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	<title>VISIT: Meteorological Interpretation Blog</title>
	<atom:link href="http://rammb.cira.colostate.edu/training/visit/blog/index.php/feed/" rel="self" type="application/rss+xml" />
	<link>http://rammb.cira.colostate.edu/training/visit/blog</link>
	<description>Questions and Answers Concerning Problems in Meteorology</description>
	<lastBuildDate>Wed, 03 Apr 2013 21:32:13 +0000</lastBuildDate>
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		<title>Synthetic imagery comparison from 2 different models</title>
		<link>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2013/04/03/synthetic-imagery-comparison-from-2-different-models/?utm_source=rss&#038;utm_medium=rss&#038;utm_campaign=synthetic-imagery-comparison-from-2-different-models</link>
		<comments>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2013/04/03/synthetic-imagery-comparison-from-2-different-models/#comments</comments>
		<pubDate>Wed, 03 Apr 2013 21:32:13 +0000</pubDate>
		<dc:creator>dbikos</dc:creator>
				<category><![CDATA[GOES]]></category>
		<category><![CDATA[GOES R]]></category>
		<category><![CDATA[GOES-R Proving Ground]]></category>
		<category><![CDATA[Satellites]]></category>
		<category><![CDATA[Severe Weather]]></category>

		<guid isPermaLink="false">http://rammb.cira.colostate.edu/training/visit/blog/?p=674</guid>
		<description><![CDATA[This blog entry will make a comparison between synthetic imagery generated from 2 different models, the NSSL WRF-ARW and the NAM-Nest, both with a horizontal grid spacing of 4 km.  After comparing the synthetic imagery between the 2 models, we &#8230; <a href="http://rammb.cira.colostate.edu/training/visit/blog/index.php/2013/04/03/synthetic-imagery-comparison-from-2-different-models/">Continue reading <span class="meta-nav">&#8594;</span></a>]]></description>
		<wfw:commentRss>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2013/04/03/synthetic-imagery-comparison-from-2-different-models/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>Synthetic imagery application of a snow event on March 5-6, 2013</title>
		<link>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2013/03/21/synthetic-imagery-application-of-a-snow-event-on-march-5-6-2013/?utm_source=rss&#038;utm_medium=rss&#038;utm_campaign=synthetic-imagery-application-of-a-snow-event-on-march-5-6-2013</link>
		<comments>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2013/03/21/synthetic-imagery-application-of-a-snow-event-on-march-5-6-2013/#comments</comments>
		<pubDate>Thu, 21 Mar 2013 22:27:02 +0000</pubDate>
		<dc:creator>dbikos</dc:creator>
				<category><![CDATA[Cyclogenesis]]></category>
		<category><![CDATA[GOES-R Proving Ground]]></category>
		<category><![CDATA[Winter Weather]]></category>

		<guid isPermaLink="false">http://rammb.cira.colostate.edu/training/visit/blog/?p=651</guid>
		<description><![CDATA[The synthetic IR (10.35 um) imagery from the 0000 UTC 5 March 2013 NSSL WRF-ARW run: http://rammb.cira.colostate.edu/templates/loop_directory.asp?data_folder=training/visit/loops/6mar13_syn_wrf&#38;image_width=1020&#38;image_height=900 forecasts a region of colder cloud tops from the Ohio Valley towards the mid-Atlantic states during the late afternoon to morning hours of &#8230; <a href="http://rammb.cira.colostate.edu/training/visit/blog/index.php/2013/03/21/synthetic-imagery-application-of-a-snow-event-on-march-5-6-2013/">Continue reading <span class="meta-nav">&#8594;</span></a>]]></description>
		<wfw:commentRss>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2013/03/21/synthetic-imagery-application-of-a-snow-event-on-march-5-6-2013/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>Transverse bands on February 8, 2013</title>
		<link>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2013/02/14/transverse-bands-on-february-8-2013/?utm_source=rss&#038;utm_medium=rss&#038;utm_campaign=transverse-bands-on-february-8-2013</link>
		<comments>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2013/02/14/transverse-bands-on-february-8-2013/#comments</comments>
		<pubDate>Thu, 14 Feb 2013 17:16:27 +0000</pubDate>
		<dc:creator>dbikos</dc:creator>
				<category><![CDATA[GOES]]></category>
		<category><![CDATA[GOES R]]></category>
		<category><![CDATA[GOES-R Proving Ground]]></category>
		<category><![CDATA[NWP Models (NCEP)]]></category>
		<category><![CDATA[Satellites]]></category>
		<category><![CDATA[Turbulence]]></category>
		<category><![CDATA[Winter Weather]]></category>

		<guid isPermaLink="false">http://rammb.cira.colostate.edu/training/visit/blog/?p=628</guid>
		<description><![CDATA[Transverse bands were observed between approximately 1400-1700 UTC in the vicinity of Buffalo, NY in the GOES water vapor imagery (from the CIMSS satellite blog): http://cimss.ssec.wisc.edu/goes/blog/wp-content/uploads/2013/02/130208_g13_wv_east_coast_storm_anim.gif and also in the GOES IR imagery: http://rammb.cira.colostate.edu/templates/loop_directory.asp?data_folder=training/visit/loops/8feb13_BUF_ir&#38;image_width=1020&#38;image_height=900 Note the orientation of the transverse &#8230; <a href="http://rammb.cira.colostate.edu/training/visit/blog/index.php/2013/02/14/transverse-bands-on-february-8-2013/">Continue reading <span class="meta-nav">&#8594;</span></a>]]></description>
		<wfw:commentRss>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2013/02/14/transverse-bands-on-february-8-2013/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>Mesoscale vortex development over Lake Ontario on January 23, 2013</title>
		<link>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2013/01/24/mesoscale-vortex-development-over-lake-ontario-on-january-23-2013/?utm_source=rss&#038;utm_medium=rss&#038;utm_campaign=mesoscale-vortex-development-over-lake-ontario-on-january-23-2013</link>
		<comments>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2013/01/24/mesoscale-vortex-development-over-lake-ontario-on-january-23-2013/#comments</comments>
		<pubDate>Thu, 24 Jan 2013 23:26:21 +0000</pubDate>
		<dc:creator>dbikos</dc:creator>
				<category><![CDATA[Convection]]></category>
		<category><![CDATA[Lake Effects]]></category>
		<category><![CDATA[RADAR]]></category>
		<category><![CDATA[Winter Weather]]></category>

		<guid isPermaLink="false">http://rammb.cira.colostate.edu/training/visit/blog/?p=603</guid>
		<description><![CDATA[An Arctic airmass over the Great Lakes provided for a significant lake-effect snow event off Lake Ontario leading up to January 23, 2013 (maximum snowfall reports 3 feet near the southeast shoreline).  Near the end of this lake-effect snow event, &#8230; <a href="http://rammb.cira.colostate.edu/training/visit/blog/index.php/2013/01/24/mesoscale-vortex-development-over-lake-ontario-on-january-23-2013/">Continue reading <span class="meta-nav">&#8594;</span></a>]]></description>
		<wfw:commentRss>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2013/01/24/mesoscale-vortex-development-over-lake-ontario-on-january-23-2013/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>December 3, 2012 Fog event in South Carolina</title>
		<link>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2012/12/12/december-3-2012-fog-event-in-south-carolina/?utm_source=rss&#038;utm_medium=rss&#038;utm_campaign=december-3-2012-fog-event-in-south-carolina</link>
		<comments>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2012/12/12/december-3-2012-fog-event-in-south-carolina/#comments</comments>
		<pubDate>Wed, 12 Dec 2012 22:47:50 +0000</pubDate>
		<dc:creator>dbikos</dc:creator>
				<category><![CDATA[Aviation Weather]]></category>
		<category><![CDATA[Fog]]></category>

		<guid isPermaLink="false">http://rammb.cira.colostate.edu/training/visit/blog/?p=583</guid>
		<description><![CDATA[During the VISIT Satellite Chat on the morning of December 12, forecasters at the WFO in Columbia, SC alerted us to a fog event that took place in their CWA during the early morning hours of December 3, 2012.  During &#8230; <a href="http://rammb.cira.colostate.edu/training/visit/blog/index.php/2012/12/12/december-3-2012-fog-event-in-south-carolina/">Continue reading <span class="meta-nav">&#8594;</span></a>]]></description>
		<wfw:commentRss>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2012/12/12/december-3-2012-fog-event-in-south-carolina/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>Synthetic Low Cloud / Fog Product for October 10, 2012</title>
		<link>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2012/10/16/synthetic-low-cloud-fog-product-for-october-10-2012/?utm_source=rss&#038;utm_medium=rss&#038;utm_campaign=synthetic-low-cloud-fog-product-for-october-10-2012</link>
		<comments>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2012/10/16/synthetic-low-cloud-fog-product-for-october-10-2012/#comments</comments>
		<pubDate>Tue, 16 Oct 2012 17:04:36 +0000</pubDate>
		<dc:creator>dbikos</dc:creator>
				<category><![CDATA[Aviation Weather]]></category>
		<category><![CDATA[Ceilings]]></category>
		<category><![CDATA[Fog]]></category>
		<category><![CDATA[GOES-R Proving Ground]]></category>
		<category><![CDATA[Visibility]]></category>

		<guid isPermaLink="false">http://rammb.cira.colostate.edu/training/visit/blog/?p=569</guid>
		<description><![CDATA[Dan Bikos This blog entry will examine the synthetic low cloud / fog product produced by the 4-km NSSL WRF-ARW model.  For detailed information on this product, see: http://rammb.cira.colostate.edu/training/visit/training_sessions/synthetic_imagery_in_forecasting_low_clouds_and_fog/ Let’s examine this product on the Washington and Oregon coastline from &#8230; <a href="http://rammb.cira.colostate.edu/training/visit/blog/index.php/2012/10/16/synthetic-low-cloud-fog-product-for-october-10-2012/">Continue reading <span class="meta-nav">&#8594;</span></a>]]></description>
		<wfw:commentRss>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2012/10/16/synthetic-low-cloud-fog-product-for-october-10-2012/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>Super Typhoon Jelawat</title>
		<link>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2012/09/25/super-typhoon-jelawat/?utm_source=rss&#038;utm_medium=rss&#038;utm_campaign=super-typhoon-jelawat</link>
		<comments>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2012/09/25/super-typhoon-jelawat/#comments</comments>
		<pubDate>Tue, 25 Sep 2012 17:02:52 +0000</pubDate>
		<dc:creator>dbikos</dc:creator>
				<category><![CDATA[MODIS]]></category>
		<category><![CDATA[POES]]></category>
		<category><![CDATA[Satellites]]></category>
		<category><![CDATA[Tropical Cyclones]]></category>

		<guid isPermaLink="false">http://rammb.cira.colostate.edu/training/visit/blog/?p=549</guid>
		<description><![CDATA[Dan Bikos Typhoon Jelawat developed in the Phillippine Sea of the western Pacific Ocean around September 20, 2012.  See the westernmost track of the figure below: As the cyclone began turning towards the north / northwest while it was east &#8230; <a href="http://rammb.cira.colostate.edu/training/visit/blog/index.php/2012/09/25/super-typhoon-jelawat/">Continue reading <span class="meta-nav">&#8594;</span></a>]]></description>
		<wfw:commentRss>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2012/09/25/super-typhoon-jelawat/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>Microburst Risk Algorithm observes Favorable Conditions for Strong Convective Winds over the Chesapeake Bay</title>
		<link>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2012/09/17/microburst-risk-algorithm-observes-favorable-conditions-for-strong-convective-winds-over-the-chesapeake-bay-2/?utm_source=rss&#038;utm_medium=rss&#038;utm_campaign=microburst-risk-algorithm-observes-favorable-conditions-for-strong-convective-winds-over-the-chesapeake-bay-2</link>
		<comments>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2012/09/17/microburst-risk-algorithm-observes-favorable-conditions-for-strong-convective-winds-over-the-chesapeake-bay-2/#comments</comments>
		<pubDate>Mon, 17 Sep 2012 17:03:44 +0000</pubDate>
		<dc:creator>dbikos</dc:creator>
				<category><![CDATA[Aviation Weather]]></category>
		<category><![CDATA[Destructive Winds]]></category>
		<category><![CDATA[Downbursts]]></category>
		<category><![CDATA[Severe Weather]]></category>

		<guid isPermaLink="false">http://rammb.cira.colostate.edu/training/visit/blog/?p=528</guid>
		<description><![CDATA[Ken Pryor (NESDIS / STAR) A GOES sounder-derived Microburst Windspeed Potential (MWP) algorithm, based on convective available potential energy (CAPE), and vertical temperature and humidity lapse rates, and based on the vertical difference in equivalent potential temperature (theta-e difference, TED) &#8230; <a href="http://rammb.cira.colostate.edu/training/visit/blog/index.php/2012/09/17/microburst-risk-algorithm-observes-favorable-conditions-for-strong-convective-winds-over-the-chesapeake-bay-2/">Continue reading <span class="meta-nav">&#8594;</span></a>]]></description>
		<wfw:commentRss>http://rammb.cira.colostate.edu/training/visit/blog/index.php/2012/09/17/microburst-risk-algorithm-observes-favorable-conditions-for-strong-convective-winds-over-the-chesapeake-bay-2/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
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