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Perché la neve si scioglie in quota ma resta a valle, il fenomeno dell’inversione termica sulle Alpi
Il fenomeno dell’inversione termica è particolarmente rilevante sulle Alpi e contribuisce a spiegare perché la neve può sciogliersi più rapidamente in quota rispetto alle valli: non si tratta di un’anomalia dal punto di vista meteorologico, ma di una particolare stratificazione delle masse d’aria che crea un gradiente termico invertito.Continua a leggere
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