10 Abubuwan Ban Sha'awa About The science behind hurricanes and how they form
10 Abubuwan Ban Sha'awa About The science behind hurricanes and how they form
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An kafa guguwa na terphoons a kan teku mai dumama, inda yanayin teku yake kai aƙalla digiri 80 Fahrenheit.
Ruwan wurare masu zafi da aka kirkira a gabas da kudu-Kudancin Tekun Atlantika galibi suna da guguwa.
Tirlhooon Storm yana buƙatar tsayayye da ƙarancin -pressure ATMOSPHERHERACHER ADDU'A BUKATAR DA ZA KA SAMU.
Winds yana busawa daga fuskoki daban-daban a cikin manyan daban-daban na iya taimaka wa guguwa ta ci gaba da motsawa.
Tsarin Typoo ya ƙunshi cibiyar ƙarancin girgije da manyan girgije da guguwa.
Talvoon zai iya isa hanzari zuwa sama zuwa mil 157 a awa daya ko fiye.
Babbar mahaukaciyar guguwa a cikin duniya mai rikodin shine takaice na tekuna wanda ya faru a arewa maso yamma Pacific a 1979, tare da diamita na mil 1,380.
Har yanzu ake maganar hadari na Typhoon.
Talji na iya haifar da babban lalacewa, gami da ambaliyar ruwa, shimfidawa, da kuma hadari Tidal.
Hadari na Typhoon na iya haifar da lalacewar muhalli, kamar asarar gandun daji da lalacewar murjani.
