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 AA247603368; Tue, 15 Jul 1997 12:02:48 -0700 Return-Path: <kasplash@crl.com-DeleteThis> Received: from mail.crl.com by hplms26.hpl.hp.com with ESMTP (1.37.109.16/15.5+ECS 3.3+HPL1.1S) id AA101423356; Tue, 15 Jul 1997 12:02:36 -0700 Received: from crl5.crl.com (crl5.crl.com [165.113.1.16]) by mail.crl.com (8.8.6/) via SMTP id LAA14955 for <wind_talk@opus.hpl.hp.com-DeleteThis>; Tue, 15 Jul 1997 11:55:01 -0700 (PDT) env-from (kasplash@crl.com-DeleteThis) Received: by crl5.crl.com id AA19014 (5.65c/IDA-1.5 for wind_talk@opus.hpl.hp.com-DeleteThis); Tue, 15 Jul 1997 11:51:54 -0700 Date: Tue, 15 Jul 1997 11:51:54 -0700 (PDT) From: Bob Galvan <kasplash@crl.com-DeleteThis> To: wind_talk@opus.hpl.hp.com-DeleteThis Subject: Re: Sherman AM report In-Reply-To: <3.0.32.19970715111441.00776f94@sfpo.macromedia.com-DeleteThis> Message-Id: <Pine.SUN.3.91.970715114623.18933A-100000@crl5.crl.com-DeleteThis> Content-Type: TEXT/PLAIN; charset=US-ASCII
On Tue, 15 Jul 1997, Tom Slattery wrote:
> I'm guessing the pressure difference is greater during those times due to
> the land cooling off slower than the
> ocean.
Well keep guessing.
Water holds heat, and conversely absorbs a lot of heat.
It 's the ocean that cools (and heats) more slowly.
Here's my theory:
Midday is when the wind is dead, right?
Midday is when the bay/ocean will be at their warmest, so that is when
the temp diff is smallest.
kasplash@crl.com-DeleteThis
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