Abstract

In scintillometry Monin–Obukhov similarity theory (MOST) is used to calculate the surface sensible heat flux from the structure parameter of temperature \({(C_{T^2})}\) . In order to prevent saturation a scintillometer can be installed at an elevated level. However, in that case the observation level might be located outside the atmospheric surface layer (ASL) and thus the validity of MOST questioned. Therefore, we examine two concepts to determine the turbulent surface sensible heat flux from the structure parameter at elevated levels with data obtained at 60-m height on the Cabauw tower (the Netherlands). In the first concept (MOSTs) \({C_{T^2}}\) is still scaled with the surface flux, whereas in the second (MOSTl) \({C_{T^2}}\) is scaled with the local sensible heat flux. The \({C_{T^2}}\) obtained from both concepts is compared with direct observations of \({C_{T^2}}\) using a sonic anemometer/thermometer. In the afternoon (when the measurement height is located within the ASL) both concepts give results that are comparable to the directly observed values of \({C_{T^2}}\) . In the morning (data outside the ASL), our data do not unequivocally support either of the two concepts. First, the peak in \({C_{T^2}}\) that occurs when the measurement height is located in the entrainment zone disqualifies the use of MOST. Second, during the morning transition, local scaling shows the correct pattern (zero flux and a minimum in \({C_{T^2}}\)) but underestimates \({C_{T^2}}\) by a factor of ten. Third, from the best linear fit a we found that the slope of MOSTl gave better results, whereas the offset is closer to zero for MOSTs. Further, the correlation between the direct observations and MOST-scaled results is low and similar for the two concepts. In the end, we conclude that MOST is not applicable for the morning hours when the observation level is above the ASL.

Highlights

  • The area-averaged surface flux of sensible heat is of interest for many meteorological and hydrological studies, e.g. to evaluate mesoscale numerical models or satellite-based retrieval algorithms

  • The surface sensible heat flux is derived by applying Monin–Obukhov similarity theory (MOST) (Wyngaard 1973; Meijninger 2003; Moene et al 2004), which is valid for the atmospheric surface layer (ASL), where fluxes are assumed to vary little with height

  • MOST is based on the observation that the statistics of turbulence in the surface layer are fully determined by four parameters: the surface flux of the scalar under consideration, the friction velocity u∗, the buoyancy flux g/(T w Tv) and the height above the surface z (Wyngaard 1973; Stull 1988; Meijninger 2003; Moene et al 2004)

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Summary

Introduction

The area-averaged surface flux of sensible heat is of interest for many meteorological and hydrological studies, e.g. to evaluate mesoscale numerical models or satellite-based retrieval algorithms. In order to obtain the surface sensible heat flux from the structure parameter of temperature at elevated levels under unstable conditions, two different theoretical concepts are proposed. The structure parameter of temperature at elevated levels has to be scaled with the local sensible heat flux, rather than with the surface flux. The main question is how the surface sensible heat flux should be determined from the structure parameter of temperature determined at 60 m under unstable conditions, during the morning period when the level of 60 m is situated above the ASL. 3. Section 4 provides a description of the boundary-layer structure, a similarity study of the MOST relationships with the data observed in the ASL is presented, and the two proposed concepts are compared.

Theory
Research Strategy and Methods
Research Strategy
The Structure Parameter of Temperature
Turbulent Heat Fluxes
The Scintillometer
The Structure of the Boundary Layer
Discussions and Conclusions
Full Text
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