<?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-1978145992618371859</id><updated>2012-02-16T19:48:11.790-08:00</updated><category term='MSL'/><category term='Geoid'/><category term='Gravity'/><title type='text'>Dynamic Meteorology</title><subtitle type='html'></subtitle><link rel='http://schemas.google.com/g/2005#feed' type='application/atom+xml' href='http://profww-dynamicmeteorology.blogspot.com/feeds/posts/default'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1978145992618371859/posts/default?max-results=100'/><link rel='alternate' type='text/html' href='http://profww-dynamicmeteorology.blogspot.com/'/><link rel='hub' href='http://pubsubhubbub.appspot.com/'/><author><name>ProfWW</name><uri>http://www.blogger.com/profile/13450023839382238408</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='24' src='http://apollo.lsc.vsc.edu/~wintelsw/images/3053557_large.jpg'/></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-1978145992618371859.post-4177946016647057096</id><published>2009-05-01T10:39:00.000-07:00</published><updated>2009-05-01T13:47:00.990-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='Geoid'/><category scheme='http://www.blogger.com/atom/ns#' term='MSL'/><category scheme='http://www.blogger.com/atom/ns#' term='Gravity'/><title type='text'>Mean sea-level pressure (MSL)</title><content type='html'>Some definitions&lt;br /&gt;&lt;ul&gt;&lt;li&gt;&lt;a href="http://amsglossary.allenpress.com/glossary/search?id=equipotential-surface1"&gt;&lt;b&gt;&lt;span style="color: rgb(0, 113, 119);"&gt;equipotential surface&lt;/span&gt;&lt;/b&gt;&lt;/a&gt;: A surface defined by the function  &lt;center&gt;&lt;img src="http://amsglossary.allenpress.com/images/amsg/ams2001glos-Ee52.gif" /&gt;&lt;/center&gt; where Φ is the &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=potential1"&gt;potential&lt;/a&gt; function associated with any &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=field1"&gt;field&lt;/a&gt; that can be written  &lt;center&gt;&lt;img src="http://amsglossary.allenpress.com/images/amsg/ams2001glos-Ee53.gif" /&gt;&lt;/center&gt; Examples are gravitational, electrostatic, and magnetostatic equipotential surfaces.  &lt;/li&gt;&lt;li&gt;&lt;b&gt;&lt;span style="color:#007177;"&gt;&lt;a href="http://amsglossary.allenpress.com/glossary/search?id=sea-level1"&gt;sea level&lt;/a&gt;&lt;/span&gt;&lt;/b&gt;—The level of the sea after averaging out the short-term variations due to &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=wind1"&gt;wind&lt;/a&gt; waves.&lt;/li&gt;&lt;li&gt;&lt;a href="http://amsglossary.allenpress.com/glossary/search?id=mean-sea-level1"&gt;&lt;b&gt;&lt;span style="color:#007177;"&gt;mean sea level&lt;/span&gt;&lt;/b&gt;&lt;/a&gt;—(Abbreviated MSL; popularly called sea level.) The &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=arithmetic-mean1"&gt;arithmetic mean&lt;/a&gt; of hourly  heights observed over some specified period. In the United States, mean sea level is defined as the mean height of the surface of the sea for  all stages of the &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=tide1"&gt;tide&lt;/a&gt; over a 19-year period. Selected values of mean sea level serve as the sea level  &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=datum1"&gt;datum&lt;/a&gt; for all &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=elevation1"&gt;elevation&lt;/a&gt; surveys in the United States. In meteorology, mean sea level is used as the reference surface for all altitudes in upper-atmospheric work; in aviation it is the level above which &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=altitude1"&gt;altitude&lt;/a&gt; is measured by a &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=pressure-altimeter1"&gt;pressure altimeter&lt;/a&gt;.&lt;/li&gt;&lt;li&gt;&lt;a href="http://amsglossary.allenpress.com/glossary/search?id=geopotential-surface1"&gt;&lt;b&gt;&lt;span style="color: rgb(0, 113, 119);"&gt;geopotential &lt;/span&gt;&lt;/b&gt; &lt;b&gt;&lt;span style="color:#007177;"&gt;&lt;/span&gt;&lt;/b&gt;—The &lt;/a&gt;&lt;a href="http://amsglossary.allenpress.com/glossary/search?id=potential-energy1"&gt;potential energy&lt;/a&gt; of a unit mass relative to &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=sea-level1"&gt;sea level&lt;/a&gt;, numerically equal to the  &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=work1"&gt;work&lt;/a&gt; that would be done in lifting the unit mass from sea level to the height at which the mass is located; commonly expressed in terms of &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=dynamic-height1"&gt;dynamic height&lt;/a&gt; or &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=geopotential-height1"&gt;geopotential height&lt;/a&gt;. &lt;table&gt;&lt;tbody&gt;&lt;tr&gt;&lt;td valign="top"&gt;&lt;br /&gt;&lt;/td&gt;&lt;td&gt;&lt;dd&gt;The geopotential Φ at height &lt;i&gt;z&lt;/i&gt; is given mathematically by the expression  &lt;center&gt;&lt;img src="http://amsglossary.allenpress.com/images/amsg/ams2001glos-Ge16.gif" /&gt;&lt;/center&gt; where &lt;i&gt;g&lt;/i&gt; is the &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=acceleration-of-gravity1"&gt;acceleration of gravity&lt;/a&gt;.  &lt;/dd&gt;&lt;/td&gt;&lt;/tr&gt;&lt;/tbody&gt;&lt;/table&gt;&lt;a href="http://amsglossary.allenpress.com/glossary/search?id=geopotential-surface1"&gt;&lt;b&gt;&lt;span style="color:#007177;"&gt;geopotential&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span style="color: rgb(0, 113, 119);"&gt; surface&lt;/span&gt;&lt;/b&gt;&lt;/a&gt;—(Also called &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=equipotential-surface1"&gt;equipotential surface&lt;/a&gt;, level surface.) A surface of constant &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=geopotential1"&gt;geopotential&lt;/a&gt;,  that is, a surface along which a &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=parcel1"&gt;parcel&lt;/a&gt; of air could move without undergoing any changes  in its &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=potential-energy1"&gt;potential energy&lt;/a&gt;. &lt;/li&gt;&lt;li&gt;&lt;a href="http://amsglossary.allenpress.com/glossary/search?p=1&amp;amp;query=geoid&amp;amp;submit=Search"&gt;&lt;b&gt;&lt;span style="color:#007177;"&gt;geoid&lt;/span&gt;&lt;/b&gt;&lt;/a&gt;—The particular &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=geopotential-surface1"&gt;geopotential surface&lt;/a&gt; that most nearly coincides with the mean level of the  oceans of the earth. For mapping purposes it is customary to use an ellipsoid of revolution as an adequate and convenient approximation to the geoid. The actual geoid can  depart from a best-fitting sphere in places by as much as 100 m.  &lt;/li&gt;&lt;li&gt;&lt;b&gt;&lt;span style="color:#007177;"&gt;atmospheric tide&lt;/span&gt;&lt;/b&gt;— (Also called atmospheric oscillation.)  An atmospheric motion of the &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=scale1"&gt;scale&lt;/a&gt; of the earth, in which vertical accelerations are neglected (but  &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=compressibility1"&gt;compressibility&lt;/a&gt; is taken into account).  Both the sun and moon produce atmospheric tides. The &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=harmonic1"&gt;&lt;/a&gt;12-hour or semidiurnal  &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=solar-atmospheric-tide1"&gt;solar atmospheric tide&lt;/a&gt; is both &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=gravitational-tide1"&gt;gravitational &lt;/a&gt;and &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=thermal-tide1"&gt;thermal &lt;/a&gt;and has the greatest &lt;a href="http://amsglossary.allenpress.com/glossary/search?id=amplitude1"&gt;amplitude&lt;/a&gt;. It is defined as &lt;/li&gt;&lt;/ul&gt;Source:&lt;br /&gt;&lt;ul&gt;&lt;li&gt;AMS, cited 2009. &lt;i&gt;&lt;a href="http://amsglossary.allenpress.com/glossary"&gt;Glossary of Meteorology&lt;/a&gt;.&lt;/i&gt;&lt;/li&gt;&lt;/ul&gt;&lt;br /&gt;Articles:&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;&lt;span style="font-size:100%;"&gt;&lt;span class="editor"&gt;Fraczek, &lt;/span&gt;&lt;/span&gt;&lt;span style="font-size:100%;"&gt;&lt;span class="editor"&gt;Witold/&lt;/span&gt;&lt;/span&gt;&lt;a href="http://www.esri.com/news/arcuser/"&gt;&lt;span&gt;&lt;span style="font-size:100%;"&gt;&lt;span class="editor"&gt;ESRI&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span style="font-size:100%;"&gt;&lt;span class="editor"&gt;- Arcuser online &lt;/span&gt;&lt;/span&gt;&lt;/a&gt;&lt;span&gt;&lt;span style="font-size:100%;"&gt;&lt;span class="editor"&gt;, cited 2009. &lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;a href="http://www.esri.com/news/arcuser/0703/geoid1of3.html"&gt;&lt;span style="font-size:100%;"&gt;Mean Sea Level, GPS, and the Geoid&lt;/span&gt;&lt;/a&gt;&lt;span style="font-size:100%;"&gt;&lt;span class="editor"&gt;,  2003.&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/li&gt;&lt;/ul&gt;&lt;h2 style="font-weight: normal;"&gt; &lt;/h2&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1978145992618371859-4177946016647057096?l=profww-dynamicmeteorology.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://profww-dynamicmeteorology.blogspot.com/feeds/4177946016647057096/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://profww-dynamicmeteorology.blogspot.com/2009/05/mean-sea-level-pressure-msl.html#comment-form' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1978145992618371859/posts/default/4177946016647057096'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1978145992618371859/posts/default/4177946016647057096'/><link rel='alternate' type='text/html' href='http://profww-dynamicmeteorology.blogspot.com/2009/05/mean-sea-level-pressure-msl.html' title='Mean sea-level pressure (MSL)'/><author><name>ProfWW</name><uri>http://www.blogger.com/profile/13450023839382238408</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='24' src='http://apollo.lsc.vsc.edu/~wintelsw/images/3053557_large.jpg'/></author><thr:total>0</thr:total></entry></feed>
