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advective thunderstorm
Definição1
A thunderstorm resulting from instability produced by advection of relatively colder air at high levels, or relatively warmer air at low levels, or by a combination of both conditions.
Fonte1
AMERICAN METEOROLOGICAL SOCIETY. Glossary of meteorology. [S.l., última modificação 05 oct. 2015]. Disponível em: < http://glossary.ametsoc.org/wiki/Main_Page >. Acesso em: 27 jun. 2022.
Fonte2
Z¨OBISCH, Isabella. Thunderstorms: Life cycle analyses and nowcasting based on multi-source data. 2019. Dissertação (Mestrado em Física) - Universidade Ludwig–Maximilians, Munique, Alemanha, 2019. Disponível em: https://edoc.ub.uni-muenchen.de/25680/1/Zoebisch_Isabella.pdf. Acesso em: 27 jun. 2022.
Contexto
Non-frontal situations are defined as the typical local heat, orographic or advective thunderstorm, originated by clear weather conditions preceding deep convection. Consequently, cloud masking is not a problem that happened often and single thunderstorms spread widely
Subárea
Aeronautical Meteorology
Français
orage d'advection