Cup Anemometer Response to Fluctuating Wind Speeds

An investigation is made into cup anemometer response to fluctuating wind speeds. The anemometer overruns under these conditions and the percentage overrun depends on the wind speed, and the frequency and amplitude of the fluctuations. An estimate of this overrun in the real atmosphere, i.e., the &q...

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Veröffentlicht in:	Journal of applied meteorology (1962) 1972-08, Vol.11 (5), p.843-848
1. Verfasser:	Hyson, P.
Format:	Artikel
Sprache:	eng
Schlagworte:	Acceleration Anemometers Atmospherics Average speed Meteors Percentages Time constants Turbulence Wind tunnels Wind velocity
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container_title	Journal of applied meteorology (1962)
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description	An investigation is made into cup anemometer response to fluctuating wind speeds. The anemometer overruns under these conditions and the percentage overrun depends on the wind speed, and the frequency and amplitude of the fluctuations. An estimate of this overrun in the real atmosphere, i.e., the "u error", is made and found to be of the order of 1% for a typical micrometeorological anemometer.
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The anemometer overruns under these conditions and the percentage overrun depends on the wind speed, and the frequency and amplitude of the fluctuations. An estimate of this overrun in the real atmosphere, i.e., the "u error", is made and found to be of the order of 1% for a typical micrometeorological anemometer.</description><subject>Acceleration</subject><subject>Anemometers</subject><subject>Atmospherics</subject><subject>Average speed</subject><subject>Meteors</subject><subject>Percentages</subject><subject>Time constants</subject><subject>Turbulence</subject><subject>Wind tunnels</subject><subject>Wind velocity</subject><issn>0021-8952</issn><issn>2163-534X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1972</creationdate><recordtype>article</recordtype><sourceid/><recordid>eNpjYuA0MjQz1jU1NolgYeA0MDAy1LWwNDXiYOAqLs4Ccs1MzMw4GYycSwsUHPNSc_NzU0tSixSCUosL8vOKUxVK8hXcckqTS0oTSzLz0hXCM_NSFIILUlNTinkYWNMSc4pTeaE0N4Osm2uIs4duVnFJflF8QVFmbmJRZbyRmaG5qYmppTEheQA6ETDJ</recordid><startdate>19720801</startdate><enddate>19720801</enddate><creator>Hyson, P.</creator><general>American Meteorological Society</general><scope/></search><sort><creationdate>19720801</creationdate><title>Cup Anemometer Response to Fluctuating Wind Speeds</title><author>Hyson, P.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-jstor_primary_261754593</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1972</creationdate><topic>Acceleration</topic><topic>Anemometers</topic><topic>Atmospherics</topic><topic>Average speed</topic><topic>Meteors</topic><topic>Percentages</topic><topic>Time constants</topic><topic>Turbulence</topic><topic>Wind tunnels</topic><topic>Wind velocity</topic><toplevel>online_resources</toplevel><creatorcontrib>Hyson, P.</creatorcontrib><jtitle>Journal of applied meteorology (1962)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Hyson, P.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Cup Anemometer Response to Fluctuating Wind Speeds</atitle><jtitle>Journal of applied meteorology (1962)</jtitle><date>1972-08-01</date><risdate>1972</risdate><volume>11</volume><issue>5</issue><spage>843</spage><epage>848</epage><pages>843-848</pages><issn>0021-8952</issn><eissn>2163-534X</eissn><abstract>An investigation is made into cup anemometer response to fluctuating wind speeds. The anemometer overruns under these conditions and the percentage overrun depends on the wind speed, and the frequency and amplitude of the fluctuations. An estimate of this overrun in the real atmosphere, i.e., the "u error", is made and found to be of the order of 1% for a typical micrometeorological anemometer.</abstract><pub>American Meteorological Society</pub></addata></record>
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language	eng
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source	Jstor Complete Legacy; Alma/SFX Local Collection
subjects	Acceleration Anemometers Atmospherics Average speed Meteors Percentages Time constants Turbulence Wind tunnels Wind velocity
title	Cup Anemometer Response to Fluctuating Wind Speeds
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