Results from One-Year Continuous Operation of a Large Aperture Scintillometer over a Heterogeneous Land Surface

A large-aperture scintillometer (LAS) was operated continuouslyduring a period of more than one year over a heterogeneous land surface in Central Europeat the transition between marine and continental climates. The LAS measurements of the refractiveindex structure parameter, CN2, were used to estimate the sensible heat flux. Thiswas possible for about 60to 80% of the time under daytime conditions during thesummer, with lower values obtained for the cold season (October to March). Using datafrom a three-week long field experiment, the LAS-based heat flux was compared with a weighedaverage of local heat flux measurements over the main land use classes (forest, agriculture,water) in the area, resulting in reasonable agreement. LAS-based heat fluxes were then used forcomparison with the heat flux values of a numerical weather prediction model. An over-predictionof the model heat flux was found in summer but the modelled values were lower than the LASderived data during the cold season.

[1]  Regional-scale surface flux observations across the boreal forest during BOREAS , 1997 .

[2]  J. Garratt The Atmospheric Boundary Layer , 1992 .

[3]  B. Hurk,et al.  The scintillation method tested over a dry vineyard area , 1995 .

[4]  M. Tjernström,et al.  Regional surface fluxes over the NOPEX area , 1998 .

[5]  B. Hurk,et al.  A verification of some methods to determine the fluxes of momentum, sensible heat, and water vapour using standard deviation and structure parameter of scalar meteorological quantities , 1993 .

[6]  Armin Raabe,et al.  A comparison of two strategies on land surface heterogeneity used in a mesoscale β meteorological model , 1996 .

[7]  Roger A. Pielke,et al.  A parameterization of heterogeneous land surfaces for atmospheric numerical models and its impact on regional meteorology , 1989 .

[8]  Roni Avissar,et al.  Representation of heterogeneity effects in Earth system modeling: Experience from land surface modeling , 1997 .

[9]  Larry Mahrt,et al.  The bulk aerodynamic formulation over heterogeneous surfaces , 1996 .

[10]  Reginald J. Hill,et al.  Algorithms for Obtaining Atmospheric Surface-Layer Fluxes from Scintillation Measurements , 1997 .

[11]  W. Meijninger,et al.  The sensible heat fluxes over irrigated areas in western Turkey determined with a large aperture scintillometer. , 2000 .

[12]  Stuart A. Collins,et al.  Behavior of the Refractive-Index-Structure Parameter near the Ground* , 1971 .

[13]  F. Beyrich,et al.  The LITFASS project of DWD and the LITFASS-98 experiment: The project strategy and the experimental setup , 2002 .

[14]  A. Chehbouni,et al.  Estimation of heat and momentum fluxes over complex terrain using a large aperture scintillometer , 2000 .

[15]  G. R. Ochs,et al.  Measuring surface-layer fluxes of heat and momentum using optical scintillation , 1992 .

[16]  A. E. Green,et al.  Path-averaged surface fluxes determined from infrared and microwave scintillometers , 2001 .

[17]  Bruno Monteny,et al.  Effective parameters of surface energy balance in heterogeneous landscape , 1994 .

[18]  Martin Claussen,et al.  Estimation of areally-averaged surface fluxes , 1991 .

[19]  W. Kohsiek,et al.  Measuring CT2, CQ2, and CTQ in the unstable surface layer, and relations to the vertical fluxes of heat and moisture , 1982 .

[20]  V. Thiermann,et al.  The measurement of turbulent surface-layer fluxes by use of bichromatic scintillation , 1992 .

[21]  D. Lüthi,et al.  The Soil-Precipitation Feedback: A Process Study with a Regional Climate Model , 1999 .

[22]  A. E. Green,et al.  Surface-layer scintillation measurements of daytime sensible heat and momentum fluxes , 1994 .