From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #8982 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 Saturday, May 21 2022 Volume 14 : Number 8982 Today's Subjects: ----------------- Reserve your free copy before itās gone! ["Philip" Subject: Reserve your free copy before itās gone! Reserve your free copy before itbs gone! http://productoon.co/8W8awB8Os5TgD-rhkcipToMilexVhPXQgq_UPGLU0LOPWc6_dg http://productoon.co/Fa1pe4N4jCXfVA6Zykyd-GTwlsqVtWMKL0viF_vxuQMuvclyaw us clouds have an average ice crystal concentration of 300,000 ice crystals per 10 cubic meters (270,000 ice crystals per 10 cubic yards). The concentration ranges from as low as 1 ice crystal per 10 cubic meters to as high as 100 million ice crystals per 10 cubic meters (just under 1 ice crystal per 10 cubic yards to 77 million ice crystals per 10 cubic yards), a difference of eight orders of magnitude. The size of each ice crystal is typically 0.25 millimeters, but they range from as short as 0.01 millimeters up to several millimeters. The ice crystals in contrails can be much smaller than those in naturally occurring cirrus cloud, being around 0.001 millimeters to 0.1 millimeters in length. In addition to forming in different sizes, the ice crystals in cirrus clouds can crystallize in different shapes: solid columns, hollow columns, plates, rosettes, and conglomerations of the various other types. The shape of the ice crystals is determined by the air temperature, atmospheric pressure, and ice supersaturation (the amount by which the relative humidity exceeds 100%). Cirrus in temperate regions typically have the various ice crystal shapes separated by type. The columns and plates conc ------------------------------ End of alt.music.moxy-fruvous digest V14 #8982 **********************************************