Received: from hplms26.hpl.hp.com by opus.hpl.hp.com with ESMTP (1.37.109.18/15.5+ECS 3.3+HPL1.1) id AA148413076; Thu, 7 Aug 1997 12:44:36 -0700 Return-Path: <stwinkle@ix.netcom.com-DeleteThis> Received: from user.host.net by hplms26.hpl.hp.com with ESMTP (1.37.109.16/15.5+ECS 3.3+HPL1.1S) id AA044233075; Thu, 7 Aug 1997 12:44:35 -0700 Received: from ScottPC.imagenet-cane.com (sjx-ca86-04.ix.netcom.com [207.94.112.196]) by user.host.net (8.8.5/8.7.3) with SMTP id PAA15612 for <wind_talk@opus.hpl.hp.com-DeleteThis>; Thu, 7 Aug 1997 15:16:22 -0400 Message-Id: <3.0.1.32.19970806165035.0068fbc0@popd.netcruiser-DeleteThis> X-Sender: stwinkle@popd.netcruiser-DeleteThis X-Mailer: Windows Eudora Light Version 3.0.1 (32) Date: Wed, 06 Aug 1997 16:50:35 -0700 To: wind_talk@opus.hpl.hp.com-DeleteThis From: Scott Winkler <stwinkle@ix.netcom.com-DeleteThis> Subject: Pressure Gradient's? In-Reply-To: <199708061835.LAA19999@zonker.hpl.hp.com-DeleteThis> Content-Type: text/plain; charset="us-ascii"
Anybody know how to translate the pressure gradients given on
the satelite images (eg. 1025 millibar high) into inches used
at the airports (29.92")?
This might be usefull in predicting wind conditions.
********************************
Scott Winkler
415 917-9674 (hm)
408 863-7260 (wk)
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