<?xml version='1.0' encoding='UTF-8'?><?xml-stylesheet href="http://www.blogger.com/styles/atom.css" type="text/css"?><feed xmlns='http://www.w3.org/2005/Atom' xmlns:openSearch='http://a9.com/-/spec/opensearchrss/1.0/' xmlns:georss='http://www.georss.org/georss' xmlns:gd='http://schemas.google.com/g/2005' xmlns:thr='http://purl.org/syndication/thread/1.0'><id>tag:blogger.com,1999:blog-7963407950078253219</id><updated>2011-11-01T10:16:22.012+05:00</updated><title type='text'>ARC98</title><subtitle type='html'></subtitle><link rel='http://schemas.google.com/g/2005#feed' type='application/atom+xml' href='http://arc98.blogspot.com/feeds/posts/default'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/7963407950078253219/posts/default?max-results=100'/><link rel='alternate' type='text/html' href='http://arc98.blogspot.com/'/><link rel='hub' href='http://pubsubhubbub.appspot.com/'/><author><name>Abdur Raheem</name><uri>http://www.blogger.com/profile/06278176155696104371</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><generator version='7.00' uri='http://www.blogger.com'>Blogger</generator><openSearch:totalResults>1</openSearch:totalResults><openSearch:startIndex>1</openSearch:startIndex><openSearch:itemsPerPage>100</openSearch:itemsPerPage><entry><id>tag:blogger.com,1999:blog-7963407950078253219.post-4501179351044992324</id><published>2011-10-03T19:52:00.004+05:00</published><updated>2011-11-01T10:16:22.041+05:00</updated><title type='text'>The three types of clouds</title><content type='html'>&lt;div dir="ltr" style="text-align: left;" trbidi="on"&gt;&lt;span style="color: white; font-size: large;"&gt;There are three types of clouds.&lt;/span&gt;&lt;br /&gt;&lt;strong&gt;&lt;span style="color: white; font-size: large;"&gt;Cirrus clouds:&lt;/span&gt;&lt;/strong&gt;&lt;br /&gt;&lt;span style="color: white; font-size: large;"&gt;Cirrus clouds (&lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/List_of_cloud_types" title="List of cloud types"&gt;&lt;span style="color: white; font-size: large;"&gt;cloud classification&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt; symbol: Ci) are &lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/Cloud" title="Cloud"&gt;&lt;span style="color: white; font-size: large;"&gt;atmospheric clouds&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt; generally characterized by thin, wispy strands, giving them their name from the &lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/Latin" title="Latin"&gt;&lt;span style="color: white; font-size: large;"&gt;Latin&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt; word &lt;i&gt;cirrus&lt;/i&gt; meaning a ringlet or curling lock of hair.The strands of cloud sometimes appear in tufts of a distinctive form referred to by the common name of &lt;i&gt;mares' tails&lt;/i&gt;.&lt;/span&gt;&lt;br /&gt;&lt;span style="color: white; font-size: large;"&gt;Cirrus clouds generally appear white or light grey in color. They form when water vapor undergoes &lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/Deposition_(phase_transition)" title="Deposition (phase transition)"&gt;&lt;span style="color: white; font-size: large;"&gt;deposition&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt; at altitudes above 5,000&amp;nbsp;m (16,500&amp;nbsp;ft) in temperate regions and above 6,100&amp;nbsp;m (20,000&amp;nbsp;ft) in tropical regions.&lt;/span&gt;&lt;br /&gt;&lt;span style="color: white;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;br /&gt;&lt;div class="thumbcaption"&gt;&lt;div class="magnify"&gt;&lt;span style="color: white;"&gt;&lt;img src="http://upload.wikimedia.org/wikipedia/commons/thumb/2/2e/CirrusField-color.jpg/320px-CirrusField-color.jpg" /&gt;&lt;/span&gt;&lt;a class="internal" href="http://en.wikipedia.org/wiki/File:CirrusField-color.jpg" title="Enlarge"&gt;&lt;/a&gt;&lt;/div&gt;&lt;span style="color: white;"&gt;A sky filled with many types of cirrus clouds&lt;/span&gt;&lt;/div&gt;&lt;span style="color: white;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;br /&gt;&lt;strong&gt;&lt;span style="color: white; font-size: large;"&gt;Stratrus clouds:&lt;/span&gt;&lt;/strong&gt;&lt;br /&gt;&lt;span style="color: white; font-size: large;"&gt;A &lt;b&gt;stratus cloud&lt;/b&gt; (St) is a &lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/Cloud" title="Cloud"&gt;&lt;span style="color: white; font-size: large;"&gt;cloud&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt; belonging to a class characterized by horizontal layering with a uniform base, as opposed to &lt;i&gt;convective clouds&lt;/i&gt; that are as tall or taller than wide (these are termed &lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/Cumulus_cloud" title="Cumulus cloud"&gt;&lt;span style="color: white; font-size: large;"&gt;cumulus clouds&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt;). More specifically, the term &lt;i&gt;stratus&lt;/i&gt; is used to describe flat, hazy, featureless clouds of low altitude varying in color from dark gray to nearly white. Stratus clouds may produce a light drizzle or snow. A "cloudy day" usually features a sky filled with stratus clouds obscuring the disk of the &lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/Sun" title="Sun"&gt;&lt;span style="color: white; font-size: large;"&gt;sun&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt;. These clouds are essentially above-ground &lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/Fog" title="Fog"&gt;&lt;span style="color: white; font-size: large;"&gt;fog&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt; formed either through the lifting of morning fog or when cold air moves at low altitudes over a region.&lt;/span&gt;&lt;br /&gt;&lt;a class="image" href="http://en.wikipedia.org/wiki/File:Stratus-Opacus-Uniformis.jpg" title="Stratus opacus uniformis"&gt;&lt;span style="color: white;"&gt;&lt;img alt="Stratus opacus uniformis" height="208px" src="http://upload.wikimedia.org/wikipedia/commons/thumb/d/d1/Stratus-Opacus-Uniformis.jpg/300px-Stratus-Opacus-Uniformis.jpg" width="300px" /&gt;&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;span style="color: white;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;br /&gt;&lt;strong&gt;&lt;span style="color: white; font-size: large;"&gt;Cumuluss clouds:&lt;/span&gt;&lt;/strong&gt;&lt;br /&gt;&lt;span style="color: white; font-size: large;"&gt;Cumulus clouds are a type of &lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/Cloud" title="Cloud"&gt;&lt;span style="color: white; font-size: large;"&gt;cloud&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt; with noticeable vertical development and clearly defined edges. &lt;i&gt;Cumulus&lt;/i&gt; means "heap" or "pile" in &lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/Latin" title="Latin"&gt;&lt;span style="color: white; font-size: large;"&gt;Latin&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt;. They are often described as "puffy" or "cotton-like" in appearance. Cumulus clouds may appear alone, in lines, or in clusters. Cumulus clouds are often precursors of other types of &lt;/span&gt;&lt;a class="mw-redirect" href="http://en.wikipedia.org/wiki/Clouds" title="Clouds"&gt;&lt;span style="color: white; font-size: large;"&gt;clouds&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt;, such as &lt;/span&gt;&lt;a class="mw-redirect" href="http://en.wikipedia.org/wiki/Cumulonimbus" title="Cumulonimbus"&gt;&lt;span style="color: white; font-size: large;"&gt;cumulonimbus&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt;, when influenced by weather factors such as &lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/Atmospheric_instability" title="Atmospheric instability"&gt;&lt;span style="color: white; font-size: large;"&gt;instability&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt;, moisture, and temperature gradient. Cumulus clouds are part of the larger category of &lt;i&gt;cumuliform clouds&lt;/i&gt;, which include cumulus, &lt;/span&gt;&lt;a class="mw-redirect" href="http://en.wikipedia.org/wiki/Cumulus_congestus" title="Cumulus congestus"&gt;&lt;span style="color: white; font-size: large;"&gt;cumulus congestus&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt;, and &lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/Cumulonimbus_cloud" title="Cumulonimbus cloud"&gt;&lt;span style="color: white; font-size: large;"&gt;cumulonimbus clouds&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt;, among others.&lt;sup class="reference" id="cite_ref-0"&gt;&lt;a href="http://en.wikipedia.org/wiki/Cumulus_cloud#cite_note-0"&gt;[1]&lt;/a&gt;&lt;/sup&gt; The most intense cumulus and cumulonimbus clouds may be associated with &lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/Severe_weather" title="Severe weather"&gt;&lt;span style="color: white; font-size: large;"&gt;severe weather&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt; phenomena such as &lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/Hail" title="Hail"&gt;&lt;span style="color: white; font-size: large;"&gt;hail&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt;, &lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/Waterspout" title="Waterspout"&gt;&lt;span style="color: white; font-size: large;"&gt;waterspouts&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt; and &lt;/span&gt;&lt;a href="http://en.wikipedia.org/wiki/Tornado" title="Tornado"&gt;&lt;span style="color: white; font-size: large;"&gt;tornadoes&lt;/span&gt;&lt;/a&gt;&lt;span style="color: white; font-size: large;"&gt;.&lt;/span&gt;&lt;br /&gt;&lt;a class="image" href="http://en.wikipedia.org/wiki/File:GoldenMedows.jpg" title="{{{image name}}}"&gt;&lt;span style="color: white;"&gt;&lt;img alt="{{{image name}}}" height="225px" src="http://upload.wikimedia.org/wikipedia/commons/thumb/3/3c/GoldenMedows.jpg/300px-GoldenMedows.jpg" width="300px" /&gt;&lt;/span&gt;&lt;/a&gt;&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/7963407950078253219-4501179351044992324?l=arc98.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://arc98.blogspot.com/feeds/4501179351044992324/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://arc98.blogspot.com/2011/10/my-first-blog.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/7963407950078253219/posts/default/4501179351044992324'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/7963407950078253219/posts/default/4501179351044992324'/><link rel='alternate' type='text/html' href='http://arc98.blogspot.com/2011/10/my-first-blog.html' title='The three types of clouds'/><author><name>Abdur Raheem</name><uri>http://www.blogger.com/profile/06278176155696104371</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry></feed>
