Near-Surface Stress Profile and Conditional Averaging of Turbulence
Using the conditional average formulation, we suggest a new explanation for why the stress in the atmospheric surface layer is often observed to vary with height. In essence, because turbulence series are always correlated for small lags, the steady-state equations of motion with negligible viscous...
Gespeichert in:
| Veröffentlicht in: | Boundary-layer meteorology 2009-09, Vol.132 (3), p.475-481 |
|---|---|
| Hauptverfasser: | , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 481 |
|---|---|
| container_issue | 3 |
| container_start_page | 475 |
| container_title | Boundary-layer meteorology |
| container_volume | 132 |
| creator | Treviño, George Andreas, Edgar L |
| description | Using the conditional average formulation, we suggest a new explanation for why the stress in the atmospheric surface layer is often observed to vary with height. In essence, because turbulence series are always correlated for small lags, the steady-state equations of motion with negligible viscous terms that traditionally require vertical fluxes to be constant with height accordingly now require the vertical fluxes to vary with height. This result has implications for interpreting and validating Monin-Obukhov similarity theory. |
| doi_str_mv | 10.1007/s10546-009-9411-5 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_36365475</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>21284633</sourcerecordid><originalsourceid>FETCH-LOGICAL-c464t-6882cb91a8cf760231845c6ab980ce48f090c0f19e786ef7ff664147d7a36fb93</originalsourceid><addsrcrecordid>eNqFkV1rFDEUhoNYcG39AV45CIo3qeckmZPksix-QbHCttchm02WKdNJTXYE_71Zpyh4Ua9CyHOevJyXsZcI5wig31eEXhEHsNwqRN4_YSvsteSotHjKVgBA3EhUz9jzWm_bVWMPK7b-Gn3hm7kkH2K3OZRYa_et5DSMsfPTrlvnaTcchjz5sbv4EYvfD9O-y6m7nst2HuMU4hk7SX6s8cXDecpuPn64Xn_ml1efvqwvLnlQpA6cjBFha9GbkDSBkGhUH8hvrYEQlUlgIUBCG7WhmHRKRKrF32kvKW2tPGVvF-99yd_nWA_ubqghjqOfYp6rkySpV7r_LyhQGEVSNvDdoyBqDVJaZURDX_-D3ua5tK0c_yXZfFY3CBcolFxricndl-HOl58OwR17cktPrvXkjj25Y9g3D2Jfgx9T8VMY6p9BgRaV_O0WC1fb07SP5W-Ax-SvlqHks_P70sQ3GwEoAYnIgJa_APZ_qOE</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>366384697</pqid></control><display><type>article</type><title>Near-Surface Stress Profile and Conditional Averaging of Turbulence</title><source>SpringerLink Journals - AutoHoldings</source><creator>Treviño, George ; Andreas, Edgar L</creator><creatorcontrib>Treviño, George ; Andreas, Edgar L</creatorcontrib><description>Using the conditional average formulation, we suggest a new explanation for why the stress in the atmospheric surface layer is often observed to vary with height. In essence, because turbulence series are always correlated for small lags, the steady-state equations of motion with negligible viscous terms that traditionally require vertical fluxes to be constant with height accordingly now require the vertical fluxes to vary with height. This result has implications for interpreting and validating Monin-Obukhov similarity theory.</description><identifier>ISSN: 0006-8314</identifier><identifier>EISSN: 1573-1472</identifier><identifier>DOI: 10.1007/s10546-009-9411-5</identifier><identifier>CODEN: BLMEBR</identifier><language>eng</language><publisher>Dordrecht: Dordrecht : Springer Netherlands</publisher><subject>Atmospheric boundary layer ; Atmospheric Protection/Air Quality Control/Air Pollution ; Atmospheric Sciences ; Atmospheric surface layer ; Boundaries ; Brief Communication ; Computational fluid dynamics ; Conditional averaging ; Correlated turbulence ; Earth and Environmental Science ; Earth Sciences ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Fluid flow ; Fluxes ; Meteorology ; Monin-Obukhov similarity theory ; Similarity theory ; Stresses ; Turbulence ; Turbulent flow ; Turbulent stress</subject><ispartof>Boundary-layer meteorology, 2009-09, Vol.132 (3), p.475-481</ispartof><rights>Springer Science+Business Media B.V. 2009</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c464t-6882cb91a8cf760231845c6ab980ce48f090c0f19e786ef7ff664147d7a36fb93</citedby><cites>FETCH-LOGICAL-c464t-6882cb91a8cf760231845c6ab980ce48f090c0f19e786ef7ff664147d7a36fb93</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10546-009-9411-5$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10546-009-9411-5$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,777,781,27905,27906,41469,42538,51300</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=21914397$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Treviño, George</creatorcontrib><creatorcontrib>Andreas, Edgar L</creatorcontrib><title>Near-Surface Stress Profile and Conditional Averaging of Turbulence</title><title>Boundary-layer meteorology</title><addtitle>Boundary-Layer Meteorol</addtitle><description>Using the conditional average formulation, we suggest a new explanation for why the stress in the atmospheric surface layer is often observed to vary with height. In essence, because turbulence series are always correlated for small lags, the steady-state equations of motion with negligible viscous terms that traditionally require vertical fluxes to be constant with height accordingly now require the vertical fluxes to vary with height. This result has implications for interpreting and validating Monin-Obukhov similarity theory.</description><subject>Atmospheric boundary layer</subject><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>Atmospheric Sciences</subject><subject>Atmospheric surface layer</subject><subject>Boundaries</subject><subject>Brief Communication</subject><subject>Computational fluid dynamics</subject><subject>Conditional averaging</subject><subject>Correlated turbulence</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Fluid flow</subject><subject>Fluxes</subject><subject>Meteorology</subject><subject>Monin-Obukhov similarity theory</subject><subject>Similarity theory</subject><subject>Stresses</subject><subject>Turbulence</subject><subject>Turbulent flow</subject><subject>Turbulent stress</subject><issn>0006-8314</issn><issn>1573-1472</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNqFkV1rFDEUhoNYcG39AV45CIo3qeckmZPksix-QbHCttchm02WKdNJTXYE_71Zpyh4Ua9CyHOevJyXsZcI5wig31eEXhEHsNwqRN4_YSvsteSotHjKVgBA3EhUz9jzWm_bVWMPK7b-Gn3hm7kkH2K3OZRYa_et5DSMsfPTrlvnaTcchjz5sbv4EYvfD9O-y6m7nst2HuMU4hk7SX6s8cXDecpuPn64Xn_ml1efvqwvLnlQpA6cjBFha9GbkDSBkGhUH8hvrYEQlUlgIUBCG7WhmHRKRKrF32kvKW2tPGVvF-99yd_nWA_ubqghjqOfYp6rkySpV7r_LyhQGEVSNvDdoyBqDVJaZURDX_-D3ua5tK0c_yXZfFY3CBcolFxricndl-HOl58OwR17cktPrvXkjj25Y9g3D2Jfgx9T8VMY6p9BgRaV_O0WC1fb07SP5W-Ax-SvlqHks_P70sQ3GwEoAYnIgJa_APZ_qOE</recordid><startdate>20090901</startdate><enddate>20090901</enddate><creator>Treviño, George</creator><creator>Andreas, Edgar L</creator><general>Dordrecht : Springer Netherlands</general><general>Springer Netherlands</general><general>Springer</general><general>Springer Nature B.V</general><scope>FBQ</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>7XB</scope><scope>88F</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>L7M</scope><scope>M1Q</scope><scope>M2P</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope></search><sort><creationdate>20090901</creationdate><title>Near-Surface Stress Profile and Conditional Averaging of Turbulence</title><author>Treviño, George ; Andreas, Edgar L</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c464t-6882cb91a8cf760231845c6ab980ce48f090c0f19e786ef7ff664147d7a36fb93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>Atmospheric boundary layer</topic><topic>Atmospheric Protection/Air Quality Control/Air Pollution</topic><topic>Atmospheric Sciences</topic><topic>Atmospheric surface layer</topic><topic>Boundaries</topic><topic>Brief Communication</topic><topic>Computational fluid dynamics</topic><topic>Conditional averaging</topic><topic>Correlated turbulence</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Fluid flow</topic><topic>Fluxes</topic><topic>Meteorology</topic><topic>Monin-Obukhov similarity theory</topic><topic>Similarity theory</topic><topic>Stresses</topic><topic>Turbulence</topic><topic>Turbulent flow</topic><topic>Turbulent stress</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Treviño, George</creatorcontrib><creatorcontrib>Andreas, Edgar L</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Military Database (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Military Database</collection><collection>Science Database</collection><collection>Advanced Technologies & Aerospace Database</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Boundary-layer meteorology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Treviño, George</au><au>Andreas, Edgar L</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Near-Surface Stress Profile and Conditional Averaging of Turbulence</atitle><jtitle>Boundary-layer meteorology</jtitle><stitle>Boundary-Layer Meteorol</stitle><date>2009-09-01</date><risdate>2009</risdate><volume>132</volume><issue>3</issue><spage>475</spage><epage>481</epage><pages>475-481</pages><issn>0006-8314</issn><eissn>1573-1472</eissn><coden>BLMEBR</coden><abstract>Using the conditional average formulation, we suggest a new explanation for why the stress in the atmospheric surface layer is often observed to vary with height. In essence, because turbulence series are always correlated for small lags, the steady-state equations of motion with negligible viscous terms that traditionally require vertical fluxes to be constant with height accordingly now require the vertical fluxes to vary with height. This result has implications for interpreting and validating Monin-Obukhov similarity theory.</abstract><cop>Dordrecht</cop><pub>Dordrecht : Springer Netherlands</pub><doi>10.1007/s10546-009-9411-5</doi><tpages>7</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0006-8314 |
| ispartof | Boundary-layer meteorology, 2009-09, Vol.132 (3), p.475-481 |
| issn | 0006-8314 1573-1472 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_36365475 |
| source | SpringerLink Journals - AutoHoldings |
| subjects | Atmospheric boundary layer Atmospheric Protection/Air Quality Control/Air Pollution Atmospheric Sciences Atmospheric surface layer Boundaries Brief Communication Computational fluid dynamics Conditional averaging Correlated turbulence Earth and Environmental Science Earth Sciences Earth, ocean, space Exact sciences and technology External geophysics Fluid flow Fluxes Meteorology Monin-Obukhov similarity theory Similarity theory Stresses Turbulence Turbulent flow Turbulent stress |
| title | Near-Surface Stress Profile and Conditional Averaging of Turbulence |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-18T01%3A03%3A33IST&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=Near-Surface%20Stress%20Profile%20and%20Conditional%20Averaging%20of%20Turbulence&rft.jtitle=Boundary-layer%20meteorology&rft.au=Trevi%C3%B1o,%20George&rft.date=2009-09-01&rft.volume=132&rft.issue=3&rft.spage=475&rft.epage=481&rft.pages=475-481&rft.issn=0006-8314&rft.eissn=1573-1472&rft.coden=BLMEBR&rft_id=info:doi/10.1007/s10546-009-9411-5&rft_dat=%3Cproquest_cross%3E21284633%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=366384697&rft_id=info:pmid/&rfr_iscdi=true |