Mesohigh

A mesohigh (sometimes called a "bubble high")^[1] is a mesoscale high-pressure area that forms beneath thunderstorms. While not always the case, it is usually associated with a mesoscale convective system.^[2] In the early stages of research on the subject, the mesohigh was often referred to as a "thunderstorm high".^[3]

^ Markowski, Paul; Yvette Richardson (2010). Mesoscale Meteorology in Midlatitudes. West Sussex, UK: John Wiley & Sons, Ltd. p. 140. ISBN 978-0-470-74213-6.
^ "Mesohigh". National Weather Service Glossary. National Weather Service. Retrieved 13 October 2011.
^ Fujita, Tetsuya (November 1955). "Results of Detailed Synoptic Studies of Squall Lines". Tellus. 7 (4): 405–436. doi:10.1111/j.2153-3490.1955.tb01181.x.

[1] Markowski, Paul; Yvette Richardson (2010). Mesoscale Meteorology in Midlatitudes. West Sussex, UK: John Wiley & Sons, Ltd. p. 140. ISBN 978-0-470-74213-6.

[2] "Mesohigh". National Weather Service Glossary. National Weather Service. Retrieved 13 October 2011.

[3] Fujita, Tetsuya (November 1955). "Results of Detailed Synoptic Studies of Squall Lines". Tellus. 7 (4): 405–436. doi:10.1111/j.2153-3490.1955.tb01181.x.

[1]

[2]

[3]