TY - JOUR

T1 - Spatial representativeness of single tower measurements and the imbalance problem with eddy-covariance fluxes

T2 - Results of a large-eddy simulation study

AU - Steinfeld, Gerald

AU - Letzel, Marcus Oliver

AU - Raasch, Siegfried

AU - Kanda, Manabu

AU - Inagaki, Atsushi

N1 - Funding Information: Acknowledgements This study was supported by the DADD Host-Program and a grant “Falressti pendium für Graduierte” of German Academic Exchange Service (DAAD), the Japanese Ministry of Education, Culture, Sports, Science and Technology (MEXT), the Core Research for evolutional science and technology (CREST) program of the Japan Science and Technology Agency (JST) and in parts through the German Science Foundation (DFG) under grant RA-617/13-1. Calculations were performed on the IBM Regatta P690 series of the “Norddeutscher Verbund für Hoch-und Höchs-tleistungsrechnen” (HLRN) in Hannover/Berlin, Germany, and partly on the SGI Origin 2000 of the Global Scientific Information and Computing Center, Tokyo Institute of Technology, Japan. We thank Henk de Bruin and one anonymous reviewer for their valuable comments on an earlier draft of this paper. The first author is grateful to Susanne Keyn for her valuable comments on the manuscript and wishes to thank Yu Nakayama for his help editing several figures.

PY - 2007/4

Y1 - 2007/4

N2 - A large-eddy simulation (LES) study is presented that investigates the spatial variability of temporal eddy covariance fluxes and the systematic underestimation of representative fluxes linked to them. It extends a prior numerical study by performing high resolution simulations that allow for virtual measurements down to 20 m in a convective boundary layer, so that conditions for small tower measurement sites can be analysed. It accounts for different convective regimes as the wind speed and the near-surface heat flux are varied. Moreover, it is the first LES imbalance study that extends to the stable boundary layer. It reveals shortcomings of single site measurements and the necessity of using horizontally-distributed observation networks. The imbalances in the convective case are attributed to a locally non-vanishing mean vertical advection due to turbulent organised structures (TOS). The strength of the TOS and thus the imbalance magnitude depends on height, the horizontal mean wind and the convection type. Contrary to the results of a prior study, TOS cannot generally be responsible for large energy imbalances: at low observation heights (corresponding to small towers and near-surface energy balance stations) the TOS related imbalances are generally about one order of magnitude smaller than those in field experiments. However, TOS may cause large imbalances at large towers not only in the case of cellular convection and low wind speeds, as found in the previous study, but also in the case of roll convection at large wind speeds. In the stably stratified boundary layer for all observation heights neither TOS nor significant imbalances are observed. Attempting to reduce imbalances in convective situations by applying the conventional linear detrending method increases the systematic flux underestimation. Thus, a new filter method is proposed.

AB - A large-eddy simulation (LES) study is presented that investigates the spatial variability of temporal eddy covariance fluxes and the systematic underestimation of representative fluxes linked to them. It extends a prior numerical study by performing high resolution simulations that allow for virtual measurements down to 20 m in a convective boundary layer, so that conditions for small tower measurement sites can be analysed. It accounts for different convective regimes as the wind speed and the near-surface heat flux are varied. Moreover, it is the first LES imbalance study that extends to the stable boundary layer. It reveals shortcomings of single site measurements and the necessity of using horizontally-distributed observation networks. The imbalances in the convective case are attributed to a locally non-vanishing mean vertical advection due to turbulent organised structures (TOS). The strength of the TOS and thus the imbalance magnitude depends on height, the horizontal mean wind and the convection type. Contrary to the results of a prior study, TOS cannot generally be responsible for large energy imbalances: at low observation heights (corresponding to small towers and near-surface energy balance stations) the TOS related imbalances are generally about one order of magnitude smaller than those in field experiments. However, TOS may cause large imbalances at large towers not only in the case of cellular convection and low wind speeds, as found in the previous study, but also in the case of roll convection at large wind speeds. In the stably stratified boundary layer for all observation heights neither TOS nor significant imbalances are observed. Attempting to reduce imbalances in convective situations by applying the conventional linear detrending method increases the systematic flux underestimation. Thus, a new filter method is proposed.

KW - Convective boundary layer

KW - Eddy covariance

KW - Imbalance problem

KW - Large-eddy simulation

KW - Stable boundary layer

KW - Turbulent fluxes

UR - http://www.scopus.com/inward/record.url?scp=33947678132&partnerID=8YFLogxK

U2 - 10.1007/s10546-006-9133-x

DO - 10.1007/s10546-006-9133-x

M3 - Article

AN - SCOPUS:33947678132

VL - 123

SP - 77

EP - 98

JO - Boundary-Layer Meteorology

JF - Boundary-Layer Meteorology

SN - 0006-8314

IS - 1

ER -