1Atmospheric Sciences, Centre for Ecology and Hydrology (CEH) Edinburgh, Bush Estate, Penicuik, Midlothian, EH26 0QB, UK
2Swiss Federal Research Station for Agroecology and Agriculture (FAL-CH), Zürich-Reckenholz and Liebefeld-Bern, 3003 Bern, Switzerland
3Institut National de la Recherche Agronomique (INRA), UMR Environnement et Grandes Cultures, Thiverval-Grignon, 78850, France
4School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Simon Building, Oxford Road, Manchester, M13 9PL, UK (formerly known as: University of Manchester Institute of Science and Technology, UMIST).
5Energy research Centre of the Netherlands (ECN), Postbus 1, 1755 ZG Petten, The Netherlands
6Eötvös Loránd University, Department of Meteorology, 1117 Budapest, Hungary
7Hungarian Meteorological Service, 1675 Budapest, Hungary
8Institute for Agroecology, German Agricultural Research Institute, Braunschweig-Völkerode, Germany
9Agrometeorological Research Station of Deutscher Wetterdienst, Bundesallee 50, 38116 Braunschweig, Germany
Received: 22 Sep 2008 – Published in Biogeosciences Discuss.: 08 Jan 2009 – Published: 07 Aug 2009
Abstract. Commonly, the micrometeorological parameters that underline the calculations of surface atmosphere exchange fluxes (e.g. friction velocity and sensible heat flux) and parameters used to model exchange fluxes with SVAT-type parameterisations (e.g. latent heat flux and canopy temperature) are measured with a single set of instrumentation and are analysed with a single methodology. This paper evaluates uncertainties in these measurements with a single instrument, by comparing the independent results from nine different institutes during the international GRAMINAE integrated field experiment over agricultural grassland near Braunschweig, Lower Saxony, Germany. The paper discusses uncertainties in measuring friction velocity, sensible and latent heat fluxes, canopy temperature and investigates the energy balance closure at this site. Although individual 15-min flux calculations show a large variability between the instruments, when averaged over the campaign, fluxes agree within 2% for momentum and 11% for sensible heat. However, the spread in estimates of latent heat flux (λE) is larger, with standard deviations of averages of 18%. The dataset averaged over the different instruments fails to close the energy budget by 20%, significantly larger than the uncertainties in the individual flux corrections. However, if the largest individual turbulent flux estimates are considered, energy closure can be achieved, indicating that the closure gap is within the spread of the measurements. The uncertainty in λE feeds results in an uncertainty in the bulk stomatal resistance, which further adds to the uncertainties in the estimation of the canopy temperature that controls the exchange. The paper demonstrated how a consensus dataset was derived, which is used by the individual investigators to calculate fluxes and drive their models.
Nemitz, E., Hargreaves, K. J., Neftel, A., Loubet, B., Cellier, P., Dorsey, J. R., Flynn, M., Hensen, A., Weidinger, T., Meszaros, R., Horvath, L., Dämmgen, U., Frühauf, C., Löpmeier, F. J., Gallagher, M. W., and Sutton, M. A.: Intercomparison and assessment of turbulent and physiological exchange parameters of grassland, Biogeosciences, 6, 1445-1466, doi:10.5194/bg-6-1445-2009, 2009.