Tawagar Hukumar Kula da Yanayi ta Jihar (Aemet) a cikin al'ummar Valencian ta sanar da cewa a wannan Asabar, ban da matsanancin zafi da ake tsammanin, "al'amura masu tayar da hankali" na iya faruwa tare da "ƙarfi mai ƙarfi" na iska ko "dumi mai zafi" irin waɗannan. da aka yi a cikin wayewar gari, lokacin da guguwar iska mai ƙarfi ta haifar da rugujewar mataki na bikin Medusa a Cullera (Valencia) kuma ya yi sanadiyar mutuwar mutum ɗaya da jikkata 17 na digiri daban-daban.
A wannan Asabar akwai jan gargadi ga daukacin gabar tekun lardin Valencia da kuma kudancin Alicante da kuma gargadi ga guguwa da ka iya barin guguwar iska mai karfi.
Kamar yadda Aemet ya bayyana, a cikin dare an yi "fitowa mai dumi" tare da gusts na "iska mai karfi da kuma tashin hankali a zazzabi", mai yiwuwa na abin da ake kira "convective".
Masu kashe gobara suna gudanar da ayyukan dare 60
Sakamakon guguwar iskar, daga karfe 2:00 na safe ma'aikatan kashe gobara sun kai dauki har sau 60 saboda iska mai karfi a duk fadin lardin Alicante da ke da alaka da fadowa ko kauce musu, na bishiyoyi, eriya, alamun zirga-zirga, pergolas. , rumfa, da sauransu. Yankunan da al'ummar kudancin kasar suka fi shafa musamman a Santa Pola, Elche da Orihuela, a cewar kungiyar hadin kan lardin Alicante.
A cikin wani zare da aka yi ta shafin Twitter, hukumar Aemet ta bayyana cewa, da sanyin dare an samu guguwa a Albacete da yankin Murcia da ke tafiya gabas, inda suka fara isa gabar tekun Alicante da misalin karfe 2.00:XNUMX na safe kuma bayan sa'o'i biyu daga Valencia.
Guguwar tana da hazo da wasu walƙiya a ciki amma, yayin da suka tunkari bakin tekun, ruwan sama ya watse kuma da ƙyar ba a sami wata walƙiya ba. A gaskiya ma, a bakin teku mai yiwuwa ba a yi ruwan sama ba ko kuma an yi ruwan sama.
Sabanin yanayin zafi da zafi
Aemet yayi cikakken bayani game da wannan al'amari da kuma dalilin da yasa yake faruwa: bayanan sararin samaniya da ke haifar da fashewar zafi "duk suna kama da juna". "An ce binciken nasa nau'in albasa ne, mai damshi, iska mai sanyi kusa da kasa da kuma busasshe mai tsananin zafi da ke da 'yan mita dari a sama." Game da filin jirgin sama na Alicante-Elche, bayan wayewar gari, wannan al'amari ya wuce digiri 40 da gust na 80 km / h.
Lalacewar zuwa ga Alcoy ALICANTE FIREFIGHTER CONSORTIUM
Sauran ruwan jika, wanda zai zama gindin gajimaren, ya kasance "mai tsayi sosai", a tsayin sama da kilomita 5, wanda ya cika tsakanin mita 5.800 zuwa 6.500 na tsayi. Don haka gindin gajimaren yana da tsayi sosai kuma a karkashinsa akwai busasshen busasshen busasshen da ya wuce kilomita hudu.
Hazo da ke faruwa a gindin girgijen, wanda yake da tsayi sosai, yana ƙafewa a cikin ƙananan ƙananan Layer; lokacin fitar da iska yana yin sanyi kuma ya zama mai yawa fiye da kewaye; yayin da ya yi yawa sai ya fara saukowa da sauri.
Ana samar da ƙaƙƙarfan saukar da ruwa ta musamman ta hanyar ƙazantar ruwa da narkewa da ƙanƙarar ƙanƙara a ƙarƙashin tushen girgije. Don haka ya bayyana cewa, a gabar tekun ba a yi ruwan sama ba, ko kuma an yi haske sosai, domin ruwan sama ya yi tururi tun kafin ya isa kasa, kuma wannan iska ya sanya iska ya sanyaya, wanda shi ne abin da ke gangarowa ya kuma haifar da busa.
Tare da iska mai saukowa, a cikin wannan gangaren yana "hanzari" kuma, idan babu jujjuyawar thermal, ya bugi ƙasa yana haifar da gusts mai ƙarfi, amma zafin jiki ba ya tashi. Wannan busasshiyar busa ce, wacce ta faru a Xàtiva, alal misali, tare da gusts na 84 km/h.
Amma idan, a gefe guda, akwai jujjuyawar kusa da ƙasa (yanki mai laushi da ɗanɗano), a kan saukowarsa iska na iya wucewa ta cikin sabon Layer, yana haifar da kutsawar iska mai dumi daga sama. A cikin yankin da yankin na zuriya ya kasance saboda jujjuyawar, haɓakar zafin jiki mai tsanani yana faruwa kuma, ba shakka, tsarin ka'idar yana hasashen yanayin zafi na akalla digiri 40, kamar yadda ya faru.
Ketare layin danshi a haƙiƙanin “birki” ne ga iskar da ke gangarowa daga sama sama da kilomita 5, amma idan juyarwar ta yi ƙasa sosai, kamar yadda yake a safiyar yau, “gudun ya isa ya haye shi ya isa ƙasa. tare da saurin gudu.
Wannan busa ya yadu sosai, a wasu lokutan kuma ba a samu hayaniya mai karfi ba, domin jujjuyawar tana da yawa sosai kuma iskar tana isa kasa sannu a hankali, wasu kuma jujjuyawar ba ta karye ba amma yanayin zafi ya tashi saboda matsewar mafi karanci. stratum . A cikin mafi munin yanayi, guguwar iska mai ƙarfi da ƙaruwar zafin jiki kwatsam sun faru a cikin gida a wasu yankuna saboda wannan fashewar zafi.
