Relay-Version: version B 2.10 5/3/83; site utzoo.UUCP Posting-Version: version B 2.10.1 6/24/83; site phoenix.UUCP Path: utzoo!watmath!clyde!burl!ulysses!mhuxr!mhuxt!houxm!ihnp4!phoenix!brent From: brent@phoenix.UUCP (Brent P. Callaghan) Newsgroups: net.aviation,net.astro Subject: Re: Something else to watch out for! Message-ID: <1199@phoenix.UUCP> Date: Fri, 14-Jun-85 09:24:45 EDT Article-I.D.: phoenix.1199 Posted: Fri Jun 14 09:24:45 1985 Date-Received: Sat, 15-Jun-85 08:03:15 EDT References: <11270@brl-tgr.ARPA> Distribution: net Organization: AT&T Information Systems, Lincroft NJ Lines: 44 Xref: watmath net.aviation:1635 net.astro:669 > Anyway, this JAL flight was cruising at some normal jet-type altitude > (like 30,000 ft or thereabouts) some distance above a rather dense cloud > layer. Suddenly, directly ahead, the pilot saw the clouds begin to rise up > in an enormous bulge. The cloud bulge grew at fantastic speed, and > soon reached up and sideways for distances measureable in miles. The pilot > took evasive action, but could not avoid flying through the cloud; he > was convinced that he was flying through the results of an atomic > explosion, so he had the crew go on emergency oxygen, and he landed > at the next available site to have the plane checked and decontaminated > if necessary. > > Well, there was no evidence of radioactivity, and no ground-based > phenomenon reported that would explain this occurrence. Normal atmospheric > changes, like the formation of cumulus clouds, cannot occur at the rate > observed. The JAL flight eventually continued on to its destination. > > What caused this? Well, the theory is that that airplane had the first > observed encounter with a meteor. A several-ton meteor, of several meters > diameter, perhaps composed of mostly ice with some stony fragments, could > have hit that cloud layer on its way down through the atmosphere. At > meteoric speeds, hitting a dense cloud layer is almost equivalent to > hitting the ground. The meteor would have fragmented and probably > vaporized, transfering all its enormous kinetic and thermal energy > to the cloud structure in the form of heat. This would have caused the > observed huge boiling-up of the clouds and the formation of such an > atmospheric structure. I can't imagine how hitting a cloud layer - no matter how dense - would be like hitting the ground (even at meteoric speeds). Supersonic aircraft, space-shuttles etc fly regularly through dense clouds without a bump. As a skydiver I've fallen through dense clouds without feeling a thing (although I've often wished they really were like soft fluffy cotton wool :-) ) Perhaps the boiling-up was due just to a ginormous thermal from the atmospheric heating in its wake. (Bet those pilots were glad it WASN'T a nuclear explosion !) -- Made in New Zealand --> Brent Callaghan AT&T Information Systems, Lincroft, NJ {ihnp4|mtuxo|pegasus}!phoenix!brent (201) 576-3475