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	<title>Comments on: Icicles and Watersheds Part 2:  How much water flows off the top of two houses</title>
	<atom:link href="http://blog.globe.gov/sciblog/2008/01/14/icicles-and-watersheds-part-2-how-much-water-flows-off-the-top-of-two-houses/feed/" rel="self" type="application/rss+xml" />
	<link>http://blog.globe.gov/sciblog/2008/01/14/icicles-and-watersheds-part-2-how-much-water-flows-off-the-top-of-two-houses/?utm_source=rss&#038;utm_medium=rss&#038;utm_campaign=icicles-and-watersheds-part-2-how-much-water-flows-off-the-top-of-two-houses</link>
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		<title>By: peggy</title>
		<link>http://blog.globe.gov/sciblog/2008/01/14/icicles-and-watersheds-part-2-how-much-water-flows-off-the-top-of-two-houses/comment-page-1/#comment-1910</link>
		<dc:creator>peggy</dc:creator>
		<pubDate>Sat, 19 Jan 2008 18:38:19 +0000</pubDate>
		<guid isPermaLink="false">http://www.globe.gov/fsl/scientistsblog/?p=85#comment-1910</guid>
		<description><![CDATA[The major effect of the pitch of the roof is affecting how much water falls on it.  So a very shallow roof would have more rain on it for the same area.

Suppose you had two roofs with equal &quot;footprints&quot; so that they received the same amount of rain.  In steady state the flow off the roofs would be equal.

But if you rolled a marble off the longer, steeper roof, it would certainly be going faster.

I suppose the key is that the roofs would have the same flow off of them for steady state, but not for an &quot;impulse&quot;.]]></description>
		<content:encoded><![CDATA[<p>The major effect of the pitch of the roof is affecting how much water falls on it.  So a very shallow roof would have more rain on it for the same area.</p>
<p>Suppose you had two roofs with equal &#8220;footprints&#8221; so that they received the same amount of rain.  In steady state the flow off the roofs would be equal.</p>
<p>But if you rolled a marble off the longer, steeper roof, it would certainly be going faster.</p>
<p>I suppose the key is that the roofs would have the same flow off of them for steady state, but not for an &#8220;impulse&#8221;.</p>
]]></content:encoded>
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		<title>By: jga</title>
		<link>http://blog.globe.gov/sciblog/2008/01/14/icicles-and-watersheds-part-2-how-much-water-flows-off-the-top-of-two-houses/comment-page-1/#comment-1891</link>
		<dc:creator>jga</dc:creator>
		<pubDate>Wed, 16 Jan 2008 22:43:30 +0000</pubDate>
		<guid isPermaLink="false">http://www.globe.gov/fsl/scientistsblog/?p=85#comment-1891</guid>
		<description><![CDATA[I&#039;m just curious, wouldn&#039;t the pitch of the roof also impact the rate at which the water runs off? For example, using the roof sheds in your Fig. 3 and assuming a constant height for the attic crawl space, say 2m, the angle of your roof would be much less than for the imaginary roof. As a result, I would expect the water to flow off it more slowly. This would also affect the icicles you mentioned in a prior blog. If your home has a shallow pitch compared to your neighbors, would not more of it be apt to freeze forming longer and wider icicles?]]></description>
		<content:encoded><![CDATA[<p>I&#8217;m just curious, wouldn&#8217;t the pitch of the roof also impact the rate at which the water runs off? For example, using the roof sheds in your Fig. 3 and assuming a constant height for the attic crawl space, say 2m, the angle of your roof would be much less than for the imaginary roof. As a result, I would expect the water to flow off it more slowly. This would also affect the icicles you mentioned in a prior blog. If your home has a shallow pitch compared to your neighbors, would not more of it be apt to freeze forming longer and wider icicles?</p>
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