Atmosfernyi front
(ot. dr.-grech. ατμός par, σφαῖρα shar i lat. frontis lob, perednyaya storona) – perehodnaya zona v troposfere mezhdu smezhnymi vozdushnymi massami s raznymi fizicheskimi svoistvami.Atmosfernyi front voznikaet pri sblizhenii i vstreche mass holodnogo i teplogo vozduha v nizhnih sloyah atmosfery ili vo vsei troposfere, ohvatyvaya sloi moshnost'yu do neskol'kih km, s obrazovaniem mezhdu nimi naklonnoi poverhnosti razdela. Atmosfernyi front mozhet nahodit'sya v stacionarnom sostoyanii ili v dvizhenii.
Razlichayut teplye, holodnye fronty, a takzhe fronty okklyuzii. Osnovnymi atmosfernymi frontami yavlyayutsya: arkticheskie, polyarnye i tropicheskie.
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Publikacii s klyuchevymi slovami:
atmosfernyi front - vozdushnye massy
Publikacii so slovami: atmosfernyi front - vozdushnye massy | |
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