Comparing Wind Speeds on the North Sea Coast and Offshore
As part of the objective to describe the wind climate of the North Sea and the coastal zone, specifically with regard to wind energy applications, we study the observations of two meteorological stations on the North Sea coast: Hoek van Holland (HVH) and Umuiden (UM). Statistical analysis of the 8-y...
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Veröffentlicht in: | Wind engineering 1997-01, Vol.21 (5), p.307-318 |
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description | As part of the objective to describe the wind climate of the North Sea and the coastal zone, specifically with regard to wind energy applications, we study the observations of two meteorological stations on the North Sea coast: Hoek van Holland (HVH) and Umuiden (UM). Statistical analysis of the 8-year datasets shows that the mean wind speeds are 7.8 m/s (at 18.5 m height) for UM, and 7.6 m/s (at 15.0 m height) for HVH, respectively. The coastal observations are compared to the observations of three offshore platforms in the North Sea analysed in earlier work. It is found that diurnal variations are very similar in autumn and winter, but differ in spring and summer. Furthermore, wind speeds with fetch over sea do behave very similarly at the coastal stations and offshore platforms. It is shown that the effects of thermal circulation leading to the sea breeze are distinctly present, at least up to 30 km offshore. These effects can be attributed to relatively low wind speeds (less than 7 m/s at 10 m height), and manifest themselves as a shift, on average, of wind directions from easterly to westerly directions during the day. Higher wind speeds (more than 7 m/s), most relevant for wind energy applications, compare well at coastal stations and offshore platforms. |
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Statistical analysis of the 8-year datasets shows that the mean wind speeds are 7.8 m/s (at 18.5 m height) for UM, and 7.6 m/s (at 15.0 m height) for HVH, respectively. The coastal observations are compared to the observations of three offshore platforms in the North Sea analysed in earlier work. It is found that diurnal variations are very similar in autumn and winter, but differ in spring and summer. Furthermore, wind speeds with fetch over sea do behave very similarly at the coastal stations and offshore platforms. It is shown that the effects of thermal circulation leading to the sea breeze are distinctly present, at least up to 30 km offshore. These effects can be attributed to relatively low wind speeds (less than 7 m/s at 10 m height), and manifest themselves as a shift, on average, of wind directions from easterly to westerly directions during the day. Higher wind speeds (more than 7 m/s), most relevant for wind energy applications, compare well at coastal stations and offshore platforms.</description><identifier>ISSN: 0309-524X</identifier><identifier>EISSN: 2048-402X</identifier><language>eng</language><publisher>Multi-Science Publishing Company</publisher><subject>Coasts ; Land ; Offshore platforms ; Sea breezes ; Sea water ; Seas ; Seasons ; Wind ; Wind power ; Wind velocity</subject><ispartof>Wind engineering, 1997-01, Vol.21 (5), p.307-318</ispartof><rights>1997 Multi-Science Publishing Company</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/43749653$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/43749653$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,776,780,799,57995,58228</link.rule.ids></links><search><creatorcontrib>Coelingh, J.P.</creatorcontrib><creatorcontrib>van Wijk, A.J.M.</creatorcontrib><creatorcontrib>Holtslag, A.A.M.</creatorcontrib><title>Comparing Wind Speeds on the North Sea Coast and Offshore</title><title>Wind engineering</title><description>As part of the objective to describe the wind climate of the North Sea and the coastal zone, specifically with regard to wind energy applications, we study the observations of two meteorological stations on the North Sea coast: Hoek van Holland (HVH) and Umuiden (UM). Statistical analysis of the 8-year datasets shows that the mean wind speeds are 7.8 m/s (at 18.5 m height) for UM, and 7.6 m/s (at 15.0 m height) for HVH, respectively. The coastal observations are compared to the observations of three offshore platforms in the North Sea analysed in earlier work. It is found that diurnal variations are very similar in autumn and winter, but differ in spring and summer. Furthermore, wind speeds with fetch over sea do behave very similarly at the coastal stations and offshore platforms. It is shown that the effects of thermal circulation leading to the sea breeze are distinctly present, at least up to 30 km offshore. These effects can be attributed to relatively low wind speeds (less than 7 m/s at 10 m height), and manifest themselves as a shift, on average, of wind directions from easterly to westerly directions during the day. Higher wind speeds (more than 7 m/s), most relevant for wind energy applications, compare well at coastal stations and offshore platforms.</description><subject>Coasts</subject><subject>Land</subject><subject>Offshore platforms</subject><subject>Sea breezes</subject><subject>Sea water</subject><subject>Seas</subject><subject>Seasons</subject><subject>Wind</subject><subject>Wind power</subject><subject>Wind velocity</subject><issn>0309-524X</issn><issn>2048-402X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1997</creationdate><recordtype>article</recordtype><sourceid/><recordid>eNotjEtqwzAUAEVpoG7SIxR0AYM-T1K0LKY_CM0igWYXnq2n2qaxjORNb99Au5nZDHPDKiVgW4NQp1tWCS18bRSc7th9KaMQEqSEivkmXWbMw_TFP4cp8MNMFApPE1964h8pLz0_EPImYVk4Xot9jKVPmTZsFfG70MO_1-z48nxs3urd_vW9edrVoxdL7TqKZFBi2ykQTgYggk5AVGitxiuUtGQstkIhtqGVYCF654Nz2wBGr9nj33YsS8rnOQ8XzD9n0A68NVr_AoGhQOA</recordid><startdate>19970101</startdate><enddate>19970101</enddate><creator>Coelingh, J.P.</creator><creator>van Wijk, A.J.M.</creator><creator>Holtslag, A.A.M.</creator><general>Multi-Science Publishing Company</general><scope/></search><sort><creationdate>19970101</creationdate><title>Comparing Wind Speeds on the North Sea Coast and Offshore</title><author>Coelingh, J.P. ; van Wijk, A.J.M. ; Holtslag, A.A.M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-j90t-7cefe5a1abc24071d4ee4c04f2a663aa66216e56ab02aabdb1464f979d778d453</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1997</creationdate><topic>Coasts</topic><topic>Land</topic><topic>Offshore platforms</topic><topic>Sea breezes</topic><topic>Sea water</topic><topic>Seas</topic><topic>Seasons</topic><topic>Wind</topic><topic>Wind power</topic><topic>Wind velocity</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Coelingh, J.P.</creatorcontrib><creatorcontrib>van Wijk, A.J.M.</creatorcontrib><creatorcontrib>Holtslag, A.A.M.</creatorcontrib><jtitle>Wind engineering</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Coelingh, J.P.</au><au>van Wijk, A.J.M.</au><au>Holtslag, A.A.M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Comparing Wind Speeds on the North Sea Coast and Offshore</atitle><jtitle>Wind engineering</jtitle><date>1997-01-01</date><risdate>1997</risdate><volume>21</volume><issue>5</issue><spage>307</spage><epage>318</epage><pages>307-318</pages><issn>0309-524X</issn><eissn>2048-402X</eissn><abstract>As part of the objective to describe the wind climate of the North Sea and the coastal zone, specifically with regard to wind energy applications, we study the observations of two meteorological stations on the North Sea coast: Hoek van Holland (HVH) and Umuiden (UM). Statistical analysis of the 8-year datasets shows that the mean wind speeds are 7.8 m/s (at 18.5 m height) for UM, and 7.6 m/s (at 15.0 m height) for HVH, respectively. The coastal observations are compared to the observations of three offshore platforms in the North Sea analysed in earlier work. It is found that diurnal variations are very similar in autumn and winter, but differ in spring and summer. Furthermore, wind speeds with fetch over sea do behave very similarly at the coastal stations and offshore platforms. It is shown that the effects of thermal circulation leading to the sea breeze are distinctly present, at least up to 30 km offshore. These effects can be attributed to relatively low wind speeds (less than 7 m/s at 10 m height), and manifest themselves as a shift, on average, of wind directions from easterly to westerly directions during the day. Higher wind speeds (more than 7 m/s), most relevant for wind energy applications, compare well at coastal stations and offshore platforms.</abstract><pub>Multi-Science Publishing Company</pub><tpages>12</tpages></addata></record> |
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subjects | Coasts Land Offshore platforms Sea breezes Sea water Seas Seasons Wind Wind power Wind velocity |
title | Comparing Wind Speeds on the North Sea Coast and Offshore |
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