ISpain iye yahlaselwa sisaqhwithi Ifilimu ukuba ilayishwe ngumoya ofumileyo ovela emazantsi kwaye ikhe yahlangana nongqameko lomoya obandayo osuswe kwindawo yeArctic. Ukungqubana kobunzima bomoya kuvelise ikhephu kwimbali yoSingasiqithi weIberia.
Kweli nqaku siza kukuxelela yonke into ngesishwankathelo malunga noqikelelo, oonobangela kunye neziphumo zesaqhwithi Filomena.
Uqikelelo lwesaqhwithi Filomena
Iisathelayithi zemozulu sele ziyazi ngaphambili intshukumo yemikhosi yomoya evela emazantsi nasemantla. Xa isixa esikhulu somoya owomileyo nobandayo sihlangana nomoya ofudumeleyo nofumileyo, isaqhwithi siveliswa ngumahluko phakathi koxinzelelo. Ukwehla koxinzelelo kuvelise ikhephu elinomtsalane kulo lonke usingasiqithi. Ikhephu liwele kwiindawo ezinendawo ephantsi kakhulu apho kuhlala kungekho mvula. Ukusukela ngoku ukuya phambili kukwakho neentsuku ezizayo kunye nomphambili omtsha we-polar enamaqondo asezantsi ashushu enza ukuba ikhephu liqhume kwaye lihlale iintsuku.
Siye sanamava ngeempelaveki ngekhephu eliwa njengaleyo ingazange ibonwe ngaphambili kwimbali yaseSpain. Yatsho ikhephu beze kuthintela isixeko saseMadrid kunye nezinye iingqukuva zephondo ezishiya ingubo enomkhenkce egubungele phantse yonke le ndawo. Olu hlobo lwesaqhwithi luvelise imeko engxamisekileyo ngenxa yokunqongophala kokuhamba kumaziko asezidolophini. Uqikelelo lwe-Arhente yeMeteorological kaRhulumente lubonakalise ukuba kukho uthotho lweemeko ezijike isaqhwithi sasePhilomena saba sisaqhwithi.
Ukuwa kwekhephu kunye neqabaka
Uqhwithela olusemazantsi lulayishwe yimvula ebinamava kwiintsuku ezimbalwa kwaye yanikezela ithuba apho isibhakabhaka sicacile kodwa ngamaqondo obushushu asezantsi kakhulu, ayisiyompembelelo eyenza imvula ngaphambili ime, Endaweni yoko, sisiganeko esingaphandle kwesiphango. Le meko yokusingqongileyo inxulumene ngokugqibeleleyo nesiqhwithi iFilomena ukuze ikwazi ukuguqula Spain kwindawo yekhephu okwethutyana. Ndiyabulela kwezi meko zemozulu kusenokwenzeka ukugcina iimeko eziyimfuneko ukuze ikhephu libambe iintsuku.
Emva kwekhephu elingaqhelekanga elenzeka ekupheleni kwexesha elidlulileyo, kuye kwafika iliza elibandayo eliphawule amaqondo obushushu angaphantsi kweedigri ezili-10 kwiindawo ezininzi. E-Madrid amaqondo obushushu we -10 degrees afikelelwe. La maxabiso awazange abonwe ukusukela nge-16 kaJanuwari, 1945 xa amaqondo obushushu afikelela kwi -11 degrees. Ubusika obunamandla kunye nemozulu ebandayo yasemini zikuthandile ukuqhubeka kwekhephu kunye nokugubungela umkhenkce kwiindawo ezininzi evekini.
Kwaye kukho isambuku esipheleleyo sezinto ezenze ukuba ikhephu lihlale iveki yonke. Makhe sibone ukuba zeziphi ezi zinto:
- I-anticyclone irhuqa imilambo ye-pole yasemantla isiya kwi-peninsula. Le anticyclone inoxanduva lokushiya isibhakabhaka sicacile, umoya uphantse wancitshiswa ngokupheleleyo kunye nemozulu ebandayo yasemini ngamaqondo obushushu asondela kwi-0 degrees.
- Ixesha elide lobusuku bexesha. Njengoko sisazi, ubusuku basebusika bude kunehlobo kwaye kuthanda ukuba namaqondo asezantsi asezantsi ngakumbi ngenxa yokunqongophala kwemitha yelanga. Ngala maqondo obushushu asezantsi umhlaba upholile ngamandla.
- Ikhephu elisandul 'ukuwa libonisa ilanga. Enkosi kwinto yokuba ikhephu liyakwazi ukubonakalisa ukukhanya kwelanga, lithintela umhlaba ukuba ubashushu ngokulula kwaye liphucula isiphumo esaziwa njengempembelelo yefriji. Ngesi sizathu, iziphumo zokuwa kwekhephu eziziswe sisaqhwithi iFilomena ziya kubonakala de kube phakathi okanye ukuphela kukaJanuwari.
Izinto ezibangela uqhwithela Filomena
Makhe sibone ukuba zeziphi izizathu zokuwa kwekhephu. Kufuneka sazi ukuba isaqhwithi asingoxanduva lwayo yonke into eyenzekileyo, nokuba kunganjani na. IFilmena ibe sisiqhwithi esikwiGulf of Cádiz ethe yavuthuza umoya ofumileyo usingise usingasiqithi. Iphambi kwesiqhelo sokubangela iintlobo ezahlukeneyo zemvula eninzi emazantsi nasempuma. Eyona inokubonakala ngemvula enkulu eMalaga apho imilambo iphuphume khona kwaye yabangela ukuphulukana nobomi babantu.
Into eyenzekileyo ngeli xesha kukuba iFilomena itsale ukufuma okuvela emazantsi kunye ne-anticyclone esuka eAtlantiki isiya e-United Kingdom ebichaphazela umoya obandayo oya kwilizwe lethu kangangeveki. Xa umoya obandayo udibene nomhlaba oneqondo lobushushu obuphantsi kwindlela yawo, uye wajika imvula esaqhutywa sisaqhwithi saba likhephu. Omnye wemibuzo oveliswe ziingcali kwimozulu kukuba konke oku kunxulumene notshintsho lwemozulu. Abaninzi bayazibuza ukuba kungabanda na oku xa umhlaba ushushu.
Utshintsho lwemozulu
Kuya kufuneka uqonde ukuba utshintsho lwemozulu lunzima kakhulu. Nangona utyekelo kukunyusa iqondo lobushushu lehlabathi, imozulu ayiphenduli ngendlela efanelekileyo. Oko kukuthi, imeko yexesha elide kwiindawo ezinkulu zobushushu xa amaqondo obushushu eza kunyuka. Siyazi ukuba iatmosfera yoMhlaba iyafudumala kwaye yinyani yesayensi ebingqinisisiwe. Konke oku kwazisa amandla amaninzi kwinkqubo enamandla ngokupheleleyo kwaye amandla ayo ashiyekileyo abangele imeko engalindelekanga kwaye inamandla ngakumbi nangakumbi okubangela iziphumo ezinamandla zasekuhlaleni.
Kwangelo xesha, njengoko amaqondo obushushu aphakathi komhlaba enyuka, ebizwa ngokuba yipolar jet itshintshiwe. Ngumoya wangoku owenzeka kwi-stratosphere kwaye unceda ukwahlula imimandla esecaleni kweendawo ezifudumeleyo. Kwiminyaka yakutshanje, lo mqobo uyatshintsha kwaye siza kubona ukuphazamiseka kwendawo yomoya yeArctic kwindawo yeJograins Peninsula.
Ndiyathemba ukuba olu lwazi ungafunda ngakumbi ngesiqhwithi Filomena kunye neempawu zayo.