo, ezifana nobushushu, isigqubuthelo samafu, okanye umoya, Ziboniswa ngexesha lendawo eliboniswe kumgca wexesha.Kwimeko yezinto eziguquguqukayo eziqokelelene ngaphezulu kweyure (umzekelo, imvula okanye umoya ovuthuzayo ophezulu), ixabiso eliboniswe kwixesha elithile lihambelana nesixa esirekhodiweyo ukususela kuloo yure ukuya kwelandelayo. Ngoko ke, ixabiso lemvula elirekhodiweyo ngo-09:00 libonisa isixa esiwe phakathi kwe-09:00 kunye ne-10:00.
Amaxesha okuphumla eeyure ezintandathu nangaphezulu adla ngokuboniswa ngexesha le-UTC, ngoko ke Kuya kufuneka wongeze iyure enye ebusika kunye nezimbini ehlotyeni Ukuze ufumane ixesha lasekuhlaleni eSpain. Le nkcukacha ibalulekile ukuze kuqondwe ngokuchanekileyo ukuba kuza kubakho nini isivuthuvuthu esibi, kuthintelwe ukudideka kweyure enye okanye ezimbini, ezinokuthi, ezintabeni, zenze umahluko phakathi kokuba namava amabi okanye ukubaleka isichotho.
Izibikezelo eziboniswe kwifomathi yemephu ziveliswa ngokuzenzekelayo, ngokuthe ngqo kwiimodeli zamanani. Nangona kunjalo, Imibhalo, izaziso ezisemthethweni, kunye neetafile zobushushu obuphantsi nobukhulu zilungiswa ngababikezeli bemozulu. Bayayihlalutya baze bayilungelelanise loo ngcaciso. Oku kuthetha ukuba, ngamanye amaxesha, kunokubakho umahluko omncinci phakathi koko imaphu ezenzekelayo ikubonisayo noko ingxelo elungiselelwe yingcali ikubonisayo, le yokugqibela iyindawo yokubhekisa xa kufikwa kukhuseleko lweentaba.
Xa ujonga uqikelelo lwendlela, kuyacetyiswa ukuba ujonge zombini umfanekiso kunye nombhalo, izilumkiso zeemeko zemozulu ezimbi kunye noqikelelo lweyure ngeyure. Idatha efana namathuba emvula, icala lomoya, isigqubuthelo samafu, kunye nobushushu obubonwayo Zisenza sikwazi ukuqikelela ngcono ukuba kulula na ukwazisa uhambo, ukufinyeza indlela, okanye ukuyihlehlisa ukuba imeko ayintle kakhulu.
Lilonke, iintsuku zobushushu obuphantsi kunye nezivuthuvuthu zasemini ezintabeni zidibanisa isibhakabhaka esitshintshayo, imvula eqina kwisiqingatha sesibini sosuku, imimoya ephakathi, kunye namaqondo obushushu anyukayo nawayo kunye nezivuthuvuthu zeDANA. Cwangcisa ngolwazi olufanelekileyo, lungisa amaxesha eeshedyuli, kwaye ungazithatheli phantsi iziphepho ze-orography. Yeyona ndlela ilungileyo yokonwabela iintaba ngeli xesha lonyaka ngaphandle kwezinto ezimangalisayo, usebenzisa ithuba lemozulu epholileyo kodwa ukhumbule ukuba, kwiiyure ezimbalwa, isibhakabhaka singatshintsha ukusuka ekuzoleni ukuya ekubeni sisebenze kakhulu.
