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	<title>CIMSS Satellite Blog &#187; Severe convection</title>
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	<description>A weblog of meteorological satellite imagery relevant to current weather events</description>
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		<title>Mesocale Convective Complex in South America</title>
		<link>http://cimss.ssec.wisc.edu/goes/blog/archives/3879</link>
		<comments>http://cimss.ssec.wisc.edu/goes/blog/archives/3879#comments</comments>
		<pubDate>Thu, 19 Nov 2009 22:19:09 +0000</pubDate>
		<dc:creator>scott.bachmeier</dc:creator>
				<category><![CDATA[GOES-10]]></category>
		<category><![CDATA[Severe convection]]></category>

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		<description><![CDATA[McIDAS images of the GOES-10 10.7 µm IR channel (above) showed very cold cloud top temperatures associated with a large Mesoscale Convective Complex (MCC) that developed over northern Argentina and moved across Uruguay and into far southern Brazil on 19 November 2009. The MCC exhibited unusually cold IR brightness temperature values, as low  as [...]]]></description>
			<content:encoded><![CDATA[<div class="wp-caption aligncenter" style="width: 490px"><a href="http://cimss.ssec.wisc.edu/goes/blog/wp-content/uploads/2009/11/091119_g10_ir4_anim.gif"><img alt="GOES-10 10.7 µm IR images" src="http://cimss.ssec.wisc.edu/goes/blog/wp-content/uploads/2009/11/091119_g10_ir4_anim.gif" title="GOES-10 10.7 µm IR images" width="480" height="360" /></a><p class="wp-caption-text">GOES-10 10.7 µm IR images</p></div>
<p><strong><a href="http://www.ssec.wisc.edu/mcidas/">McIDAS</a></strong> images of the GOES-10 10.7 µm IR channel <strong><em>(above)</em></strong> showed very cold cloud top temperatures associated with a large Mesoscale Convective Complex (MCC) that developed over northern Argentina and moved across Uruguay and into far southern Brazil on <strong>19 November 2009</strong>. The MCC exhibited unusually cold IR brightness temperature values, as low  as <strong>-89º C</strong> <em>(dark purple color enhancement)</em> at 04:58 UTC. In addition, early in the animation you can see several &#8220;enhanced-v&#8221; signatures on the IR imagery &#8212; this satellite  signature indicates that severe convective storms have a high potential for producing damaging winds, large hail, or tornadoes. There were media reports of a  tornado and hail  in parts of Uruguay, and according to the <strong><a href="http://www.metsul.com/blog/">Metsul Blog</a></strong> this MCC produced very strong winds <em>(gusting to 82 mph or 36.8 meters per second)</em> and heavy rainfall <em>(2.8 inches or 70 mm in 2 hours)</em> as the storm moved into the Rio Grande do Sul region of southern Brazil.</p>
<p>GOES-10 <em>(launched in 1997)</em> is currently positioned in orbit  at approximately 60 degrees West longitude  in support of the Earth Observation Partnership of the Americas EOPA project or  GEOSS Americas &#8212; however, due to end-of-life fuel conditions, <strong>GOES-10 will cease operations  on 01 December 2009.</strong</p>
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		<title>Mesoscale Convective Vortex (MCV) in the Upper Midwest region</title>
		<link>http://cimss.ssec.wisc.edu/goes/blog/archives/3215</link>
		<comments>http://cimss.ssec.wisc.edu/goes/blog/archives/3215#comments</comments>
		<pubDate>Fri, 14 Aug 2009 21:54:18 +0000</pubDate>
		<dc:creator>scott.bachmeier</dc:creator>
				<category><![CDATA[AWIPS]]></category>
		<category><![CDATA[GOES-12]]></category>
		<category><![CDATA[Severe convection]]></category>

		<guid isPermaLink="false">http://cimss.ssec.wisc.edu/goes/blog/?p=3215</guid>
		<description><![CDATA[AWIPS images of the GOES-12 10.7 µm IR channel (above) showed a strong Mesoscale Convective System (MCS) that developed over  South Dakota on 13 August 2009. This MCS spawned a long-lived Mesoscale Convective Vortex (MCV)  &#8212; sometimes referred to as a Mesocale Vorticity Center or MVC &#8212; that later helped to initiate another MCS over [...]]]></description>
			<content:encoded><![CDATA[<div class="wp-caption aligncenter" style="width: 490px"><a href="http://cimss.ssec.wisc.edu/goes/blog/wp-content/uploads/2009/08/090813-14_g12_ir_anim.gif"><img title="GOES-12 10.7 µm IR images" src="http://cimss.ssec.wisc.edu/goes/blog/wp-content/uploads/2009/08/090813-14_g12_ir_anim.gif" alt="GOES-12 10.7 µm IR images" width="480" height="360" /></a><p class="wp-caption-text">GOES-12 10.7 µm IR images</p></div>
<p>AWIPS images of the GOES-12 10.7 µm IR channel <em><strong>(above)</strong></em> showed a strong Mesoscale Convective System (MCS) that developed over  South Dakota on <strong><a title="13 August 2009 daily weather map" href="http://www.hpc.ncep.noaa.gov/dailywxmap/index_20090813.html" target="_blank">13 August 2009</a>. </strong>This MCS spawned a long-lived Mesoscale Convective Vortex (MCV)  &#8212; sometimes referred to as a Mesocale Vorticity Center or MVC &#8212; that later helped to initiate another MCS over Minnesota and Wisconsin during the pre-dawn hours on <a title="14 August 2009 daily weather map" href="http://www.hpc.ncep.noaa.gov/dailywxmap/index_20090814.html" target="_blank"><strong>14 August 2009</strong></a>.</p>
<div class="wp-caption aligncenter" style="width: 490px"><a href="http://cimss.ssec.wisc.edu/goes/blog/wp-content/uploads/2009/08/090814_g12_vis_anim.gif"><img title="GOES-12 visible images" src="http://cimss.ssec.wisc.edu/goes/blog/wp-content/uploads/2009/08/090814_g12_vis_anim.gif" alt="GOES-12 visible images" width="480" height="360" /></a><p class="wp-caption-text">GOES-12 visible images</p></div>
<p>The circulation of the MCV then continued to move northeastward across the Upper Peninsula of Michigan during the day on 14 August, as seen on an animation of GOES-12 visible images <em><strong>(above)</strong></em> and radar reflectivity <em><strong>(below)</strong></em>.</p>
<div class="wp-caption aligncenter" style="width: 489px"><a href="http://cimss.ssec.wisc.edu/goes/blog/wp-content/uploads/2009/08/090814_radar_anim.gif"><img title="Radar reflectivity" src="http://cimss.ssec.wisc.edu/goes/blog/wp-content/uploads/2009/08/090814_radar_anim.gif" alt="Radar reflectivity" width="479" height="359" /></a><p class="wp-caption-text">Radar reflectivity</p></div>
<p>The Blended Total Precipitable Water (TPW) product <em><strong>(below)</strong></em> showed that there was a plume of higher moisture <em>(TPW values of 37-41 mm or 1.5 to 1.6 inches)</em> feeding northeastward across Wisconsin into the Upper Peninsula, helping to sustain convective development in the vicinity of the MCV.</p>
<div class="wp-caption aligncenter" style="width: 490px"><a href="http://cimss.ssec.wisc.edu/goes/blog/wp-content/uploads/2009/08/090814_ir_pw_anim.gif"><img title="Blended TPW product + GOES-12 IR images" src="http://cimss.ssec.wisc.edu/goes/blog/wp-content/uploads/2009/08/090814_ir_pw_anim.gif" alt="Blended TPW product + GOES-12 IR images" width="480" height="360" /></a><p class="wp-caption-text">Blended TPW product + GOES-12 IR images</p></div>
<p>Since the Atlantic Basin has been seemingly disinterested in producing any notable tropical cyclone activity so far this season, one had to look to the Upper Midwest region of the US for signs of any &#8220;tropical development&#8221;:</p>
<blockquote>
<pre>AREA FORECAST DISCUSSION
NATIONAL WEATHER SERVICE MARQUETTE MI
500 PM EDT FRI AUG 14 2009

.SYNOPSIS...

TO THE S...LAZY FLOW EXISTS ACROSS THE UPPER MISSISSIPPI VALLEY AND
GREAT LAKES. AS A RESULT...MESOSCALE VORTICITY CENTER GENERATED BY
CONVECTION IN SD TWO NIGHTS AGO AND NOW LOCATED OVER CNTRL UPPER MI
IS STILL JUST DRIFTING ALONG IN AN ERLY DIRECTION. MVC CIRCULATION
REMAINS VERYWELL-DEFINED...JUST AS IMPRESSIVE AS IT WAS 24HRS AGO
DUE TO THE VERY LIGHT MID/UPPER FLOW IN WHICH IT IS EMBEDDED. WEAK
FLOW HASKEPT IT FROM SHEARING APART. <strong>IF THIS WAS LOCATED IN THE TROPICS...
YOU WOULD THINK IT WAS A TROPICAL SYSTEM.</strong> ALTHOUGH COMPACT...TIGHT
SPIRALING CLOUD CANOPY AROUND MVC HAS BEEN SUFFICIENT TO LIMIT AFTN
HEATING...SO CONVECTIVE DEVELOPMENT HAS BEEN KEPT IN CHECK THIS AFTN.</pre>
</blockquote>
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