Monson

El Monsón (de la lengua araba mausim che ‘l voeurd dì ‘’stagion’’) l’è on vent periòdich associaa cont di cambiament climatich stagional per v

Monson
Lumbard ucidental Quest articol chì l'è scrivuu in lombard, grafia milanesa.
Monson de l’estàa.
Monson de l’invèrna

El Monsón (de la lengua araba mausim che ‘l voeurd dì ‘’stagion’’) l’è on vent periòdich associaa cont di cambiament climatich stagional per via de on divèrs riscaldament de la tèrra e di oceani.

D'estaa la fòrt radiazion solar la prodùs on fòrt riscaldament di continent pussée fòrt de quèll di oceani. Quèst el pròvoca ‘na circolazion convettiva con mòti verticaj discendent in sui ocean e ascendent in sui continent indoe el pieouv. L’effètt piovos l’è anmò pussée se in sui continent a gh’è anca na barriera orografica. La situazion a l’incontrari la succed d'invèrna quand el pioev in su i oceani. [1]


I zòn interssàa di monson hinn: [2]

Riferiment

  1. ↑ Mario Giuliacci (2010). Manuale di meteorologia (in italian). Alpha Test, 406–407. ISBN 88-483-1168-7. 
  2. ↑ Mario Giuliacci (2010). Manuale di meteorologia (in italian). Alpha Test, 407–409. ISBN 88-483-1168-7. 

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