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Energy partitioning between latent and sensible heat flux during the warm season at FLUXNET sites

Identifieur interne : 001694 ( Istex/Corpus ); précédent : 001693; suivant : 001695

Energy partitioning between latent and sensible heat flux during the warm season at FLUXNET sites

Auteurs : Kell B. Wilson ; Dennis D. Baldocchi ; Marc Aubinet ; Paul Berbigier ; Christian Bernhofer ; Han Dolman ; Eva Falge ; Chris Field ; Allen Goldstein ; Andre Granier ; Achim Grelle ; Thorgeirsson Halldor ; Dave Hollinger ; Gabriel Katul ; B. E. Law ; Anders Lindroth ; Tilden Meyers ; John Moncrieff ; Russ Monson ; Walter Oechel ; John Tenhunen ; Riccardo Valentini ; Shashi Verma ; Timo Vesala ; Steve Wofsy

Source :

RBID : ISTEX:A51733EC65325A9A5B2732F17D1FD9A9672AEDD0

Abstract

The warm season (mid‐June through late August) partitioning between sensible (H) and latent (LE) heat flux, or the Bowen ratio (β = H/LE), was investigated at 27 sites over 66 site years within the international network of eddy covariance sites (FLUXNET). Variability in β across ecosystems and climates was analyzed by quantifying general climatic and surface characteristics that control flux partitioning. The climatic control on β was quantified using the climatological resistance (Ri), which is proportional to the ratio of vapor pressure deficit (difference between saturation vapor pressure and atmospheric vapor pressure) to net radiation (large values of Ri decrease β). The control of flux partitioning by the vegetation and underlying surface was quantified by computing the surface resistance to water vapor transport (Rc, with large values tending to increase β). There was a considerable range in flux partitioning characteristics (Rc, Ri and β) among sites, but it was possible to define some general differences between vegetation types and climates. Deciduous forest sites and the agricultural site had the lowest values of Rc and β (0.25–0.50). Coniferous forests typically had a larger Rc and higher β (typically between 0.50 and 1.00 but also much larger). However, there was notable variability in Rc and Ri between coniferous site years, most notably differences between oceanic and continental climates and sites with a distinct dry summer season (Mediterranean climate). Sites with Mediterranean climates generally had the highest net radiation, Rc, Ri, and β. There was considerable variability in β between grassland site years, primarily the result of interannual differences in soil water content and Rc.

Url:
DOI: 10.1029/2001WR000989

Links to Exploration step

ISTEX:A51733EC65325A9A5B2732F17D1FD9A9672AEDD0

Le document en format XML

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<div type="abstract">The warm season (mid‐June through late August) partitioning between sensible (H) and latent (LE) heat flux, or the Bowen ratio (β = H/LE), was investigated at 27 sites over 66 site years within the international network of eddy covariance sites (FLUXNET). Variability in β across ecosystems and climates was analyzed by quantifying general climatic and surface characteristics that control flux partitioning. The climatic control on β was quantified using the climatological resistance (Ri), which is proportional to the ratio of vapor pressure deficit (difference between saturation vapor pressure and atmospheric vapor pressure) to net radiation (large values of Ri decrease β). The control of flux partitioning by the vegetation and underlying surface was quantified by computing the surface resistance to water vapor transport (Rc, with large values tending to increase β). There was a considerable range in flux partitioning characteristics (Rc, Ri and β) among sites, but it was possible to define some general differences between vegetation types and climates. Deciduous forest sites and the agricultural site had the lowest values of Rc and β (0.25–0.50). Coniferous forests typically had a larger Rc and higher β (typically between 0.50 and 1.00 but also much larger). However, there was notable variability in Rc and Ri between coniferous site years, most notably differences between oceanic and continental climates and sites with a distinct dry summer season (Mediterranean climate). Sites with Mediterranean climates generally had the highest net radiation, Rc, Ri, and β. There was considerable variability in β between grassland site years, primarily the result of interannual differences in soil water content and Rc.</div>
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</json:item>
<json:item>
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<subject>
<json:item>
<lang>
<json:string>eng</json:string>
</lang>
<value>eddy covariance</value>
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<json:item>
<lang>
<json:string>eng</json:string>
</lang>
<value>evaporation</value>
</json:item>
<json:item>
<lang>
<json:string>eng</json:string>
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<value>ecohydrology</value>
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<json:item>
<lang>
<json:string>eng</json:string>
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<value>hydrology</value>
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<articleId>
<json:string>2001WR000989</json:string>
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<language>
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<json:string>article</json:string>
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<abstract>The warm season (mid‐June through late August) partitioning between sensible (H) and latent (LE) heat flux, or the Bowen ratio (β = H/LE), was investigated at 27 sites over 66 site years within the international network of eddy covariance sites (FLUXNET). Variability in β across ecosystems and climates was analyzed by quantifying general climatic and surface characteristics that control flux partitioning. The climatic control on β was quantified using the climatological resistance (Ri), which is proportional to the ratio of vapor pressure deficit (difference between saturation vapor pressure and atmospheric vapor pressure) to net radiation (large values of Ri decrease β). The control of flux partitioning by the vegetation and underlying surface was quantified by computing the surface resistance to water vapor transport (Rc, with large values tending to increase β). There was a considerable range in flux partitioning characteristics (Rc, Ri and β) among sites, but it was possible to define some general differences between vegetation types and climates. Deciduous forest sites and the agricultural site had the lowest values of Rc and β (0.25–0.50). Coniferous forests typically had a larger Rc and higher β (typically between 0.50 and 1.00 but also much larger). However, there was notable variability in Rc and Ri between coniferous site years, most notably differences between oceanic and continental climates and sites with a distinct dry summer season (Mediterranean climate). Sites with Mediterranean climates generally had the highest net radiation, Rc, Ri, and β. There was considerable variability in β between grassland site years, primarily the result of interannual differences in soil water content and Rc.</abstract>
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<p xml:id="wrcr9248-para-0001" label="1">The warm season (mid‐June through late August) partitioning between sensible (
<i>H</i>
) and latent (
<i>LE</i>
) heat flux, or the Bowen ratio (β =
<i>H</i>
/
<i>LE</i>
), was investigated at 27 sites over 66 site years within the international network of eddy covariance sites (FLUXNET). Variability in β across ecosystems and climates was analyzed by quantifying general climatic and surface characteristics that control flux partitioning. The climatic control on β was quantified using the climatological resistance (
<i>R</i>
<sub>
<i>i</i>
</sub>
), which is proportional to the ratio of vapor pressure deficit (difference between saturation vapor pressure and atmospheric vapor pressure) to net radiation (large values of
<i>R</i>
<sub>
<i>i</i>
</sub>
decrease β). The control of flux partitioning by the vegetation and underlying surface was quantified by computing the surface resistance to water vapor transport (
<i>R</i>
<sub>
<i>c</i>
</sub>
, with large values tending to increase β). There was a considerable range in flux partitioning characteristics (
<i>R</i>
<sub>
<i>c</i>
</sub>
,
<i>R</i>
<sub>
<i>i</i>
</sub>
and β) among sites, but it was possible to define some general differences between vegetation types and climates. Deciduous forest sites and the agricultural site had the lowest values of
<i>R</i>
<sub>
<i>c</i>
</sub>
and β (0.25–0.50). Coniferous forests typically had a larger
<i>R</i>
<sub>
<i>c</i>
</sub>
and higher β (typically between 0.50 and 1.00 but also much larger). However, there was notable variability in
<i>R</i>
<sub>
<i>c</i>
</sub>
and
<i>R</i>
<sub>
<i>i</i>
</sub>
between coniferous site years, most notably differences between oceanic and continental climates and sites with a distinct dry summer season (Mediterranean climate). Sites with Mediterranean climates generally had the highest net radiation,
<i>R</i>
<sub>
<i>c</i>
</sub>
,
<i>R</i>
<sub>
<i>i</i>
</sub>
, and β. There was considerable variability in β between grassland site years, primarily the result of interannual differences in soil water content and
<i>R</i>
<sub>
<i>c</i>
</sub>
.</p>
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<title>Energy partitioning between latent and sensible heat flux during the warm season at FLUXNET sites</title>
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<titleInfo type="abbreviated" lang="en">
<title>ENERGY BALANCE PARTITIONING AT FLUXNET SITES</title>
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<titleInfo type="alternative" contentType="CDATA" lang="en">
<title>Energy partitioning between latent and sensible heat flux during the warm season at FLUXNET sites</title>
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<name type="personal">
<namePart type="given">Kell B.</namePart>
<namePart type="family">Wilson</namePart>
<affiliation>Atmospheric Turbulence and Diffusion Division, NOAA, Tennessee, Oak Ridge, USA</affiliation>
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<name type="personal">
<namePart type="given">Dennis D.</namePart>
<namePart type="family">Baldocchi</namePart>
<affiliation>Department of Environmental Science Policy and Management, University of California at Berkeley, California, Berkeley, USA</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Marc</namePart>
<namePart type="family">Aubinet</namePart>
<affiliation>Unité de Physique, Faculté des Sciences Agronomiques de Gembloux, Gembloux, Belgium</affiliation>
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<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Paul</namePart>
<namePart type="family">Berbigier</namePart>
<affiliation>Unité de Bioclimatologie, INRA Bourdeaux, Gazinet, France</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Christian</namePart>
<namePart type="family">Bernhofer</namePart>
<affiliation>Institute für Hydrologie und Meteorologie, Tharandt, Germany</affiliation>
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<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Han</namePart>
<namePart type="family">Dolman</namePart>
<affiliation>Alterra, Wageningen, Netherlands</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Eva</namePart>
<namePart type="family">Falge</namePart>
<affiliation>Pflanzenökologie, University Bayreuth, Bayreuth, Germany</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Chris</namePart>
<namePart type="family">Field</namePart>
<affiliation>Department of Plant Biology, Carnegie Institution of Washington, California, Stanford, USA</affiliation>
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<roleTerm type="text">author</roleTerm>
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</name>
<name type="personal">
<namePart type="given">Allen</namePart>
<namePart type="family">Goldstein</namePart>
<affiliation>Department of Environmental Science Policy and Management, University of California at Berkeley, California, Berkeley, USA</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Andre</namePart>
<namePart type="family">Granier</namePart>
<affiliation>Unite Ecophysiologie Forestieres, Institut Nationale de la Recherche Agronomique, Champenoux, France</affiliation>
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<roleTerm type="text">author</roleTerm>
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</name>
<name type="personal">
<namePart type="given">Achim</namePart>
<namePart type="family">Grelle</namePart>
<affiliation>Department of Ecology and Environmental Research, Swedish University of Agricultural Sciences, Uppsala, Sweden</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
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</name>
<name type="personal">
<namePart type="given">Thorgeirsson</namePart>
<namePart type="family">Halldor</namePart>
<affiliation>Department of Environmental Research, Agricultural Research Institute, Reykjavik, Iceland</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
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</name>
<name type="personal">
<namePart type="given">Dave</namePart>
<namePart type="family">Hollinger</namePart>
<affiliation>USDA Forest Service, Northeastern Forest Experiment Station, New Hampshire, Durham, USA</affiliation>
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<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Gabriel</namePart>
<namePart type="family">Katul</namePart>
<affiliation>School of the Environment, Duke University, North Carolina, Durham, USA</affiliation>
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<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">B. E.</namePart>
<namePart type="family">Law</namePart>
<affiliation>College of Forestry, Oregon State University, Oregon, Corvallis, USA</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Anders</namePart>
<namePart type="family">Lindroth</namePart>
<affiliation>Department of Ecology and Environmental Research, Swedish University of Agricultural Sciences, Uppsala, Sweden</affiliation>
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<roleTerm type="text">author</roleTerm>
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</name>
<name type="personal">
<namePart type="given">Tilden</namePart>
<namePart type="family">Meyers</namePart>
<affiliation>Atmospheric Turbulence and Diffusion Division, NOAA, Tennessee, Oak Ridge, USA</affiliation>
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<roleTerm type="text">author</roleTerm>
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</name>
<name type="personal">
<namePart type="given">John</namePart>
<namePart type="family">Moncrieff</namePart>
<affiliation>Department of Ecology and Environmental Research, University of Edinburgh, Edinburgh, UK</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Russ</namePart>
<namePart type="family">Monson</namePart>
<affiliation>Department of Environmental, Population, and Organismic Biology, University of Colorado, Colorado, Boulder, USA</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Walter</namePart>
<namePart type="family">Oechel</namePart>
<affiliation>Global Change Research Group, San Diego State University, California, San Diego, USA</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">John</namePart>
<namePart type="family">Tenhunen</namePart>
<affiliation>Pflanzenökologie, University Bayreuth, Bayreuth, Germany</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Riccardo</namePart>
<namePart type="family">Valentini</namePart>
<affiliation>Department of Forest Science and Resources, University of Tuscia, Viterbo, Italy</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Shashi</namePart>
<namePart type="family">Verma</namePart>
<affiliation>School of Natural Resource Sciences, University of Nebraska, Lincoln, Nebraska, Lincoln, USA</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Timo</namePart>
<namePart type="family">Vesala</namePart>
<affiliation>Department of Physical Sciences, University of Helsinki, Helsinki, Finland</affiliation>
<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Steve</namePart>
<namePart type="family">Wofsy</namePart>
<affiliation>Department of Earth and Planetary Sciences, Harvard University, Massachusetts, Cambridge, USA</affiliation>
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<publisher>Blackwell Publishing Ltd</publisher>
<dateIssued encoding="w3cdtf">2002-12</dateIssued>
<dateCaptured encoding="w3cdtf">2001-10-03</dateCaptured>
<dateValid encoding="w3cdtf">2002-01-03</dateValid>
<edition>Wilson, K. B., et al., Energy partitioning between latent and sensible heat flux during the warm season at FLUXNET sites, Water Resour. Res., 38(12), 1294, doi:10.1029/2001WR000989, 2002.</edition>
<copyrightDate encoding="w3cdtf">2002</copyrightDate>
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<abstract>The warm season (mid‐June through late August) partitioning between sensible (H) and latent (LE) heat flux, or the Bowen ratio (β = H/LE), was investigated at 27 sites over 66 site years within the international network of eddy covariance sites (FLUXNET). Variability in β across ecosystems and climates was analyzed by quantifying general climatic and surface characteristics that control flux partitioning. The climatic control on β was quantified using the climatological resistance (Ri), which is proportional to the ratio of vapor pressure deficit (difference between saturation vapor pressure and atmospheric vapor pressure) to net radiation (large values of Ri decrease β). The control of flux partitioning by the vegetation and underlying surface was quantified by computing the surface resistance to water vapor transport (Rc, with large values tending to increase β). There was a considerable range in flux partitioning characteristics (Rc, Ri and β) among sites, but it was possible to define some general differences between vegetation types and climates. Deciduous forest sites and the agricultural site had the lowest values of Rc and β (0.25–0.50). Coniferous forests typically had a larger Rc and higher β (typically between 0.50 and 1.00 but also much larger). However, there was notable variability in Rc and Ri between coniferous site years, most notably differences between oceanic and continental climates and sites with a distinct dry summer season (Mediterranean climate). Sites with Mediterranean climates generally had the highest net radiation, Rc, Ri, and β. There was considerable variability in β between grassland site years, primarily the result of interannual differences in soil water content and Rc.</abstract>
<subject>
<genre>keywords</genre>
<topic>eddy covariance</topic>
<topic>evaporation</topic>
<topic>ecohydrology</topic>
<topic>hydrology</topic>
</subject>
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<title>Water Resources Research</title>
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<titleInfo type="abbreviated">
<title>Water Resour. Res.</title>
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<topic authorityURI="http://psi.agu.org/taxonomy5/0300">Atmospheric Composition and Structure</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0315">Atmospheric Composition and Structure: Biosphere/atmosphere interactions</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/1800">Hydrology</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/1818">Hydrology: Evapotranspiration</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/1851">Hydrology: Plant ecology</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/3300">Atmospheric Processes</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/3322">Meteorology and Atmospheric Dynamics: Land/atmosphere interactions</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/3307">Meteorology and Atmospheric Dynamics: Boundary layer processes</topic>
</subject>
<identifier type="ISSN">0043-1397</identifier>
<identifier type="eISSN">1944-7973</identifier>
<identifier type="DOI">10.1002/(ISSN)1944-7973</identifier>
<identifier type="CODEN">WRERAQ</identifier>
<identifier type="PublisherID">WRCR</identifier>
<part>
<date>2002</date>
<detail type="volume">
<caption>vol.</caption>
<number>38</number>
</detail>
<detail type="issue">
<caption>no.</caption>
<number>12</number>
</detail>
<extent unit="pages">
<start>30-1</start>
<end>30-11</end>
<total>11</total>
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<identifier type="DOI">10.1029/2001WR000989</identifier>
<identifier type="ArticleID">2001WR000989</identifier>
<accessCondition type="use and reproduction" contentType="copyright">Copyright 2002 by the American Geophysical Union.</accessCondition>
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