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Measurements of turbulent transfer in the near‐surface layer over a rice paddy in China

Identifieur interne : 000D56 ( Istex/Corpus ); précédent : 000D55; suivant : 000D57

Measurements of turbulent transfer in the near‐surface layer over a rice paddy in China

Auteurs : Zhiqiu Gao ; Lingen Bian ; Xiuji Zhou

Source :

RBID : ISTEX:0DC2604FD3614503E42B92B17879729AC9E1BA6C

Abstract

Eddy covariance measurements were conducted on fluxes of moisture, heat, and CO2 in a near‐surface layer over a rice paddy in the central plain of China from 10 June to 20 July 2001. During this period, the canopy height increased from 0.16 to 0.65 m. The study site, typical of the agricultural region in China, was ∼600 m × 600 m, was surrounded by similar rice paddies and was flooded throughout the entire experiment. We estimated the zero plane displacement and the roughness length at the end of the experiment to be 0.43 m and 0.027 m, respectively. Aerodynamic roughness length increased with increasing wind speed when the rice height was >0.5 m. On the basis of footprint analysis, we expected >90% of the measured flux (at a height of 3 m above water) to occur within the nearest 600 m of upwind area. We examined daily and seasonal variations in the components of the surface energy balance and in CO2 flux. Results show that the pattern of energy partition had no obvious variation during the season. Daytime absorption and nighttime release of CO2 flux by the rice paddy gradually increased as the rice grew. We examined the energy budget closure and found it to be around 0.91. We tested the extended Louis scheme using eddy covariance techniques. It estimated surface stress in good agreement with direct measurements. However, on average, this scheme underestimated sensible heat flux by 10% and latent heat flux by 11%.

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DOI: 10.1029/2002JD002779

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<p xml:id="jgrd10109-para-0001" label="1">Eddy covariance measurements were conducted on fluxes of moisture, heat, and CO
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in a near‐surface layer over a rice paddy in the central plain of China from 10 June to 20 July 2001. During this period, the canopy height increased from 0.16 to 0.65 m. The study site, typical of the agricultural region in China, was ∼600 m × 600 m, was surrounded by similar rice paddies and was flooded throughout the entire experiment. We estimated the zero plane displacement and the roughness length at the end of the experiment to be 0.43 m and 0.027 m, respectively. Aerodynamic roughness length increased with increasing wind speed when the rice height was >0.5 m. On the basis of footprint analysis, we expected >90% of the measured flux (at a height of 3 m above water) to occur within the nearest 600 m of upwind area. We examined daily and seasonal variations in the components of the surface energy balance and in CO
<sub>2</sub>
flux. Results show that the pattern of energy partition had no obvious variation during the season. Daytime absorption and nighttime release of CO
<sub>2</sub>
flux by the rice paddy gradually increased as the rice grew. We examined the energy budget closure and found it to be around 0.91. We tested the extended Louis scheme using eddy covariance techniques. It estimated surface stress in good agreement with direct measurements. However, on average, this scheme underestimated sensible heat flux by 10% and latent heat flux by 11%.</p>
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<title>Measurements of turbulent transfer in the near‐surface layer over a rice paddy in China</title>
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<namePart type="given">Zhiqiu</namePart>
<namePart type="family">Gao</namePart>
<affiliation>Chinese Academy of Meteorological Science, Beijing, China</affiliation>
<affiliation>Now at Department of Meteorology, Naval Postgraduate School, Monterey, California, USA.</affiliation>
<affiliation>E-mail: zgao@nps.navy.mil</affiliation>
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<edition>Gao, Zhiqiu, Lingen Bian, and Xiuji Zhou (2003), Measurements of turbulent transfer in the near‐surface layer over a rice paddy in China, J. Geophys. Res., 108, 4387, doi:10.1029/2002JD002779, D13.</edition>
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<abstract>Eddy covariance measurements were conducted on fluxes of moisture, heat, and CO2 in a near‐surface layer over a rice paddy in the central plain of China from 10 June to 20 July 2001. During this period, the canopy height increased from 0.16 to 0.65 m. The study site, typical of the agricultural region in China, was ∼600 m × 600 m, was surrounded by similar rice paddies and was flooded throughout the entire experiment. We estimated the zero plane displacement and the roughness length at the end of the experiment to be 0.43 m and 0.027 m, respectively. Aerodynamic roughness length increased with increasing wind speed when the rice height was >0.5 m. On the basis of footprint analysis, we expected >90% of the measured flux (at a height of 3 m above water) to occur within the nearest 600 m of upwind area. We examined daily and seasonal variations in the components of the surface energy balance and in CO2 flux. Results show that the pattern of energy partition had no obvious variation during the season. Daytime absorption and nighttime release of CO2 flux by the rice paddy gradually increased as the rice grew. We examined the energy budget closure and found it to be around 0.91. We tested the extended Louis scheme using eddy covariance techniques. It estimated surface stress in good agreement with direct measurements. However, on average, this scheme underestimated sensible heat flux by 10% and latent heat flux by 11%.</abstract>
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<genre>keywords</genre>
<topic>measurements</topic>
<topic>turbulent transfer</topic>
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<title>J. Geophys. Res.</title>
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<topic authorityURI="http://psi.agu.org/subset/ACL">Climate and Dynamics</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0300">ATMOSPHERIC COMPOSITION AND STRUCTURE</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0315">Biosphere/atmosphere interactions</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/3300">ATMOSPHERIC PROCESSES</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/3307">Meteorology and Atmospheric Dynamics: Boundary layer processes</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/3322">Meteorology and Atmospheric Dynamics: Land/atmosphere interactions</topic>
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<topic>Climate and Dynamics</topic>
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<identifier type="ISSN">0148-0227</identifier>
<identifier type="eISSN">2156-2202</identifier>
<identifier type="DOI">10.1002/(ISSN)2156-2202d</identifier>
<identifier type="CODEN">JGREA2</identifier>
<identifier type="PublisherID">JGRD</identifier>
<part>
<date>2003</date>
<detail type="volume">
<caption>vol.</caption>
<number>108</number>
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<detail type="issue">
<caption>no.</caption>
<number>D13</number>
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<identifier type="DOI">10.1029/2002JD002779</identifier>
<identifier type="ArticleID">2002JD002779</identifier>
<accessCondition type="use and reproduction" contentType="copyright">Copyright 2003 by the American Geophysical Union.</accessCondition>
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