<table cellspacing="0" cellpadding="0" border="0" ><tr><td valign="top" style="font: inherit;"><br>Thank you Tere. That was the way I calculated early. <br>But like thies, there is a lack of moist from surface to 1000hPa, in the cases when surface pressure is higher than 1000. Otherwise I guess it could be some problems by the fact of having constant pressure files in one side, and surface files apart. That is puzzling me.<br><br> best<br><br> mario <br>--- On <b>Wed, 1/18/12, Tereza Cavazos <i><tcavazos@cicese.mx></i></b> wrote:<br><blockquote style="border-left: 2px solid rgb(16, 16, 255); margin-left: 5px; padding-left: 5px;"><br>From: Tereza Cavazos <tcavazos@cicese.mx><br>Subject: Re: [gradsusr] vertically integrated moisture flux<br>To: gradsusr@gradsusr.org<br>Date: Wednesday, January 18, 2012, 4:45 PM<br><br><div
id="yiv1811918116">
<div>
Hi,<br>
<br>
Another way to calculate<br>
Vertically integarted moisture flux convergence (VIMFC)<br>
from 1000mb to 100mb:<br>
<br>
sdfopen shum.nc<br>
sdfopen uwnd.nc<br>
sdfopen vwnd.nc<br>
<br>
set lon x1 x2<br>
set lat y1 y2<br>
set t 1 T<br>
set lev 1<br>
qu=vint(1000,shum.1*uwnd.2,100)<br>
qv=vint(1000,shum.1*vwnd.3,100)<br>
vimf=-hdivg(qu,qv)<br>
d vimf<br>
<br>
Best,<br>
Tereza Cavazos<br>
<br>
On 1/18/2012 10:30 AM, khaled ammar wrote:
<blockquote type="cite">
<div>
<div>dear friends <br>
</div>
<div>you can use the script to calculate qu component and adjust
for qv comonent for vertically integrated moisture flux vector
between 1000 and 300 hpa levels <br>
</div>
<div><br>
</div>
<div>my best</div>
<div>khaled ammar</div>
</div>
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