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		<title>EdGCM</title>
		<description>EdGCM</description>
		<link>http://test.edgcm.columbia.edu</link>
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			<title>EdGCM</title>
			<link>http://test.edgcm.columbia.edu</link>
			<description>EdGCM</description>
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			<title>Examining the Effects of Global Warming on Greenland</title>
			<link>http://test.edgcm.columbia.edu/outreach/exercises/greenland.html</link>
			<description> Tracking the changes in temperature and snowfall over Greenland is of great interest to scientists because of the concern that global warming could lead to a melting of the Greenland ice sheet and add to rising sea levels.

We are interested in using EdGCM to explore whether or not the climate model can give us insight into the potential for snow to increase in a warming climate, especially over Greenland.</description>
			<category>Outreach - Exercises</category>
			<pubDate>Sun, 11 Dec 2005 11:18:09 +0100</pubDate>
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			<title>EdGCM Global Warming Exercise</title>
			<link>http://test.edgcm.columbia.edu/content/view/59/107/</link>
			<description>The following exercise explores the topic of Global Warming, but first it discusses how you would use a global climate model, and EdGCM, to construct the appropriate Modern climate control runs that are used as the base map for all climate change simulations. This exercise is used at many of our EdGCM training workshops and is a standard for getting started with EdGCM. The simulations used in this exercise come pre-installed with EdGCM 2.4 to EdGCM 3.0.</description>
			<category>Outreach - Exercises</category>
			<pubDate>Mon, 06 Mar 2006 12:27:36 +0100</pubDate>
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			<title>Simulating a Snowball Earth</title>
			<link>http://test.edgcm.columbia.edu/outreach/showcase/snowball_earth_750ma.html</link>
			<description>Extreme glacial events, the so-called &quot;snowball Earth&quot; intervals, are by far the coldest periods in Earth history, with evidence of ice sheets existing even in tropical regions. By trying to identify the key climate forcings that could have led to such cold conditions, we seek to understand the full natural range of climate variability on Earth. In this report, we simulate the effects of major changes to certain climate forcings in an effort to reproduce, with our model, the climatic conditions suggested by the geologic record. We find that while the combination of reduced solar luminosity, atmospheric CO2 levels, and ocean heat transports does cool the planet significantly, it is still not sufficient to reproduce the first-order characteristics of the Sturtian snowball Earth glaciation.
</description>
			<category>Outreach - Community Showcase</category>
			<pubDate>Fri, 31 Mar 2006 07:34:38 +0100</pubDate>
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			<title>A Climate Model Vacation Planner</title>
			<link>http://test.edgcm.columbia.edu/outreach/showcase/cambodia.html</link>
			<description> While planning a vacation to Cambodia last fall, I decided to try using an EdGCM simulation to verify information provided in the tour guide books. Though one should not expect statistically significant results from one or two grid cells in a GCM, compared to the limited and qualitative climate information in guidebooks, I discovered that a climate model can provide much more... cloud cover (tanning), soil moisture and ground wetness (camping), wind speed (windsurfing), and diurnal temperature variation. EdGCM, and presumably higher-resolution GCMs, are capable of local scale studies when the scientific accuracy of the results does not require a high degree of quantitative precision. EdGCM provides similar information (spatially and temporally) as guide books and the CIA World Factbook and then provides many additional variables.
</description>
			<category>Outreach - Community Showcase</category>
			<pubDate>Fri, 12 May 2006 23:59:14 +0100</pubDate>
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		<item>
			<title>The Last Ice Age - Part I</title>
			<link>http://test.edgcm.columbia.edu/outreach/showcase/21k.html</link>
			<description> Our first Commmunity Showcase article was written by Paolo Zamparutti of MTG Climate (http://mtgclimate.it) in Italy, and was translated by Giuseppe Petricca. MTG Climate used EdGCM to recreate the climatic conditions of 21 thousand years ago, when our planet was at the peak of the last Ice Age (i.e. The Last Glacial Maximum).</description>
			<category>Outreach - Community Showcase</category>
			<pubDate>Mon, 07 Nov 2005 12:00:00 +0100</pubDate>
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		<item>
			<title>The Last Ice Age - Part II</title>
			<link>http://test.edgcm.columbia.edu/outreach/showcase/21k2.html</link>
			<description> The first part of this investigation (http://edgcm.columbia.edu/outreach/showcase/21k.html) on the last Ice Age was published on MTG Climate (http://www.mtgclimate.it) in November. It  focused on some aspects of the climate of 21 thousand years ago. Now we can use the data given by the Ice Age 21k (http://edgcm.columbia.edu/outreach/showcase/21k.html) simulation to understand what are the fundamental differences between the climate of today and the glacial one: in particular we will focus our attention on the thermal aspect. We will base our studies on a simulation that represents a medium condition of the Wurmian period, when there were some warm and favourable phases and some colder ones.</description>
			<category>Outreach - Community Showcase</category>
			<pubDate>Mon, 27 Mar 2006 11:31:38 +0100</pubDate>
		</item>
		<item>
			<title>Simulating the Maunder Minimum</title>
			<link>http://test.edgcm.columbia.edu/outreach/showcase/maunder_minimum.html</link>
			<description>Our second Community Showcase article involves a simulation of the Maunder Minimum. Author Tom Rees recreates the work done in a recent paper by Shindell et al., offering his own insights on the subject of the Maunder Minimum and climate change.</description>
			<category>Outreach - Community Showcase</category>
			<pubDate>Tue, 20 Dec 2005 15:19:19 +0100</pubDate>
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