Models of CO2 and water vapour fluxes from a sparse millet crop in the Sahel

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Standard

Models of CO2 and water vapour fluxes from a sparse millet crop in the Sahel. / Boegh, E.; Soegaard, H.; Friborg, T.; Levy, P. E.

I: Agricultural and Forest Meteorology, Bind 93, Nr. 1, 1999, s. 7-26.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Boegh, E, Soegaard, H, Friborg, T & Levy, PE 1999, 'Models of CO2 and water vapour fluxes from a sparse millet crop in the Sahel', Agricultural and Forest Meteorology, bind 93, nr. 1, s. 7-26. https://doi.org/10.1016/S0168-1923(99)00108-2

APA

Boegh, E., Soegaard, H., Friborg, T., & Levy, P. E. (1999). Models of CO2 and water vapour fluxes from a sparse millet crop in the Sahel. Agricultural and Forest Meteorology, 93(1), 7-26. https://doi.org/10.1016/S0168-1923(99)00108-2

Vancouver

Boegh E, Soegaard H, Friborg T, Levy PE. Models of CO2 and water vapour fluxes from a sparse millet crop in the Sahel. Agricultural and Forest Meteorology. 1999;93(1):7-26. https://doi.org/10.1016/S0168-1923(99)00108-2

Author

Boegh, E. ; Soegaard, H. ; Friborg, T. ; Levy, P. E. / Models of CO2 and water vapour fluxes from a sparse millet crop in the Sahel. I: Agricultural and Forest Meteorology. 1999 ; Bind 93, Nr. 1. s. 7-26.

Bibtex

@article{5f7741974752491781f126d87e3f8e6d,
title = "Models of CO2 and water vapour fluxes from a sparse millet crop in the Sahel",
abstract = "Canopy fluxes of water vapour and CO2 from a sparse millet crop are simulated on the basis of a leaf scale model designed to predict stomatal conductance, leaf temperature, transpiration rate and photosynthetic rate for millet on a diurnal basis. The modelled leaf fluxes are extrapolated using two different big-leaf approaches. In the traditional big-leaf approach, all leaves are exposed to the same microenvironment which is different from the environmental conditions above the canopy, whereas in the modified big-leaf approach the canopy is regarded as a partly shaded big-leaf. In the sun/shade big-leaf model, soil reflection, diffuse radiation and separate evaluations of the radiation load on sunlit and shaded leaf surfaces are taken into account. Due to the low fraction of shaded leaves in the sparse canopy, the two types of big-leaf models predict both canopy fluxes equally well. The sensitivity of the modelled fluxes to the various input parameters was ranked for the identification of the most important parameters controlling photosynthesis and transpiration. This information is used for identification of more simple scaling models aimed at predicting daily canopy fluxes. The influx of sensible heat to the leaf was found to be an important energy source for transpiration. It was confirmed that daily transpiration can be parameterized by the air humidity gradient using only the leaf area index (LAI) for the evaluation of seasonal changes in bulk stomatal conductance. The photosynthetic rate was found to be most sensitive to radiation and leaf temperature. It is shown that the daily canopy photosynthesis can he estimated on the basis of LAI and midday values (1200 h) of incoming radiation density and leaf temperature.",
keywords = "Carbon dioxide assimilation, Leaf temperature, Local advection, Millet, Permisetum glaucum, Sapflow",
author = "E. Boegh and H. Soegaard and T. Friborg and Levy, {P. E.}",
year = "1999",
doi = "10.1016/S0168-1923(99)00108-2",
language = "English",
volume = "93",
pages = "7--26",
journal = "Agricultural and Forest Meteorology",
issn = "0168-1923",
publisher = "Elsevier",
number = "1",

}

RIS

TY - JOUR

T1 - Models of CO2 and water vapour fluxes from a sparse millet crop in the Sahel

AU - Boegh, E.

AU - Soegaard, H.

AU - Friborg, T.

AU - Levy, P. E.

PY - 1999

Y1 - 1999

N2 - Canopy fluxes of water vapour and CO2 from a sparse millet crop are simulated on the basis of a leaf scale model designed to predict stomatal conductance, leaf temperature, transpiration rate and photosynthetic rate for millet on a diurnal basis. The modelled leaf fluxes are extrapolated using two different big-leaf approaches. In the traditional big-leaf approach, all leaves are exposed to the same microenvironment which is different from the environmental conditions above the canopy, whereas in the modified big-leaf approach the canopy is regarded as a partly shaded big-leaf. In the sun/shade big-leaf model, soil reflection, diffuse radiation and separate evaluations of the radiation load on sunlit and shaded leaf surfaces are taken into account. Due to the low fraction of shaded leaves in the sparse canopy, the two types of big-leaf models predict both canopy fluxes equally well. The sensitivity of the modelled fluxes to the various input parameters was ranked for the identification of the most important parameters controlling photosynthesis and transpiration. This information is used for identification of more simple scaling models aimed at predicting daily canopy fluxes. The influx of sensible heat to the leaf was found to be an important energy source for transpiration. It was confirmed that daily transpiration can be parameterized by the air humidity gradient using only the leaf area index (LAI) for the evaluation of seasonal changes in bulk stomatal conductance. The photosynthetic rate was found to be most sensitive to radiation and leaf temperature. It is shown that the daily canopy photosynthesis can he estimated on the basis of LAI and midday values (1200 h) of incoming radiation density and leaf temperature.

AB - Canopy fluxes of water vapour and CO2 from a sparse millet crop are simulated on the basis of a leaf scale model designed to predict stomatal conductance, leaf temperature, transpiration rate and photosynthetic rate for millet on a diurnal basis. The modelled leaf fluxes are extrapolated using two different big-leaf approaches. In the traditional big-leaf approach, all leaves are exposed to the same microenvironment which is different from the environmental conditions above the canopy, whereas in the modified big-leaf approach the canopy is regarded as a partly shaded big-leaf. In the sun/shade big-leaf model, soil reflection, diffuse radiation and separate evaluations of the radiation load on sunlit and shaded leaf surfaces are taken into account. Due to the low fraction of shaded leaves in the sparse canopy, the two types of big-leaf models predict both canopy fluxes equally well. The sensitivity of the modelled fluxes to the various input parameters was ranked for the identification of the most important parameters controlling photosynthesis and transpiration. This information is used for identification of more simple scaling models aimed at predicting daily canopy fluxes. The influx of sensible heat to the leaf was found to be an important energy source for transpiration. It was confirmed that daily transpiration can be parameterized by the air humidity gradient using only the leaf area index (LAI) for the evaluation of seasonal changes in bulk stomatal conductance. The photosynthetic rate was found to be most sensitive to radiation and leaf temperature. It is shown that the daily canopy photosynthesis can he estimated on the basis of LAI and midday values (1200 h) of incoming radiation density and leaf temperature.

KW - Carbon dioxide assimilation

KW - Leaf temperature

KW - Local advection

KW - Millet

KW - Permisetum glaucum

KW - Sapflow

U2 - 10.1016/S0168-1923(99)00108-2

DO - 10.1016/S0168-1923(99)00108-2

M3 - Journal article

AN - SCOPUS:0033601864

VL - 93

SP - 7

EP - 26

JO - Agricultural and Forest Meteorology

JF - Agricultural and Forest Meteorology

SN - 0168-1923

IS - 1

ER -

ID: 260406146