Five-year measurements of ozone fluxes to a Danish Norway spruce canopy

Teis Nørgaard Mikkelsen, H. Ro-Poulsen, M.F. Hovmand, N.O. Jensen, K. Pilegaard, A.H. Egeløv

    Research output: Contribution to journalJournal articleResearchpeer-review

    Abstract

    Ozone concentrations and fluxes have been measured continuously during 5 years (1996-2000) by the gradient method in a Norway spruce dominated forest stand in West Jutland, Denmark, planted in 1965. The method has been validated against other methodologies and a relatively good relationship was found. The data are analysed to quantify diurnal, seasonal and yearly fluxes, and non-stomatal and stomatal removal are estimated. Monthly means of climatic data are shown, and day and night values of the aerodynamic resistance, r(a), viscous sub-layer resistance, r(b), and the surface or canopy resistance, r(c), are presented. The yearly ozone deposition is approximately 126 kg ha(-1). The canopy ozone uptake is highest during the day and during the summer. This is interpreted as increased stomatal uptake and physical and chemical reactions. The daily means of ozone concentration and fluxes averaged over 5 years correlate, but the correlation is primarily based on two different uncoupled processes outside and inside the stomates: (1) The ozone destruction in the canopy occurring outside the stomates is much influenced by temperature, light and humidity, e.g. surface reactions, NO- and VOC-emissions. (2) The same factors have a strong influence on the stomatal opening, e.g. midday and night closure. Thus, looking at diurnal variations, the diurnal ozone concentration and ozone flux do not correlate at all during the growing season. The maximum diurnal difference for the ozone concentration is a factor 1.3 and the maximum diurnal difference for the ozone flux is a factor 3. From dawn to ca. 8:00 the ozone deposition increases and the ozone concentration decreases.

    The yearly stomatal uptake of ozone is estimated to minimum 21% of the total deposition, being highest in May-August (30-33%) and lowest in November-February (4-9%). The physiological ozone uptake per leaf area is estimated to 0.33 g ozone m(-2) Y(-1). (C) 2004 Elsevier Ltd. All rights reserved.
    Original languageEnglish
    JournalAtmospheric Environment
    Volume38
    Issue number15
    Pages (from-to)2361-2371
    ISSN1352-2310
    DOIs
    Publication statusPublished - 2004

    Cite this

    Mikkelsen, Teis Nørgaard ; Ro-Poulsen, H. ; Hovmand, M.F. ; Jensen, N.O. ; Pilegaard, K. ; Egeløv, A.H. / Five-year measurements of ozone fluxes to a Danish Norway spruce canopy. In: Atmospheric Environment. 2004 ; Vol. 38, No. 15. pp. 2361-2371.
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    abstract = "Ozone concentrations and fluxes have been measured continuously during 5 years (1996-2000) by the gradient method in a Norway spruce dominated forest stand in West Jutland, Denmark, planted in 1965. The method has been validated against other methodologies and a relatively good relationship was found. The data are analysed to quantify diurnal, seasonal and yearly fluxes, and non-stomatal and stomatal removal are estimated. Monthly means of climatic data are shown, and day and night values of the aerodynamic resistance, r(a), viscous sub-layer resistance, r(b), and the surface or canopy resistance, r(c), are presented. The yearly ozone deposition is approximately 126 kg ha(-1). The canopy ozone uptake is highest during the day and during the summer. This is interpreted as increased stomatal uptake and physical and chemical reactions. The daily means of ozone concentration and fluxes averaged over 5 years correlate, but the correlation is primarily based on two different uncoupled processes outside and inside the stomates: (1) The ozone destruction in the canopy occurring outside the stomates is much influenced by temperature, light and humidity, e.g. surface reactions, NO- and VOC-emissions. (2) The same factors have a strong influence on the stomatal opening, e.g. midday and night closure. Thus, looking at diurnal variations, the diurnal ozone concentration and ozone flux do not correlate at all during the growing season. The maximum diurnal difference for the ozone concentration is a factor 1.3 and the maximum diurnal difference for the ozone flux is a factor 3. From dawn to ca. 8:00 the ozone deposition increases and the ozone concentration decreases.The yearly stomatal uptake of ozone is estimated to minimum 21{\%} of the total deposition, being highest in May-August (30-33{\%}) and lowest in November-February (4-9{\%}). The physiological ozone uptake per leaf area is estimated to 0.33 g ozone m(-2) Y(-1). (C) 2004 Elsevier Ltd. All rights reserved.",
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    author = "Mikkelsen, {Teis N{\o}rgaard} and H. Ro-Poulsen and M.F. Hovmand and N.O. Jensen and K. Pilegaard and A.H. Egel{\o}v",
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    Five-year measurements of ozone fluxes to a Danish Norway spruce canopy. / Mikkelsen, Teis Nørgaard; Ro-Poulsen, H.; Hovmand, M.F.; Jensen, N.O.; Pilegaard, K.; Egeløv, A.H.

    In: Atmospheric Environment, Vol. 38, No. 15, 2004, p. 2361-2371.

    Research output: Contribution to journalJournal articleResearchpeer-review

    TY - JOUR

    T1 - Five-year measurements of ozone fluxes to a Danish Norway spruce canopy

    AU - Mikkelsen, Teis Nørgaard

    AU - Ro-Poulsen, H.

    AU - Hovmand, M.F.

    AU - Jensen, N.O.

    AU - Pilegaard, K.

    AU - Egeløv, A.H.

    PY - 2004

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    N2 - Ozone concentrations and fluxes have been measured continuously during 5 years (1996-2000) by the gradient method in a Norway spruce dominated forest stand in West Jutland, Denmark, planted in 1965. The method has been validated against other methodologies and a relatively good relationship was found. The data are analysed to quantify diurnal, seasonal and yearly fluxes, and non-stomatal and stomatal removal are estimated. Monthly means of climatic data are shown, and day and night values of the aerodynamic resistance, r(a), viscous sub-layer resistance, r(b), and the surface or canopy resistance, r(c), are presented. The yearly ozone deposition is approximately 126 kg ha(-1). The canopy ozone uptake is highest during the day and during the summer. This is interpreted as increased stomatal uptake and physical and chemical reactions. The daily means of ozone concentration and fluxes averaged over 5 years correlate, but the correlation is primarily based on two different uncoupled processes outside and inside the stomates: (1) The ozone destruction in the canopy occurring outside the stomates is much influenced by temperature, light and humidity, e.g. surface reactions, NO- and VOC-emissions. (2) The same factors have a strong influence on the stomatal opening, e.g. midday and night closure. Thus, looking at diurnal variations, the diurnal ozone concentration and ozone flux do not correlate at all during the growing season. The maximum diurnal difference for the ozone concentration is a factor 1.3 and the maximum diurnal difference for the ozone flux is a factor 3. From dawn to ca. 8:00 the ozone deposition increases and the ozone concentration decreases.The yearly stomatal uptake of ozone is estimated to minimum 21% of the total deposition, being highest in May-August (30-33%) and lowest in November-February (4-9%). The physiological ozone uptake per leaf area is estimated to 0.33 g ozone m(-2) Y(-1). (C) 2004 Elsevier Ltd. All rights reserved.

    AB - Ozone concentrations and fluxes have been measured continuously during 5 years (1996-2000) by the gradient method in a Norway spruce dominated forest stand in West Jutland, Denmark, planted in 1965. The method has been validated against other methodologies and a relatively good relationship was found. The data are analysed to quantify diurnal, seasonal and yearly fluxes, and non-stomatal and stomatal removal are estimated. Monthly means of climatic data are shown, and day and night values of the aerodynamic resistance, r(a), viscous sub-layer resistance, r(b), and the surface or canopy resistance, r(c), are presented. The yearly ozone deposition is approximately 126 kg ha(-1). The canopy ozone uptake is highest during the day and during the summer. This is interpreted as increased stomatal uptake and physical and chemical reactions. The daily means of ozone concentration and fluxes averaged over 5 years correlate, but the correlation is primarily based on two different uncoupled processes outside and inside the stomates: (1) The ozone destruction in the canopy occurring outside the stomates is much influenced by temperature, light and humidity, e.g. surface reactions, NO- and VOC-emissions. (2) The same factors have a strong influence on the stomatal opening, e.g. midday and night closure. Thus, looking at diurnal variations, the diurnal ozone concentration and ozone flux do not correlate at all during the growing season. The maximum diurnal difference for the ozone concentration is a factor 1.3 and the maximum diurnal difference for the ozone flux is a factor 3. From dawn to ca. 8:00 the ozone deposition increases and the ozone concentration decreases.The yearly stomatal uptake of ozone is estimated to minimum 21% of the total deposition, being highest in May-August (30-33%) and lowest in November-February (4-9%). The physiological ozone uptake per leaf area is estimated to 0.33 g ozone m(-2) Y(-1). (C) 2004 Elsevier Ltd. All rights reserved.

    KW - 9-B risiko

    U2 - 10.1016/j.atmosenv.2003.12.036

    DO - 10.1016/j.atmosenv.2003.12.036

    M3 - Journal article

    VL - 38

    SP - 2361

    EP - 2371

    JO - Atmospheric Environment

    JF - Atmospheric Environment

    SN - 1352-2310

    IS - 15

    ER -