Loading…
The Frøya database and maritime boundary layer wind description
High-quality maritime wind-turbulence data obtained at exposed sites on the western coast of Norway during gale and stormy conditions are described. With a resolution of 1 Hz, and a height range of 10–100 m, the database is most suitable for describing the wind structure of the maritime boundary lay...
Saved in:
| Published in: | Marine structures 2006-04, Vol.19 (2), p.173-192 |
|---|---|
| Main Authors: | , |
| Format: | Article |
| Language: | English |
| Subjects: | |
| Citations: | Items that this one cites Items that cite this one |
| Online Access: | Get full text |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| cited_by | cdi_FETCH-LOGICAL-c373t-4d5b82b8b4c7c123a28bd070f60973d5f35f7f82eae2f4cd661becfacd6b76723 |
|---|---|
| cites | cdi_FETCH-LOGICAL-c373t-4d5b82b8b4c7c123a28bd070f60973d5f35f7f82eae2f4cd661becfacd6b76723 |
| container_end_page | 192 |
| container_issue | 2 |
| container_start_page | 173 |
| container_title | Marine structures |
| container_volume | 19 |
| creator | Andersen, Odd Jan Løvseth, Jørgen |
| description | High-quality maritime wind-turbulence data obtained at exposed sites on the western coast of Norway during gale and stormy conditions are described. With a resolution of 1
Hz, and a height range of 10–100
m, the database is most suitable for describing the wind structure of the maritime boundary layer (MBL) with relevance for offshore compliant floating structures. The established description covers both static and dynamic wind, the latter with particular attention given to the low-frequency range 0.002–0.03
Hz (0.5–10
min). The relevance for and extrapolation to very strong wind speed design conditions has been emphasized.
The static description of wind is found to be consistent with the Charnock relation reflecting the interaction between wind and waves. A most important conclusion is reached for the one-point wind speed spectrum. The low-frequency range ( |
| doi_str_mv | 10.1016/j.marstruc.2006.07.003 |
| format | article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_29938834</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0951833906000542</els_id><sourcerecordid>29938834</sourcerecordid><originalsourceid>FETCH-LOGICAL-c373t-4d5b82b8b4c7c123a28bd070f60973d5f35f7f82eae2f4cd661becfacd6b76723</originalsourceid><addsrcrecordid>eNqFkM1OwzAQhC0EEqXwCigXuCX4J4mdW1FFAakSl3K2_LMWrtKk2Amob8adF8NVizhy2pV2ZlbzIXRNcEEwqe_WxUaFOITRFBTjusC8wJidoAkRnOUl4fgUTXBTkVww1pyjixjXGBNOCJmg2eoNskX4_tqpzKpBaRUhU53NUqYf_AYy3Y-dVWGXtWoHIfv06WghmuC3g--7S3TmVBvh6jin6HXxsJo_5cuXx-f5_TI3jLMhL22lBdVCl4YbQpmiQlvMsatxw5mtHKscd4KCAupKY-uaaDBOpU3zmlM2RbeH3G3o30eIg9z4aKBtVQf9GCVtGiYEK5OwPghN6GMM4OQ2-NRmJwmWe2ByLX-ByT0wiblMwJLx5vhBRaNaF1RnfPxzi6qqCGmSbnbQQar74SHIaDx0BqwPYAZpe__fqx_VL4Zd</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>29938834</pqid></control><display><type>article</type><title>The Frøya database and maritime boundary layer wind description</title><source>Elsevier ScienceDirect Freedom Collection 2023</source><creator>Andersen, Odd Jan ; Løvseth, Jørgen</creator><creatorcontrib>Andersen, Odd Jan ; Løvseth, Jørgen</creatorcontrib><description>High-quality maritime wind-turbulence data obtained at exposed sites on the western coast of Norway during gale and stormy conditions are described. With a resolution of 1
Hz, and a height range of 10–100
m, the database is most suitable for describing the wind structure of the maritime boundary layer (MBL) with relevance for offshore compliant floating structures. The established description covers both static and dynamic wind, the latter with particular attention given to the low-frequency range 0.002–0.03
Hz (0.5–10
min). The relevance for and extrapolation to very strong wind speed design conditions has been emphasized.
The static description of wind is found to be consistent with the Charnock relation reflecting the interaction between wind and waves. A most important conclusion is reached for the one-point wind speed spectrum. The low-frequency range (<0.01
Hz) is significantly more energetic than indicated by land-based studies. Concerning correlations, it is noteworthy that coherence for lateral separation is significantly lower than indicated by some other studies. Coherence for vertical separation is on the low side but in reasonable agreement with these studies. The data does not support a low-frequency asymptote for coherence different from 1.</description><identifier>ISSN: 0951-8339</identifier><identifier>EISSN: 1873-4170</identifier><identifier>DOI: 10.1016/j.marstruc.2006.07.003</identifier><language>eng</language><publisher>Oxford: Elsevier Ltd</publisher><subject>Applied sciences ; Buildings. Public works ; Climatology and bioclimatics for buildings ; Climatology. Bioclimatology. Climate change ; Dynamic wind ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Extreme wind loads ; Hydraulic constructions ; Maritime conditions ; Meteorology ; Offshore structure (platforms, tanks, etc.) ; Static wind</subject><ispartof>Marine structures, 2006-04, Vol.19 (2), p.173-192</ispartof><rights>2006</rights><rights>2007 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c373t-4d5b82b8b4c7c123a28bd070f60973d5f35f7f82eae2f4cd661becfacd6b76723</citedby><cites>FETCH-LOGICAL-c373t-4d5b82b8b4c7c123a28bd070f60973d5f35f7f82eae2f4cd661becfacd6b76723</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=18555119$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Andersen, Odd Jan</creatorcontrib><creatorcontrib>Løvseth, Jørgen</creatorcontrib><title>The Frøya database and maritime boundary layer wind description</title><title>Marine structures</title><description>High-quality maritime wind-turbulence data obtained at exposed sites on the western coast of Norway during gale and stormy conditions are described. With a resolution of 1
Hz, and a height range of 10–100
m, the database is most suitable for describing the wind structure of the maritime boundary layer (MBL) with relevance for offshore compliant floating structures. The established description covers both static and dynamic wind, the latter with particular attention given to the low-frequency range 0.002–0.03
Hz (0.5–10
min). The relevance for and extrapolation to very strong wind speed design conditions has been emphasized.
The static description of wind is found to be consistent with the Charnock relation reflecting the interaction between wind and waves. A most important conclusion is reached for the one-point wind speed spectrum. The low-frequency range (<0.01
Hz) is significantly more energetic than indicated by land-based studies. Concerning correlations, it is noteworthy that coherence for lateral separation is significantly lower than indicated by some other studies. Coherence for vertical separation is on the low side but in reasonable agreement with these studies. The data does not support a low-frequency asymptote for coherence different from 1.</description><subject>Applied sciences</subject><subject>Buildings. Public works</subject><subject>Climatology and bioclimatics for buildings</subject><subject>Climatology. Bioclimatology. Climate change</subject><subject>Dynamic wind</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Extreme wind loads</subject><subject>Hydraulic constructions</subject><subject>Maritime conditions</subject><subject>Meteorology</subject><subject>Offshore structure (platforms, tanks, etc.)</subject><subject>Static wind</subject><issn>0951-8339</issn><issn>1873-4170</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNqFkM1OwzAQhC0EEqXwCigXuCX4J4mdW1FFAakSl3K2_LMWrtKk2Amob8adF8NVizhy2pV2ZlbzIXRNcEEwqe_WxUaFOITRFBTjusC8wJidoAkRnOUl4fgUTXBTkVww1pyjixjXGBNOCJmg2eoNskX4_tqpzKpBaRUhU53NUqYf_AYy3Y-dVWGXtWoHIfv06WghmuC3g--7S3TmVBvh6jin6HXxsJo_5cuXx-f5_TI3jLMhL22lBdVCl4YbQpmiQlvMsatxw5mtHKscd4KCAupKY-uaaDBOpU3zmlM2RbeH3G3o30eIg9z4aKBtVQf9GCVtGiYEK5OwPghN6GMM4OQ2-NRmJwmWe2ByLX-ByT0wiblMwJLx5vhBRaNaF1RnfPxzi6qqCGmSbnbQQar74SHIaDx0BqwPYAZpe__fqx_VL4Zd</recordid><startdate>20060401</startdate><enddate>20060401</enddate><creator>Andersen, Odd Jan</creator><creator>Løvseth, Jørgen</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TB</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>20060401</creationdate><title>The Frøya database and maritime boundary layer wind description</title><author>Andersen, Odd Jan ; Løvseth, Jørgen</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c373t-4d5b82b8b4c7c123a28bd070f60973d5f35f7f82eae2f4cd661becfacd6b76723</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Applied sciences</topic><topic>Buildings. Public works</topic><topic>Climatology and bioclimatics for buildings</topic><topic>Climatology. Bioclimatology. Climate change</topic><topic>Dynamic wind</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Extreme wind loads</topic><topic>Hydraulic constructions</topic><topic>Maritime conditions</topic><topic>Meteorology</topic><topic>Offshore structure (platforms, tanks, etc.)</topic><topic>Static wind</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Andersen, Odd Jan</creatorcontrib><creatorcontrib>Løvseth, Jørgen</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Marine structures</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Andersen, Odd Jan</au><au>Løvseth, Jørgen</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Frøya database and maritime boundary layer wind description</atitle><jtitle>Marine structures</jtitle><date>2006-04-01</date><risdate>2006</risdate><volume>19</volume><issue>2</issue><spage>173</spage><epage>192</epage><pages>173-192</pages><issn>0951-8339</issn><eissn>1873-4170</eissn><abstract>High-quality maritime wind-turbulence data obtained at exposed sites on the western coast of Norway during gale and stormy conditions are described. With a resolution of 1
Hz, and a height range of 10–100
m, the database is most suitable for describing the wind structure of the maritime boundary layer (MBL) with relevance for offshore compliant floating structures. The established description covers both static and dynamic wind, the latter with particular attention given to the low-frequency range 0.002–0.03
Hz (0.5–10
min). The relevance for and extrapolation to very strong wind speed design conditions has been emphasized.
The static description of wind is found to be consistent with the Charnock relation reflecting the interaction between wind and waves. A most important conclusion is reached for the one-point wind speed spectrum. The low-frequency range (<0.01
Hz) is significantly more energetic than indicated by land-based studies. Concerning correlations, it is noteworthy that coherence for lateral separation is significantly lower than indicated by some other studies. Coherence for vertical separation is on the low side but in reasonable agreement with these studies. The data does not support a low-frequency asymptote for coherence different from 1.</abstract><cop>Oxford</cop><pub>Elsevier Ltd</pub><doi>10.1016/j.marstruc.2006.07.003</doi><tpages>20</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0951-8339 |
| ispartof | Marine structures, 2006-04, Vol.19 (2), p.173-192 |
| issn | 0951-8339 1873-4170 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_29938834 |
| source | Elsevier ScienceDirect Freedom Collection 2023 |
| subjects | Applied sciences Buildings. Public works Climatology and bioclimatics for buildings Climatology. Bioclimatology. Climate change Dynamic wind Earth, ocean, space Exact sciences and technology External geophysics Extreme wind loads Hydraulic constructions Maritime conditions Meteorology Offshore structure (platforms, tanks, etc.) Static wind |
| title | The Frøya database and maritime boundary layer wind description |
| url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-03-10T05%3A31%3A15IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=The%20Fr%C3%B8ya%20database%20and%20maritime%20boundary%20layer%20wind%20description&rft.jtitle=Marine%20structures&rft.au=Andersen,%20Odd%20Jan&rft.date=2006-04-01&rft.volume=19&rft.issue=2&rft.spage=173&rft.epage=192&rft.pages=173-192&rft.issn=0951-8339&rft.eissn=1873-4170&rft_id=info:doi/10.1016/j.marstruc.2006.07.003&rft_dat=%3Cproquest_cross%3E29938834%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c373t-4d5b82b8b4c7c123a28bd070f60973d5f35f7f82eae2f4cd661becfacd6b76723%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=29938834&rft_id=info:pmid/&rfr_iscdi=true |