Loading…

Large-scale circulation features in the tropical western Pacific and their representation in climate models

Within the Western Pacific Monsoon (WPM) region the zonal component of the low‐level winds tends to weaken and reverse from east to west during the peak monsoon season, which also marks a peak in rainfall. This study examines how well climate models can simulate these phenomena prior to evaluating t...

Full description

Saved in:
Bibliographic Details
Published in:Journal of Geophysical Research: Atmospheres 2012-02, Vol.117 (D4), p.n/a
Main Authors: Smith, Ian N., Moise, Aurel F., Colman, Robert A.
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-c3750-23a31174ac62afbb63023e0f42abd29ebd6c03952cc5380c06cd50e8f614a3b33
cites cdi_FETCH-LOGICAL-c3750-23a31174ac62afbb63023e0f42abd29ebd6c03952cc5380c06cd50e8f614a3b33
container_end_page n/a
container_issue D4
container_start_page
container_title Journal of Geophysical Research: Atmospheres
container_volume 117
creator Smith, Ian N.
Moise, Aurel F.
Colman, Robert A.
description Within the Western Pacific Monsoon (WPM) region the zonal component of the low‐level winds tends to weaken and reverse from east to west during the peak monsoon season, which also marks a peak in rainfall. This study examines how well climate models can simulate these phenomena prior to evaluating their projections for later this century. While a seasonal wind reversal or weakening appears to be reasonably well simulated by most models over much of the WPM, the relationships between large‐scale average winds and rainfall are not always well simulated. This allows us to discriminate among the models in order to see if this affects the projections. However, it so happens that this has relatively little effect, and the predominant signal is for an increase in rainfall with a weakening or negligible change to the low‐level monsoon winds. These results indicate that the WPM climate will respond more to global scale drivers such as an increase in atmospheric water vapor content and a weakening of the global circulation, rather than to more regional changes such as an increase in the land/ocean temperature contrast. Key Points The climate of the western Pacific is monsoon‐dominated Model projections favor increased rainfall, but little change to the winds Model performance at simulating the monsoon does not alter the projections
doi_str_mv 10.1029/2011JD016667
format article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_1020329780</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2686662131</sourcerecordid><originalsourceid>FETCH-LOGICAL-c3750-23a31174ac62afbb63023e0f42abd29ebd6c03952cc5380c06cd50e8f614a3b33</originalsourceid><addsrcrecordid>eNp9kE1v1DAQhi0EEqt2b_wAS4gboeNx7CRHaGHbEgFCfOzNcpwJeJsmi53Vsv8eL1lVnJjLXJ7nndHL2DMBrwRgdYEgxO0VCK118YgtUCidIQI-ZgsQeZkBYvGULWPcQJpc6RzEgt3VNvygLDrbE3c-uF1vJz8OvCM77QJF7gc-_SQ-hXHrE8X3FCcKA_9kne-843Zoj4APPNA2CTRMc0ISXe_v7UT8fmypj-fsSWf7SMvTPmNf3739cnmd1R9XN5ev68zJQkGG0kohitw6jbZrGi0BJUGXo21arKhptQNZKXROyRIcaNcqoLLTIreykfKMPZ9zt2H8tUvvms24C0M6aVJTILEqSkjUy5lyYYwxUGe2IX0bDgk6cpX5t9GEvziF2mNZXbCD8_HBQVWVmP-NlTO39z0d_ptpblefr0ShqqOVzZZP5f5-sGy4M-l2ocz3Dyvzbb1-U9er90bLP0k5k7I</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1020329780</pqid></control><display><type>article</type><title>Large-scale circulation features in the tropical western Pacific and their representation in climate models</title><source>Wiley-Blackwell Journals</source><source>Wiley-Blackwell AGU Digital Archive</source><creator>Smith, Ian N. ; Moise, Aurel F. ; Colman, Robert A.</creator><creatorcontrib>Smith, Ian N. ; Moise, Aurel F. ; Colman, Robert A.</creatorcontrib><description>Within the Western Pacific Monsoon (WPM) region the zonal component of the low‐level winds tends to weaken and reverse from east to west during the peak monsoon season, which also marks a peak in rainfall. This study examines how well climate models can simulate these phenomena prior to evaluating their projections for later this century. While a seasonal wind reversal or weakening appears to be reasonably well simulated by most models over much of the WPM, the relationships between large‐scale average winds and rainfall are not always well simulated. This allows us to discriminate among the models in order to see if this affects the projections. However, it so happens that this has relatively little effect, and the predominant signal is for an increase in rainfall with a weakening or negligible change to the low‐level monsoon winds. These results indicate that the WPM climate will respond more to global scale drivers such as an increase in atmospheric water vapor content and a weakening of the global circulation, rather than to more regional changes such as an increase in the land/ocean temperature contrast. Key Points The climate of the western Pacific is monsoon‐dominated Model projections favor increased rainfall, but little change to the winds Model performance at simulating the monsoon does not alter the projections</description><identifier>ISSN: 0148-0227</identifier><identifier>ISSN: 2169-897X</identifier><identifier>EISSN: 2156-2202</identifier><identifier>EISSN: 2169-8996</identifier><identifier>DOI: 10.1029/2011JD016667</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Atmospheric sciences ; Climate change ; Earth ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Geophysics ; Hydrology ; Meteorology ; monsoon ; Precipitation ; rainfall ; Regions ; western Pacific ; winds</subject><ispartof>Journal of Geophysical Research: Atmospheres, 2012-02, Vol.117 (D4), p.n/a</ispartof><rights>Published in 2012 by the American Geophysical Union</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3750-23a31174ac62afbb63023e0f42abd29ebd6c03952cc5380c06cd50e8f614a3b33</citedby><cites>FETCH-LOGICAL-c3750-23a31174ac62afbb63023e0f42abd29ebd6c03952cc5380c06cd50e8f614a3b33</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2011JD016667$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2011JD016667$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>315,786,790,11541,27957,27958,46503,46927,50923,51032</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=25982480$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Smith, Ian N.</creatorcontrib><creatorcontrib>Moise, Aurel F.</creatorcontrib><creatorcontrib>Colman, Robert A.</creatorcontrib><title>Large-scale circulation features in the tropical western Pacific and their representation in climate models</title><title>Journal of Geophysical Research: Atmospheres</title><addtitle>J. Geophys. Res</addtitle><description>Within the Western Pacific Monsoon (WPM) region the zonal component of the low‐level winds tends to weaken and reverse from east to west during the peak monsoon season, which also marks a peak in rainfall. This study examines how well climate models can simulate these phenomena prior to evaluating their projections for later this century. While a seasonal wind reversal or weakening appears to be reasonably well simulated by most models over much of the WPM, the relationships between large‐scale average winds and rainfall are not always well simulated. This allows us to discriminate among the models in order to see if this affects the projections. However, it so happens that this has relatively little effect, and the predominant signal is for an increase in rainfall with a weakening or negligible change to the low‐level monsoon winds. These results indicate that the WPM climate will respond more to global scale drivers such as an increase in atmospheric water vapor content and a weakening of the global circulation, rather than to more regional changes such as an increase in the land/ocean temperature contrast. Key Points The climate of the western Pacific is monsoon‐dominated Model projections favor increased rainfall, but little change to the winds Model performance at simulating the monsoon does not alter the projections</description><subject>Atmospheric sciences</subject><subject>Climate change</subject><subject>Earth</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Geophysics</subject><subject>Hydrology</subject><subject>Meteorology</subject><subject>monsoon</subject><subject>Precipitation</subject><subject>rainfall</subject><subject>Regions</subject><subject>western Pacific</subject><subject>winds</subject><issn>0148-0227</issn><issn>2169-897X</issn><issn>2156-2202</issn><issn>2169-8996</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><recordid>eNp9kE1v1DAQhi0EEqt2b_wAS4gboeNx7CRHaGHbEgFCfOzNcpwJeJsmi53Vsv8eL1lVnJjLXJ7nndHL2DMBrwRgdYEgxO0VCK118YgtUCidIQI-ZgsQeZkBYvGULWPcQJpc6RzEgt3VNvygLDrbE3c-uF1vJz8OvCM77QJF7gc-_SQ-hXHrE8X3FCcKA_9kne-843Zoj4APPNA2CTRMc0ISXe_v7UT8fmypj-fsSWf7SMvTPmNf3739cnmd1R9XN5ev68zJQkGG0kohitw6jbZrGi0BJUGXo21arKhptQNZKXROyRIcaNcqoLLTIreykfKMPZ9zt2H8tUvvms24C0M6aVJTILEqSkjUy5lyYYwxUGe2IX0bDgk6cpX5t9GEvziF2mNZXbCD8_HBQVWVmP-NlTO39z0d_ptpblefr0ShqqOVzZZP5f5-sGy4M-l2ocz3Dyvzbb1-U9er90bLP0k5k7I</recordid><startdate>20120227</startdate><enddate>20120227</enddate><creator>Smith, Ian N.</creator><creator>Moise, Aurel F.</creator><creator>Colman, Robert A.</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</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>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>L7M</scope><scope>M2O</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope></search><sort><creationdate>20120227</creationdate><title>Large-scale circulation features in the tropical western Pacific and their representation in climate models</title><author>Smith, Ian N. ; Moise, Aurel F. ; Colman, Robert A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3750-23a31174ac62afbb63023e0f42abd29ebd6c03952cc5380c06cd50e8f614a3b33</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Atmospheric sciences</topic><topic>Climate change</topic><topic>Earth</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Geophysics</topic><topic>Hydrology</topic><topic>Meteorology</topic><topic>monsoon</topic><topic>Precipitation</topic><topic>rainfall</topic><topic>Regions</topic><topic>western Pacific</topic><topic>winds</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Smith, Ian N.</creatorcontrib><creatorcontrib>Moise, Aurel F.</creatorcontrib><creatorcontrib>Colman, Robert A.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</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>Research Library (Alumni Edition)</collection><collection>Materials Science &amp; Engineering Collection</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest Central</collection><collection>Advanced Technologies &amp; Aerospace Database‎ (1962 - current)</collection><collection>ProQuest Agricultural &amp; Environmental Science</collection><collection>ProQuest Central Essentials</collection><collection>AUTh Library subscriptions: ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Earth, Atmospheric &amp; Aquatic Science</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>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aerospace Database</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>SciTech Premium Collection (Proquest) (PQ_SDU_P3)</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>ProQuest research library</collection><collection>ProQuest Engineering Database</collection><collection>Research Library (Corporate)</collection><collection>ProQuest Advanced Technologies &amp; Aerospace Database</collection><collection>ProQuest Advanced Technologies &amp; Aerospace Collection</collection><collection>Environmental Science Database</collection><collection>ProQuest Earth, Atmospheric &amp; 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>ProQuest Central China</collection><collection>Engineering Collection</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Journal of Geophysical Research: Atmospheres</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Smith, Ian N.</au><au>Moise, Aurel F.</au><au>Colman, Robert A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Large-scale circulation features in the tropical western Pacific and their representation in climate models</atitle><jtitle>Journal of Geophysical Research: Atmospheres</jtitle><addtitle>J. Geophys. Res</addtitle><date>2012-02-27</date><risdate>2012</risdate><volume>117</volume><issue>D4</issue><epage>n/a</epage><issn>0148-0227</issn><issn>2169-897X</issn><eissn>2156-2202</eissn><eissn>2169-8996</eissn><notes>ark:/67375/WNG-VXXBLLGK-6</notes><notes>ArticleID:2011JD016667</notes><notes>istex:CA1CCE7D7E78BEA7A57B37B5AF035CE83E094010</notes><notes>Tab-delimited Table 1.Tab-delimited Table 2.</notes><abstract>Within the Western Pacific Monsoon (WPM) region the zonal component of the low‐level winds tends to weaken and reverse from east to west during the peak monsoon season, which also marks a peak in rainfall. This study examines how well climate models can simulate these phenomena prior to evaluating their projections for later this century. While a seasonal wind reversal or weakening appears to be reasonably well simulated by most models over much of the WPM, the relationships between large‐scale average winds and rainfall are not always well simulated. This allows us to discriminate among the models in order to see if this affects the projections. However, it so happens that this has relatively little effect, and the predominant signal is for an increase in rainfall with a weakening or negligible change to the low‐level monsoon winds. These results indicate that the WPM climate will respond more to global scale drivers such as an increase in atmospheric water vapor content and a weakening of the global circulation, rather than to more regional changes such as an increase in the land/ocean temperature contrast. Key Points The climate of the western Pacific is monsoon‐dominated Model projections favor increased rainfall, but little change to the winds Model performance at simulating the monsoon does not alter the projections</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2011JD016667</doi><tpages>15</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0148-0227
ispartof Journal of Geophysical Research: Atmospheres, 2012-02, Vol.117 (D4), p.n/a
issn 0148-0227
2169-897X
2156-2202
2169-8996
language eng
recordid cdi_proquest_journals_1020329780
source Wiley-Blackwell Journals; Wiley-Blackwell AGU Digital Archive
subjects Atmospheric sciences
Climate change
Earth
Earth sciences
Earth, ocean, space
Exact sciences and technology
Geophysics
Hydrology
Meteorology
monsoon
Precipitation
rainfall
Regions
western Pacific
winds
title Large-scale circulation features in the tropical western Pacific and their representation in climate models
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-09-22T09%3A32%3A58IST&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=Large-scale%20circulation%20features%20in%20the%20tropical%20western%20Pacific%20and%20their%20representation%20in%20climate%20models&rft.jtitle=Journal%20of%20Geophysical%20Research:%20Atmospheres&rft.au=Smith,%20Ian%20N.&rft.date=2012-02-27&rft.volume=117&rft.issue=D4&rft.epage=n/a&rft.issn=0148-0227&rft.eissn=2156-2202&rft_id=info:doi/10.1029/2011JD016667&rft_dat=%3Cproquest_cross%3E2686662131%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c3750-23a31174ac62afbb63023e0f42abd29ebd6c03952cc5380c06cd50e8f614a3b33%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=1020329780&rft_id=info:pmid/&rfr_iscdi=true