[Date Prev][Date Next][Thread Prev][Thread Next][Date Index][Thread Index]
Re: Dust Aloft Late Breaking-OT
- To: meteorite-list@meteoritecentral.com
- Subject: Re: Dust Aloft Late Breaking-OT
- From: GeoZay@aol.com
- Date: Wed, 6 Oct 1999 15:05:54 EDT
- Old-X-Envelope-To: <meteorite-list@meteoritecentral.com>
- Resent-Date: Wed, 6 Oct 1999 15:07:51 -0400 (EDT)
- Resent-From: meteorite-list@meteoritecentral.com
- Resent-Message-ID: <algiqD.A.cOD.125-3@mu.pair.com>
- Resent-Sender: meteorite-list-request@meteoritecentral.com
In a message dated 99-10-06 14:13:58 EDT, you write:
elton<<
The study shows that the "warm rain" processes that often
create rain in tropical clouds are practically shut off when the
clouds are polluted with heavy smoke from forest fires. In these
clouds, scientists found, the cloud tops must grow considerably
above the freezing level (16,000 feet) in order for them to start
producing rain by an alternative mechanism.
>>
The effects they were observing were of clouds within the troposphere where
most of our normal weather occurs. But in relation to this discussion, the
article also indicates nothing to show the inhibition of the formation of
moisture by the alternative mechanisms in the upper regions. From a large
impact, copious amounts of water vapor is driven by a high rising super
heated air mass to where it will eventually condense out from colder air or
the cold of space itself if it rises that high. There will probably be a
significant amount of collodial suspension to be seen as from volcanoes for a
few years, but dust dense enough to blot out all sunlight for dozens of years
doesn't seen likely to me.
GeoZay
----------
Archives located at:
http://www.meteoritecentral.com/list_best.html
For help, FAQ's and sub. info. visit:
http://www.meteoritecentral.com/mailing_list.html
----------