From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #11429 Reply-To: ammf@fruvous.com Sender: owner-ammf-digest@smoe.org Errors-To: owner-ammf-digest@smoe.org Precedence: bulk alt.music.moxy-fruvous digest Wednesday, May 24 2023 Volume 14 : Number 11429 Today's Subjects: ----------------- Squeeze THIS on your foot (it kills pain in 2-seconds) ["Detoxing and cle] ---------------------------------------------------------------------- Date: Wed, 24 May 2023 17:05:36 +0200 From: "Detoxing and cleansing" Subject: Squeeze THIS on your foot (it kills pain in 2-seconds) Squeeze THIS on your foot (it kills pain in 2-seconds) http://neckrelaxz.shop/E9T2aqtjTSZYBiX9LPh7fgOwSw1F-Bd_crP3vrv3HA4zrUcBbQ http://neckrelaxz.shop/W4PJeOVn7J34_gbGLmPBvPByP3T5WRGFVCGu8wMgVBAYZwK4AA Eyewall mesovortices are small scale rotational features found in the eyewalls of intense tropical cyclones. They are similar, in principle, to small "suction vortices" often observed in multiple-vortex tornadoes. In these vortices, wind speeds may be greater than anywhere else in the eyewall. Eyewall mesovortices are most common during periods of intensification in tropical cyclones. Eyewall mesovortices often exhibit unusual behavior in tropical cyclones. They usually revolve around the low pressure center, but sometimes they remain stationary. Eyewall mesovortices have even been documented to cross the eye of a storm. These phenomena have been documented observationally, experimentally, and theoretically. Eyewall mesovortices are a significant factor in the formation of tornadoes after tropical cyclone landfall. Mesovortices can spawn rotation in individual convective cells or updrafts (a mesocyclone), which leads to tornadic activity. At landfall, friction is generated between the circulation of the tropical cyclone and land. This can allow the mesovortices to descend to the surface, causing tornadoes. These tornadic circulations in the boundary layer may be prevalent in the inner eyewalls of intense tropical cyclones but with short duration and small size they are not frequently observed. Stadium effect View of Typhoon Maysak's eye from the International Space Station on March 31, 2015, displaying a pronounced stadium effect The stadium effect is a phenomenon observed in strong tropical cyclones. It is a fairly common event, where the clouds of the eyewall curve outward from the surface with height. This gives the eye an appearance resembling a sports stadium from the air. An eye is always larger at the top of the storm, and smallest at the bottom of the storm because the rising air in the eyewall follows isolines ------------------------------ End of alt.music.moxy-fruvous digest V14 #11429 ***********************************************