Concept

Anticyclonic storm

An anticyclonic storm is a storm with a high-pressure center, in which winds flow in the direction opposite to that of the flow above a region of low pressure. These storms can create powerful mesoanticylonic supercell storms that can generate anticyclonic tornadoes. Examples include the anticyclonic blizzard of 2018, Hartmut, Jupiter, and Neptune's anticyclonic cloud system. Anticyclonic storms usually form around high-pressure systems where air moves apart and sinks. Air at the center of these storms is forced away from the high pressure zones and replaced by a downdraft of air from higher altitudes. Anticyclonic storms have fewer clouds than cyclonic storms, due to a lower humidity. This lower humidity is caused by the air compressing and heating up as it moves downward. Anticyclonic storms, as high-pressure systems, usually accompany cold weather and are frequently a factor in large snowstorms. Along a cold front, an anticyclonic storm is called a wave, frontal, or mid-latitude anticyclonic storm when they are connected to a weather front. Due to the Coriolis effect, anticyclonic storms involve clockwise flow in the Northern Hemisphere and counterclockwise flow in the Southern Hemisphere. Supercells are long-lasting convective storms that are formed when thunderstorms are accompanied by strong vertical wind shear. For an antimesocyclone to form, there must be strong convective energy for cloud systems to be heavily reinforced with moist air. A supercell has a rotating updraft (mid-altitude mesocyclone) and a downdraft. The rotating updraft typically moves to the right. When it moves to the left (anticyclonically), mesoanticylonic super-cells are created. Anticyclonic supercells can produce hail storms, but rarely produce anticyclonic tornados. Tornadoes' vortices are low-pressure regions, but tornadoes rotate anticyclonically because tornadoes occur on a small enough scale that Coriolis effect is negligible. Anticyclonic supercells can go through tornadogenesis to develop into anticyclonic tornadoes.

About this result
This page is automatically generated and may contain information that is not correct, complete, up-to-date, or relevant to your search query. The same applies to every other page on this website. Please make sure to verify the information with EPFL's official sources.

Graph Chatbot

Chat with Graph Search

Ask any question about EPFL courses, lectures, exercises, research, news, etc. or try the example questions below.

DISCLAIMER: The Graph Chatbot is not programmed to provide explicit or categorical answers to your questions. Rather, it transforms your questions into API requests that are distributed across the various IT services officially administered by EPFL. Its purpose is solely to collect and recommend relevant references to content that you can explore to help you answer your questions.