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Mereline kliima Vaata ka | Viited | NavigeerimismenüüЗначение слова "Морской климат" в Большой Советской Энциклопедии

Klimatoloogia


kliimatüüpööpäevasedaastased õhutemperatuuride amplituudidsuhteline niiskuspilvisusaastane sademete hulktsüklonidmandrilise kliimagaLääne-Euroopaparasvöötme mereline kliimaläänetuuledAtlandi ookeani










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Mereline kliima




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Merelise kliimaga alad Köppeni kliimaklassifikatsiooni järgi


Mereline kliima on kliimatüüp, millele on iseloomulikud väikesed ööpäevased ja aastased õhutemperatuuride amplituudid, kõrge suhteline niiskus, suur pilvisus ja aastane sademete hulk. Selline kliima on iseloomulik ookeanidele ja mereäärsetele rannikualadele, mille kliimat mõjutavad merelised õhumassid.[1] Näiteks mõjutavad Lääne-Euroopa kliimat Atlandi ookeani peal kujundavad merelised õhumassid, mis liiguvad läänest itta. Parasvöötmes liiguvad sageli mandri peale tsüklonid. Merelise kliimaga aladel on tavaliselt kõrgeimad ja madalaimad õhutemperatuurid 1–2 kuud võrra hiljem kui mandrilise kliimaga piirkondades, sest veemassid soojenevad ja jahutavad aeglasem, kui maismaa. Sügis on tavaliselt soojem, kui kevad.




Merelise kliima kliimadiagramm


Tüüpilise merelise kliima näide on Lääne-Euroopa parasvöötme mereline kliima, kus on aasta ringi ülekaalus läänetuuled, mistõttu soojad ja niisked õhumassid liiguvad Atlandi ookeani kohalt mandrialadele. Selle tõttu on aastased amplituudid Euroopa lääneosas vaid paar kraadi ja ida poole (mandri poole) liikudes amplituud järk-järgult suurenevad.



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  • Mandriline kliima

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  1. ↑ Значение слова "Морской климат" в Большой Советской Энциклопедии










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