Nonlinear balanced models for stratified fluids conserving Ertel–Rossby PV

Nonlinear balanced models for stratified fluids conserving Ertel–Rossby PV

A derivation of consistent balanced models for stratified fluids conserving the Ertel–Rossby potential vorticity (PV) is presented. It is used to develop a set of balanced models incorporating new omega equations valid for flow regimes from synoptic scale to mesoscale. The models are developed for q...

Full description

Saved in:
Bibliographic Details
Published in:Quarterly journal of the Royal Meteorological Society 2003-01, Vol.129 (587), p.139-156
Main Authors: Ziemia'Nski, Micha Z., Thorpe, Alan J.
Format: Article
Language:eng
Subjects:
Convection, turbulence, diffusion. Boundary layer structure and dynamics
Earth, ocean, space
Exact sciences and technology
External geophysics
Meteorology
Omega equation
Potential vorticity
Vertical velocity
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
recordid cdi_crossref_primary_10_1256_qj_02_58
title Nonlinear balanced models for stratified fluids conserving Ertel–Rossby PV
format Article
creator Ziemia'Nski, Micha Z.
Thorpe, Alan J.
subjects Convection, turbulence, diffusion. Boundary layer structure and dynamics
Earth, ocean, space
Exact sciences and technology
External geophysics
Meteorology
Omega equation
Potential vorticity
Vertical velocity
ispartof Quarterly journal of the Royal Meteorological Society, 2003-01, Vol.129 (587), p.139-156
description A derivation of consistent balanced models for stratified fluids conserving the Ertel–Rossby potential vorticity (PV) is presented. It is used to develop a set of balanced models incorporating new omega equations valid for flow regimes from synoptic scale to mesoscale. The models are developed for quasi‐Boussinesq and real atmospheres, and for adiabatic and frictionless as well as non‐conservative processes. The new omega equations allow the identification of additional forcing of the vertical velocity due to the ageostrophic and stability effects, and the modification of atmospheric response due to the non‐Boussinesq effects. It is shown that the new omega equation, valid beyond the limit of small Rossby number, allows for a subjective analysis of the vertical‐velocity forcing based on an approach involving the isentropic upgliding, Ertel–Rossby PV advection and boundary temperature advection. Copyright © 2003 Royal Meteorological Society
language eng
source EZB Electronic Journals Library
identifier ISSN: 0035-9009
fulltext fulltext
issn 0035-9009
1477-870X
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-05-28T15%3A38%3A06IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-wiley_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Nonlinear%20balanced%20models%20for%20stratified%20fluids%20conserving%20Ertel%E2%80%93Rossby%20PV&rft.jtitle=Quarterly%20journal%20of%20the%20Royal%20Meteorological%20Society&rft.au=Ziemia'Nski,%20Micha%20Z.&rft.date=2003-01&rft.volume=129&rft.issue=587&rft.spage=139&rft.epage=156&rft.pages=139-156&rft.issn=0035-9009&rft.eissn=1477-870X&rft.coden=QJRMAM&rft_id=info:doi/10.1256/qj.02.58&rft_dat=%3Cwiley_cross%3EQJ200312958708%3C/wiley_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c3008-537e702a711ede2650e152c8df18f1a18f0824f1f6512801848898a82080bd2a3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_id=info:pmid/
container_title Quarterly journal of the Royal Meteorological Society
container_volume 129
container_issue 587
container_start_page 139
container_end_page 156
fullrecord <record><control><sourceid>wiley_cross</sourceid><recordid>TN_cdi_crossref_primary_10_1256_qj_02_58</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>QJ200312958708</sourcerecordid><originalsourceid>FETCH-LOGICAL-c3008-537e702a711ede2650e152c8df18f1a18f0824f1f6512801848898a82080bd2a3</originalsourceid><addsrcrecordid>eNp1kE1LAzEQhoMoWKvgT8hF8LJ1MrtpZo9S6hfFL1S8LeluIinpbptUpTf_g__QX2Kkgicv88Lw8A7zMHYoYCBQDk-WswHgQNIW64lCqYwUPG-zHkAusxKg3GV7Mc4AQCpUPTa57lrvWqMDn2qv29o0fN41xkduu8DjKuiVsy5trX91TeR110YT3lz7wsdhZfzXx-d9F-N0zW-f9tmO1T6ag9_ss8ez8cPoIpvcnF-OTidZnQNQJnNlFKBWQpjG4FCCERJraqwgK3QaQFhYYYdSIIGggqgkTQgE0wZ13mfHm946pNPB2GoR3FyHdSWg-rFQLWcVYCUpoUcbdKFjrb0N6UUX__hC5oAoEldsuHfnzfrfvuruCpNKgaVMYin_BgHebFY</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><isCDI>true</isCDI><recordtype>article</recordtype></control><display><type>article</type><title>Nonlinear balanced models for stratified fluids conserving Ertel–Rossby PV</title><source>EZB Electronic Journals Library</source><creator>Ziemia'Nski, Micha Z. ; Thorpe, Alan J.</creator><creatorcontrib>Ziemia'Nski, Micha Z. ; Thorpe, Alan J.</creatorcontrib><description>A derivation of consistent balanced models for stratified fluids conserving the Ertel–Rossby potential vorticity (PV) is presented. It is used to develop a set of balanced models incorporating new omega equations valid for flow regimes from synoptic scale to mesoscale. The models are developed for quasi‐Boussinesq and real atmospheres, and for adiabatic and frictionless as well as non‐conservative processes. The new omega equations allow the identification of additional forcing of the vertical velocity due to the ageostrophic and stability effects, and the modification of atmospheric response due to the non‐Boussinesq effects. It is shown that the new omega equation, valid beyond the limit of small Rossby number, allows for a subjective analysis of the vertical‐velocity forcing based on an approach involving the isentropic upgliding, Ertel–Rossby PV advection and boundary temperature advection. Copyright © 2003 Royal Meteorological Society</description><identifier>ISSN: 0035-9009</identifier><identifier>EISSN: 1477-870X</identifier><identifier>DOI: 10.1256/qj.02.58</identifier><identifier>CODEN: QJRMAM</identifier><language>eng</language><publisher>Chichester, UK: John Wiley &amp; Sons, Ltd</publisher><subject>Convection, turbulence, diffusion. Boundary layer structure and dynamics ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Meteorology ; Omega equation ; Potential vorticity ; Vertical velocity</subject><ispartof>Quarterly journal of the Royal Meteorological Society, 2003-01, Vol.129 (587), p.139-156</ispartof><rights>Copyright © 2003 Royal Meteorological Society</rights><rights>2003 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3008-537e702a711ede2650e152c8df18f1a18f0824f1f6512801848898a82080bd2a3</citedby><cites>FETCH-LOGICAL-c3008-537e702a711ede2650e152c8df18f1a18f0824f1f6512801848898a82080bd2a3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>315,787,791,4046,27984,27985,27986</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=14530221$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Ziemia'Nski, Micha Z.</creatorcontrib><creatorcontrib>Thorpe, Alan J.</creatorcontrib><title>Nonlinear balanced models for stratified fluids conserving Ertel–Rossby PV</title><title>Quarterly journal of the Royal Meteorological Society</title><description>A derivation of consistent balanced models for stratified fluids conserving the Ertel–Rossby potential vorticity (PV) is presented. It is used to develop a set of balanced models incorporating new omega equations valid for flow regimes from synoptic scale to mesoscale. The models are developed for quasi‐Boussinesq and real atmospheres, and for adiabatic and frictionless as well as non‐conservative processes. The new omega equations allow the identification of additional forcing of the vertical velocity due to the ageostrophic and stability effects, and the modification of atmospheric response due to the non‐Boussinesq effects. It is shown that the new omega equation, valid beyond the limit of small Rossby number, allows for a subjective analysis of the vertical‐velocity forcing based on an approach involving the isentropic upgliding, Ertel–Rossby PV advection and boundary temperature advection. Copyright © 2003 Royal Meteorological Society</description><subject>Convection, turbulence, diffusion. Boundary layer structure and dynamics</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Meteorology</subject><subject>Omega equation</subject><subject>Potential vorticity</subject><subject>Vertical velocity</subject><issn>0035-9009</issn><issn>1477-870X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><recordid>eNp1kE1LAzEQhoMoWKvgT8hF8LJ1MrtpZo9S6hfFL1S8LeluIinpbptUpTf_g__QX2Kkgicv88Lw8A7zMHYoYCBQDk-WswHgQNIW64lCqYwUPG-zHkAusxKg3GV7Mc4AQCpUPTa57lrvWqMDn2qv29o0fN41xkduu8DjKuiVsy5trX91TeR110YT3lz7wsdhZfzXx-d9F-N0zW-f9tmO1T6ag9_ss8ez8cPoIpvcnF-OTidZnQNQJnNlFKBWQpjG4FCCERJraqwgK3QaQFhYYYdSIIGggqgkTQgE0wZ13mfHm946pNPB2GoR3FyHdSWg-rFQLWcVYCUpoUcbdKFjrb0N6UUX__hC5oAoEldsuHfnzfrfvuruCpNKgaVMYin_BgHebFY</recordid><startdate>200301</startdate><enddate>200301</enddate><creator>Ziemia'Nski, Micha Z.</creator><creator>Thorpe, Alan J.</creator><general>John Wiley &amp; Sons, Ltd</general><general>Wiley</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>200301</creationdate><title>Nonlinear balanced models for stratified fluids conserving Ertel–Rossby PV</title><author>Ziemia'Nski, Micha Z. ; Thorpe, Alan J.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3008-537e702a711ede2650e152c8df18f1a18f0824f1f6512801848898a82080bd2a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2003</creationdate><topic>Convection, turbulence, diffusion. Boundary layer structure and dynamics</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Meteorology</topic><topic>Omega equation</topic><topic>Potential vorticity</topic><topic>Vertical velocity</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ziemia'Nski, Micha Z.</creatorcontrib><creatorcontrib>Thorpe, Alan J.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><jtitle>Quarterly journal of the Royal Meteorological Society</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ziemia'Nski, Micha Z.</au><au>Thorpe, Alan J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Nonlinear balanced models for stratified fluids conserving Ertel–Rossby PV</atitle><jtitle>Quarterly journal of the Royal Meteorological Society</jtitle><date>2003-01</date><risdate>2003</risdate><volume>129</volume><issue>587</issue><spage>139</spage><epage>156</epage><pages>139-156</pages><issn>0035-9009</issn><eissn>1477-870X</eissn><coden>QJRMAM</coden><abstract>A derivation of consistent balanced models for stratified fluids conserving the Ertel–Rossby potential vorticity (PV) is presented. It is used to develop a set of balanced models incorporating new omega equations valid for flow regimes from synoptic scale to mesoscale. The models are developed for quasi‐Boussinesq and real atmospheres, and for adiabatic and frictionless as well as non‐conservative processes. The new omega equations allow the identification of additional forcing of the vertical velocity due to the ageostrophic and stability effects, and the modification of atmospheric response due to the non‐Boussinesq effects. It is shown that the new omega equation, valid beyond the limit of small Rossby number, allows for a subjective analysis of the vertical‐velocity forcing based on an approach involving the isentropic upgliding, Ertel–Rossby PV advection and boundary temperature advection. Copyright © 2003 Royal Meteorological Society</abstract><cop>Chichester, UK</cop><pub>John Wiley &amp; Sons, Ltd</pub><doi>10.1256/qj.02.58</doi><tpages>18</tpages></addata></record>