A mechanism for the influence of vegetation on the response of the diurnal temperature range to changing climate

We propose a new mechanism that could contribute to the observed decrease in the diurnal temperature range (DTR) over the last century: the physiological behavior of vegetation in response to climate. Using a physiologically based land surface model, we analyze the influence of vegetation on the res...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Geophysical research letters 2000-10, Vol.27 (20), p.3381-3384
Hauptverfasser: Collatz, G. James, Bounoua, L., Los, S. O., Randall, D. A., Fung, I. Y., Sellers, P. J.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 3384
container_issue 20
container_start_page 3381
container_title Geophysical research letters
container_volume 27
creator Collatz, G. James
Bounoua, L.
Los, S. O.
Randall, D. A.
Fung, I. Y.
Sellers, P. J.
description We propose a new mechanism that could contribute to the observed decrease in the diurnal temperature range (DTR) over the last century: the physiological behavior of vegetation in response to climate. Using a physiologically based land surface model, we analyze the influence of vegetation on the response of the DTR to perturbations in the state of the climate and vegetation. Increasing down‐welling long wave radiation and surface air temperature together, conditions that could occur as a result of doubling of atmospheric CO2, produced little change in the DTR. Changes in the state of the vegetation (i.e. amount, physiological capacity, stress) produce changes in the DTR of the order or larger than observed. Results emphasize that DTR modeling studies need to consider vegetation responses and suggest that recently reported increases in vegetation over the last decade could contribute to the observed decreases in the DTR.
doi_str_mv 10.1029/1999GL010947
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_18509209</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>18509209</sourcerecordid><originalsourceid>FETCH-LOGICAL-c4774-24c9ba4a4ceaa5cd66f4e1c410efa9fc65dc840bec90b004d6876e2b97c7936e3</originalsourceid><addsrcrecordid>eNp9kFFrFDEQx4NY8Gx98wMEBJ_cOtnNJpvHUuwpLLUeFR9DLje5Rneza5LV9tub80rxSRgYZub3_zMzhLxmcM6gVu-ZUmrdAwPF5TOyYorzqgOQz8kKSq_qailekJcpfQeABhq2IvMFHdHemeDTSN0Uab5D6oMbFgwW6eToL9xjNtlPgZY4jCOmeQrp7_RQ7_wSgxloxnHGaPISC2PCHmme6MF778Oe2sGPJuMZOXFmSPjqMZ-Sr1cfbi8_Vv3n9afLi76yXEpe1dyqreGGWzSmtTshHEdmOQN0Rjkr2p3tOGzRKtgC8J3opMB6q6SVqhHYnJK3R985Tj8XTFmPPlkcBhNwWpJmXQuqBlXAd0fQximliE7PsWwaHzQDfXir_vetBX_z6GuSNYMrh1qfnjSy64TsClUfqd9-wIf_Our1pmd1y3kRVUeRTxnvn0Qm_tBCNrLV367X-rbuhfxys9Gb5g_QMpab</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>18509209</pqid></control><display><type>article</type><title>A mechanism for the influence of vegetation on the response of the diurnal temperature range to changing climate</title><source>Wiley Online Library Free Content</source><source>Access via Wiley Online Library</source><source>Wiley-Blackwell AGU Digital Library</source><source>EZB-FREE-00999 freely available EZB journals</source><creator>Collatz, G. James ; Bounoua, L. ; Los, S. O. ; Randall, D. A. ; Fung, I. Y. ; Sellers, P. J.</creator><creatorcontrib>Collatz, G. James ; Bounoua, L. ; Los, S. O. ; Randall, D. A. ; Fung, I. Y. ; Sellers, P. J.</creatorcontrib><description>We propose a new mechanism that could contribute to the observed decrease in the diurnal temperature range (DTR) over the last century: the physiological behavior of vegetation in response to climate. Using a physiologically based land surface model, we analyze the influence of vegetation on the response of the DTR to perturbations in the state of the climate and vegetation. Increasing down‐welling long wave radiation and surface air temperature together, conditions that could occur as a result of doubling of atmospheric CO2, produced little change in the DTR. Changes in the state of the vegetation (i.e. amount, physiological capacity, stress) produce changes in the DTR of the order or larger than observed. Results emphasize that DTR modeling studies need to consider vegetation responses and suggest that recently reported increases in vegetation over the last decade could contribute to the observed decreases in the DTR.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/1999GL010947</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Climatology. Bioclimatology. Climate change ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Meteorology</subject><ispartof>Geophysical research letters, 2000-10, Vol.27 (20), p.3381-3384</ispartof><rights>Copyright 2000 by the American Geophysical Union.</rights><rights>2001 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4774-24c9ba4a4ceaa5cd66f4e1c410efa9fc65dc840bec90b004d6876e2b97c7936e3</citedby><cites>FETCH-LOGICAL-c4774-24c9ba4a4ceaa5cd66f4e1c410efa9fc65dc840bec90b004d6876e2b97c7936e3</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%2F1999GL010947$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F1999GL010947$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,1433,11514,27924,27925,45574,45575,46409,46468,46833,46892</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=788678$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Collatz, G. James</creatorcontrib><creatorcontrib>Bounoua, L.</creatorcontrib><creatorcontrib>Los, S. O.</creatorcontrib><creatorcontrib>Randall, D. A.</creatorcontrib><creatorcontrib>Fung, I. Y.</creatorcontrib><creatorcontrib>Sellers, P. J.</creatorcontrib><title>A mechanism for the influence of vegetation on the response of the diurnal temperature range to changing climate</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>We propose a new mechanism that could contribute to the observed decrease in the diurnal temperature range (DTR) over the last century: the physiological behavior of vegetation in response to climate. Using a physiologically based land surface model, we analyze the influence of vegetation on the response of the DTR to perturbations in the state of the climate and vegetation. Increasing down‐welling long wave radiation and surface air temperature together, conditions that could occur as a result of doubling of atmospheric CO2, produced little change in the DTR. Changes in the state of the vegetation (i.e. amount, physiological capacity, stress) produce changes in the DTR of the order or larger than observed. Results emphasize that DTR modeling studies need to consider vegetation responses and suggest that recently reported increases in vegetation over the last decade could contribute to the observed decreases in the DTR.</description><subject>Climatology. Bioclimatology. Climate change</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Meteorology</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2000</creationdate><recordtype>article</recordtype><recordid>eNp9kFFrFDEQx4NY8Gx98wMEBJ_cOtnNJpvHUuwpLLUeFR9DLje5Rneza5LV9tub80rxSRgYZub3_zMzhLxmcM6gVu-ZUmrdAwPF5TOyYorzqgOQz8kKSq_qailekJcpfQeABhq2IvMFHdHemeDTSN0Uab5D6oMbFgwW6eToL9xjNtlPgZY4jCOmeQrp7_RQ7_wSgxloxnHGaPISC2PCHmme6MF778Oe2sGPJuMZOXFmSPjqMZ-Sr1cfbi8_Vv3n9afLi76yXEpe1dyqreGGWzSmtTshHEdmOQN0Rjkr2p3tOGzRKtgC8J3opMB6q6SVqhHYnJK3R985Tj8XTFmPPlkcBhNwWpJmXQuqBlXAd0fQximliE7PsWwaHzQDfXir_vetBX_z6GuSNYMrh1qfnjSy64TsClUfqd9-wIf_Our1pmd1y3kRVUeRTxnvn0Qm_tBCNrLV367X-rbuhfxys9Gb5g_QMpab</recordid><startdate>20001015</startdate><enddate>20001015</enddate><creator>Collatz, G. James</creator><creator>Bounoua, L.</creator><creator>Los, S. O.</creator><creator>Randall, D. A.</creator><creator>Fung, I. Y.</creator><creator>Sellers, P. J.</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>KL.</scope></search><sort><creationdate>20001015</creationdate><title>A mechanism for the influence of vegetation on the response of the diurnal temperature range to changing climate</title><author>Collatz, G. James ; Bounoua, L. ; Los, S. O. ; Randall, D. A. ; Fung, I. Y. ; Sellers, P. J.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4774-24c9ba4a4ceaa5cd66f4e1c410efa9fc65dc840bec90b004d6876e2b97c7936e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2000</creationdate><topic>Climatology. Bioclimatology. Climate change</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Meteorology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Collatz, G. James</creatorcontrib><creatorcontrib>Bounoua, L.</creatorcontrib><creatorcontrib>Los, S. O.</creatorcontrib><creatorcontrib>Randall, D. A.</creatorcontrib><creatorcontrib>Fung, I. Y.</creatorcontrib><creatorcontrib>Sellers, P. J.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Collatz, G. James</au><au>Bounoua, L.</au><au>Los, S. O.</au><au>Randall, D. A.</au><au>Fung, I. Y.</au><au>Sellers, P. J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A mechanism for the influence of vegetation on the response of the diurnal temperature range to changing climate</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>2000-10-15</date><risdate>2000</risdate><volume>27</volume><issue>20</issue><spage>3381</spage><epage>3384</epage><pages>3381-3384</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>We propose a new mechanism that could contribute to the observed decrease in the diurnal temperature range (DTR) over the last century: the physiological behavior of vegetation in response to climate. Using a physiologically based land surface model, we analyze the influence of vegetation on the response of the DTR to perturbations in the state of the climate and vegetation. Increasing down‐welling long wave radiation and surface air temperature together, conditions that could occur as a result of doubling of atmospheric CO2, produced little change in the DTR. Changes in the state of the vegetation (i.e. amount, physiological capacity, stress) produce changes in the DTR of the order or larger than observed. Results emphasize that DTR modeling studies need to consider vegetation responses and suggest that recently reported increases in vegetation over the last decade could contribute to the observed decreases in the DTR.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/1999GL010947</doi><tpages>4</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0094-8276
ispartof Geophysical research letters, 2000-10, Vol.27 (20), p.3381-3384
issn 0094-8276
1944-8007
language eng
recordid cdi_proquest_miscellaneous_18509209
source Wiley Online Library Free Content; Access via Wiley Online Library; Wiley-Blackwell AGU Digital Library; EZB-FREE-00999 freely available EZB journals
subjects Climatology. Bioclimatology. Climate change
Earth, ocean, space
Exact sciences and technology
External geophysics
Meteorology
title A mechanism for the influence of vegetation on the response of the diurnal temperature range to changing climate
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-27T03%3A34%3A30IST&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=A%20mechanism%20for%20the%20influence%20of%20vegetation%20on%20the%20response%20of%20the%20diurnal%20temperature%20range%20to%20changing%20climate&rft.jtitle=Geophysical%20research%20letters&rft.au=Collatz,%20G.%20James&rft.date=2000-10-15&rft.volume=27&rft.issue=20&rft.spage=3381&rft.epage=3384&rft.pages=3381-3384&rft.issn=0094-8276&rft.eissn=1944-8007&rft.coden=GPRLAJ&rft_id=info:doi/10.1029/1999GL010947&rft_dat=%3Cproquest_cross%3E18509209%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=18509209&rft_id=info:pmid/&rfr_iscdi=true