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	<title>The Why Files &#187; Interactives</title>
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	<link>http://whyfiles.org</link>
	<description>The Science Behind The News</description>
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		<title>How does tornado season vary across the United States?</title>
		<link>http://whyfiles.org/2010/tornado-season-variations-across-the-united-states/</link>
		<comments>http://whyfiles.org/2010/tornado-season-variations-across-the-united-states/#comments</comments>
		<pubDate>Mon, 10 May 2010 13:00:40 +0000</pubDate>
		<dc:creator>admin</dc:creator>
				<category><![CDATA[August]]></category>
		<category><![CDATA[December]]></category>
		<category><![CDATA[February]]></category>
		<category><![CDATA[Interactives]]></category>
		<category><![CDATA[January]]></category>
		<category><![CDATA[Weather Guys]]></category>
		<category><![CDATA[tornado]]></category>
		<category><![CDATA[Tornado Alley]]></category>
		<category><![CDATA[tornado season]]></category>

		<guid isPermaLink="false">http://whyfiles.org/2010/tornado-season-variations-across-the-united-states/</guid>
		<description><![CDATA[How does tornado season vary across the United States? Tornado season begins as early as late February or early March in northern Texas and Oklahoma, the southern portion of Tornado Alley, where the tornado threat remains through most of May. By early June, the greatest threats tend to lie to the north, in Kansas and [...]]]></description>
			<content:encoded><![CDATA[<h3>How does tornado season vary across the United States?</h3>
<p>Tornado season begins as early as late February or early March in northern Texas and Oklahoma, the southern portion of Tornado Alley, where the tornado threat remains through most of May.  By early June, the greatest threats tend to lie to the north, in Kansas and Nebraska. By July, the peak threat finally reaches the southern Great Lakes states.</p>
<p>This northward march of the tornado threat is most directly related to the northward retreat of the jet stream over the same period.  The jet stream is a ribbon of high wind speeds, about six miles above the surface, that is located roughly at the warm edge of polar air at upper levels.</p>
<p>In early spring, the Northern Hemisphere is still rather chilly and the warm edge of the upper level polar air resides over or near the Gulf of Mexico.  The polar air gradually retreats to the Great Lakes by late June and even further north later in the summer.</p>
<p>As climate warms, there is some reason to expect a change in the number of tornadoes in some locations in the United States but, since other factors contribute to tornado frequency, it is not clear if the numbers will increase or decrease.</p>
<div class="imgBigBlack">
<a href="http://whyfiles.org/wp-content/uploads/2010/05/081805_30mi1.jpg"><img class="alignnone size-full wp-image-7566" title="August 18 tornado over Stoughton, WI" src="http://whyfiles.org/wp-content/uploads/2010/05/081805_30mi1.jpg" alt="Supercell forms anvil-shaped cloud over treeline" width="620" height="203" /></a></p>
<div class="caption">August 18, 2005: A late-season tornado forms a supercell over Stoughton, Wisconsin. Photo: S.V. Medaris</div>
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<p>
Steven A. Ackerman and Jonathan Martin are professors in the Department of Atmospheric and Oceanic Sciences at UW-Madison, are guests on the <a href="http://www.wpr.org/larrymeiller/">Larry Meiller</a>&#8216;s WHA-AM radio show the last Monday of each month at 11:45 a.m.</p>
</div>
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		<item>
		<title>Hit a home run</title>
		<link>http://whyfiles.org/2010/hit-a-home-run/</link>
		<comments>http://whyfiles.org/2010/hit-a-home-run/#comments</comments>
		<pubDate>Thu, 18 Feb 2010 18:34:39 +0000</pubDate>
		<dc:creator>admin</dc:creator>
				<category><![CDATA[Interactives]]></category>
		<category><![CDATA[atmosphere]]></category>
		<category><![CDATA[baseball]]></category>
		<category><![CDATA[physics]]></category>

		<guid isPermaLink="false">http://whyfiles.org/2010/hit-a-home-run/</guid>
		<description><![CDATA[Whack that baseball! When you hit a baseball, speed, angle and air resistance all affect how far it travels. Balls hit too low quickly return to Earth; balls hit too high travel a long way vertically, but not far horizontally. Can you find the &#8220;sweet spot&#8221; where horizontal travel is greatest. Can you find the [...]]]></description>
			<content:encoded><![CDATA[<p><strong>Whack that baseball!</strong><br />
When you hit a baseball, speed, angle and air resistance all affect how far it travels. Balls hit too low quickly return to Earth; balls hit too high travel a long way vertically, but not far horizontally. Can you find the &#8220;sweet spot&#8221; where horizontal travel is greatest. Can you find the best angle?</p>
<p>Air resistance absorbs kinetic energy from the ball, slowing it. A slow-moving ball has less travel time before gravity pulls it back to Earth. Change air resistance by choosing a different stadium location.</p>
<div class="imgBigClear">
<applet name="applet" codebase="/wp-content/" code="Homerun.class" archive="homerun.jar" width="425" height="296" alt="You must have Java enabled on your computer to view this applet">
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<div id="relateds">
<p>
Applet and illustrations copyright (C) 2003 Tom Whittaker, S.V. Medaris, and Steve Ackerman. The Motion-W® and Bucky Badger® logos are trademarks of the University of Wisconsin-Madison.
</p>
</div>
]]></content:encoded>
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		<title>Make a snowflake</title>
		<link>http://whyfiles.org/2010/make-a-snowflake/</link>
		<comments>http://whyfiles.org/2010/make-a-snowflake/#comments</comments>
		<pubDate>Thu, 18 Feb 2010 18:31:39 +0000</pubDate>
		<dc:creator>admin</dc:creator>
				<category><![CDATA[Interactives]]></category>
		<category><![CDATA[atmosphere]]></category>
		<category><![CDATA[snowflake]]></category>

		<guid isPermaLink="false">http://whyfiles.org/2010/make-a-snowflake/</guid>
		<description><![CDATA[The curious growth of a snow crystal Temperature and humidity affects the shape of snowflake crystals. The temperature of formation determines the original crystal shape. Large (&#8220;dendritic&#8221;) flakes grow best between -10° and -12° C. Plates grow at warmer or colder conditions. Humidity &#8212; water vapor pressure in the cloud &#8212; affects the growth rate [...]]]></description>
			<content:encoded><![CDATA[<p><strong>The curious growth of a snow crystal</strong><br />
Temperature and humidity affects the shape of snowflake crystals. The temperature of formation determines the original crystal shape. Large (&#8220;dendritic&#8221;) flakes grow best between -10° and -12° C. Plates grow at warmer or colder conditions.</p>
<p>Humidity &#8212; water vapor pressure in the cloud &#8212; affects the growth rate due to deposition. A flake that passes through dry air may sublimate (lose mass by converting from solid to gas).</p>
<p>Because temperature and humidity change as a flake bounces around in a cloud, the basic shapes can blend into countless crystal shapes. An ice crystal may also collide with another crystal and aggregate into a snowflake of a different shape. Or crystals may grow as they accrete (collide and adhere) tiny drops of liquid water in the cloud.</p>
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</div>
<div id="relateds">
<p>
Applet and illustrations copyright (C) 2003 Tom Whittaker, S.V. Medaris, and Steve Ackerman. The Motion-W® and Bucky Badger® logos are trademarks of the University of Wisconsin-Madison.
</p>
</div>
]]></content:encoded>
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		<title>Play with lightning</title>
		<link>http://whyfiles.org/2010/play-with-lightning/</link>
		<comments>http://whyfiles.org/2010/play-with-lightning/#comments</comments>
		<pubDate>Thu, 18 Feb 2010 18:30:02 +0000</pubDate>
		<dc:creator>admin</dc:creator>
				<category><![CDATA[Interactives]]></category>
		<category><![CDATA[lightning]]></category>

		<guid isPermaLink="false">http://whyfiles.org/2010/play-with-lightning/</guid>
		<description><![CDATA[Light on Lightning! Danger! Sound moves about 1,000 feet per second through air. To find out how far away the storm is, start counting &#8220;1 one-thousand, 2 one-thousand&#8230;&#8221; when you see a flash. Five counts, or five seconds, equals about one mile. But lightning bolts don&#8217;t come just from the center of the storm. To [...]]]></description>
			<content:encoded><![CDATA[<p><strong>Light on Lightning! Danger!</strong><br />
Sound moves about 1,000 feet per second through air. To find out how far away the storm is, start counting &#8220;1 one-thousand, 2 one-thousand&#8230;&#8221; when you see a flash. Five counts, or five seconds, equals about one mile.</p>
<p>But lightning bolts don&#8217;t come just from the center of the storm. To see the dangers of a &#8220;bolt from the blue,&#8221; place the little humanoid about five or six miles from the storm. Wait, and watch!</p>
<p><strong>The shadow of sound</strong><br />
Light and sound both refract (changes direction) when their waves move into a medium of different density. Glass lenses work because of the different density of air and glass. This is harder to see with sound waves, but it can happen near a thunderstorm, where air temperature and density can both change quickly. When air near the ground is warmer than air higher up, sound will travel faster through the denser air near the ground, and sound waves will refract, as you can see around mile seven. During the <a href="http://asa.aip.org/Echoes/Vol9No1/EchoesWinter1999.html">Civil War</a>, these &#8220;<a href="http://paws.kettering.edu/~drussell/Demos/refract/refract.html">acoustical shadows</a>&#8221; caused artillery that could be seen in the distance to be inaudible on parts of the battlefield.</p>
<div class="imgBigClear">
<applet name="applet" codebase="/wp-content/" code="Lightning.class" archive="lightning.jar" width="100%" height="385" alt="You must have Java enabled on your computer to view this applet">
</div>
<div id="relateds">
<p>
Applet and illustrations copyright (C) 2003 Tom Whittaker, S.V. Medaris, and Steve Ackerman. The Motion-W® and Bucky Badger® logos are trademarks of the University of Wisconsin-Madison.
</p>
</div>
]]></content:encoded>
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		<title>Control a tornado</title>
		<link>http://whyfiles.org/2010/control-a-tornado/</link>
		<comments>http://whyfiles.org/2010/control-a-tornado/#comments</comments>
		<pubDate>Thu, 18 Feb 2010 18:26:15 +0000</pubDate>
		<dc:creator>admin</dc:creator>
				<category><![CDATA[Interactives]]></category>
		<category><![CDATA[atmosphere]]></category>
		<category><![CDATA[tornado]]></category>

		<guid isPermaLink="false">http://whyfiles.org/2010/control-a-tornado/</guid>
		<description><![CDATA[A tornado that&#8217;s 500 meters in diameter looks a lot more ominous than the average twister, which is &#8220;only&#8221; 150 meters across. All other things being equal, larger tornadoes are more damaging, but size is not related to wind speed. Instead, wind speed increases along with the difference between atmospheric pressure inside the funnel, and [...]]]></description>
			<content:encoded><![CDATA[<p>A tornado that&#8217;s 500 meters in diameter looks a lot more ominous than the average twister, which is &#8220;only&#8221; 150 meters across. All other things being equal, larger tornadoes are more damaging, but size is not related to wind speed. Instead, wind speed increases along with the difference between atmospheric pressure inside the funnel, and the pressure outside it (the core pressure difference). The larger the core pressure difference, the faster the winds. But at a given wind speed, a larger tornado will do more total damage because it will hit more objects. The Fujita scale estimates tornado damage.</p>
<div class="imgBigClear">
<applet name="applet" codebase="/wp-content/" code="Twister.class" archive="twister.jar" width="100%" height="450" alt="You must have Java enabled on your computer to view this applet">
</div>
<div id="relateds">
<p>
Applet and illustrations copyright (C) 2003 Tom Whittaker, S.V. Medaris, and Steve Ackerman. The Motion-W® and Bucky Badger® logos are trademarks of the University of Wisconsin-Madison.
</p>
</div>
]]></content:encoded>
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		<title>Make rainbows!</title>
		<link>http://whyfiles.org/2010/make-rainbows/</link>
		<comments>http://whyfiles.org/2010/make-rainbows/#comments</comments>
		<pubDate>Thu, 21 Jan 2010 20:38:13 +0000</pubDate>
		<dc:creator>admin</dc:creator>
				<category><![CDATA[Interactives]]></category>
		<category><![CDATA[meteorology weather]]></category>
		<category><![CDATA[rainbow]]></category>

		<guid isPermaLink="false">http://whyfiles.org/?p=4232</guid>
		<description><![CDATA[Rainbows are one of the wonders of the natural world: But why do you sometimes see one rainbow, and other times a double? Why do you always see rainbows with your back to the sun? How do they really work? Operate your own rainbow, then find out! OPERATING INSTRUCTIONS: CHOOSE YOUR &#8216;BOW: • Primary shows [...]]]></description>
			<content:encoded><![CDATA[<p>Rainbows are one of the wonders of the natural world: But why do you sometimes see one rainbow, and other times a double? Why do you always see rainbows with your back to the sun? How do they really work?</p>
<p>Operate your own rainbow, then find out!</p>
<div class="imgBigClear">
<applet name="applet" codebase="/wp-content/" code="Rainbows.class" archive="rainbows.jar" width="100%" height="450" alt="You must have Java enabled on your computer to view this applet">
</div>
<p>OPERATING INSTRUCTIONS:<br />
CHOOSE YOUR &#8216;BOW:<br />
• <strong>Primary</strong> shows the primary rainbow and its light rays.</p>
<p>• <strong>Secondary</strong> shows the secondary &#8216;bow and its light rays. Notice this bow is seen from different places on the ground; some observers can see a primary, but not a secondary, or vice versa. Lucky people can see both rainbows.</p>
<p>• <strong>To see both</strong> &#8216;bows (but no light rays), uncheck both rainbow boxes in Rain Curtain Mode.</p>
<p>PICK YOUR MODE:<br />
<strong>• Rain Curtain mode</strong> shows parallel light rays from the sun refracting and reflecting from raindrops at the top and bottom of the rain curtain. Outgoing beams show where the rainbow is visible.</p>
<p><strong>• Multi-drop mode</strong> shows three light rays refracting from three raindrops at different altitudes. The color you see depends on the angle of refraction.</p>
<p><strong>• Single-drop mode </strong>shows the path inside one drop. Change from primary to secondary to see how the light takes a different path for each rainbow. A secondary rainbow is reflected twice, so it&#8217;s dimmer.</p>
<p>DRAG YOUR OBJECTS:<br />
<strong>• Drag the sun-like object</strong> (top and right side) to change the angle of the light rays. This changes the time of day.<br />
<strong>• Drag the humanoid object</strong> to see how distance from the rain affects rainbow<br />
location in the sky.<br />
<strong>• In multi-drop mode, drag raindrops</strong> up and down to see how altitude affects viewing on the ground.</p>
<div id="relateds">
<p>
Applet and illustrations copyright (C) 2003 Tom Whittaker, S.V. Medaris, and Steve Ackerman. The Motion-W® and Bucky Badger® logos are trademarks of the University of Wisconsin-Madison.
</p>
</div>
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