Relay-Version: version B 2.10 5/3/83; site utzoo.UUCP Posting-Version: version B 2.10.2 9/18/84; site shell.UUCP Path: utzoo!watmath!clyde!bonnie!akgua!whuxlm!harpo!decvax!genrad!panda!talcott!harvard!seismo!ut-sally!utmbvax!shell!buck From: buck@shell.UUCP (Lester Buck) Newsgroups: net.aviation,net.astro Subject: Re: Something else to watch out for! Message-ID: <122@shell.UUCP> Date: Wed, 19-Jun-85 10:44:58 EDT Article-I.D.: shell.122 Posted: Wed Jun 19 10:44:58 1985 Date-Received: Sun, 23-Jun-85 00:34:05 EDT References: <11270@brl-tgr.ARPA> <1199@phoenix.UUCP> <1679@amdahl.UUCP> Distribution: net Organization: CS Dept., Shell Development Co., Houston Lines: 11 Xref: watmath net.aviation:1653 net.astro:682 > I can't imagine how hitting a cloud layer - no matter how > dense - would be like hitting the ground (even at meteoric speeds). I remember from ground school that air filled with water vapor is less dense than dry air, even though is feels "heavy". If clouds are water vapor, doesn't this make them *less* dense than the surrounding air? Unless there was a storm in progess with condensed water, I guess. A. Lester Buck {ihnp4, pur-ee, ut-sally}!shell!buck