Variability of annual CO sub(2) exchange from Dutch grasslands

An intercomparison is made of the Net Ecosystem Exchange of CO sub(2), NEE, for eight Dutch grassland sites: four natural grasslands, two production grasslands and two meteorological stations within a rotational grassland region. At all sites the NEE was determined during at least 10 months per site...

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Veröffentlicht in:Biogeosciences 2007-10, Vol.4 (5), p.803-816
Hauptverfasser: J Jacobs, CM, G Jacobs, AF, Bosveld, F C, Hendriks, D, Hensen, A, Kroon, P S, Moors, E J, Nol, L, Schrier-Uijl, A, Veenendaal, E M
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Sprache:eng
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Zusammenfassung:An intercomparison is made of the Net Ecosystem Exchange of CO sub(2), NEE, for eight Dutch grassland sites: four natural grasslands, two production grasslands and two meteorological stations within a rotational grassland region. At all sites the NEE was determined during at least 10 months per site, using the eddy-covariance (EC) technique, but in different years. The NEE does not include any import or export other than CO sub(2). The photosynthesis-light response analysis technique is used along with the respiration-temperature response technique to partition NEE into Gross Primary Production (GPP) and Ecosystem Respiration (R sub(e)) and to obtain the eco-physiological characteristics of the sites at the field scale. Annual sums of NEE, GPP and R sub(e) are then estimated using the fitted response curves with observed radiation and air temperature from a meteorological site in the centre of The Netherlands as drivers. These calculations are carried out for four years (2002-2005). Land use and management histories are not considered. The estimated annual R sub(e) for all individual sites is more or less constant per site and the average for all sites amounts to 1390 plus or minus 30 gC m super(− 2) a super(− 1). The narrow uncertainty band ( plus or minus 2%) reflects the small differences in the mean annual air temperature. The mean annual GPP was estimated to be 1325 g C m super(− 2) a super(− 1), and displays a much higher standard deviation, of plus or minus 110 gC m super(− 2) a super(− 1) (8%), which reflects the relatively large variation in annual solar radiation. The mean annual NEE amounts to -65 plus or minus 85 gC m super(− 2) a super(− 1). From two sites, four-year records of CO sub(2) flux were available and analyzed (2002-2005). Using the weather record of 2005 with optimizations from the other years, the standard deviation of annual GPP was estimated to be 171-206 gC m super(− 2) a super(− 1) (8-14%), of annual R sub(e) 227-247 gC m super(− 2) a super(− 1) (14-16%) and of annual NEE 176-276 gC m super(− 2) a super(− 1). The inter-site standard deviation was higher for GPP and R sub(e), 534 gC m super(− 2) a super(− 1) (37.3%) and 486 gC m super(− 2) a super(− 1) (34.8%), respectively. However, the inter-site standard deviation of NEE was similar to the interannual one, amounting to 207 gC m super(− 2) a super(− 1). Large differences occur due to soil type. The grasslands on organic (peat) soils show a mean net release of CO sub(2) of 220
ISSN:1726-4170
1726-4189