On the Retrieval of Surface-Layer Parameters from Lidar Wind-Profile Measurements

Author:

Araújo da Silva Marcos Paulo1ORCID,Salcedo-Bosch Andreu1ORCID,Rocadenbosch Francesc12ORCID,Peña Alfredo3ORCID

Affiliation:

1. CommSensLab-UPC, Department of Signal Theory and Communications, Universitat Politècnica de Catalunya (UPC), C/ Jordi Girona, 1-3, 08034 Barcelona, Spain

2. Institut d’Estudis Espacials de Catalunya (Institute of Space Studies of Catalonia, IEEC), 08034 Barcelona, Spain

3. DTU Wind and Energy Systems, Technical University of Denmark, Frederiksborgvej 399, 4000 Roskilde, Denmark

Abstract

We revisit two recent methodologies based on Monin–Obukhov Similarity Theory (MOST), the 2D method and Hybrid-Wind (HW), which are aimed at estimation of the Obukhov length, friction velocity and kinematic heat flux within the surface layer. Both methods use wind-speed profile measurements only and their comparative performance requires assessment. Synthetic and observational data are used for their quantitative assessment. We also present a procedure to generate synthetic noise-corrupted wind profiles based on estimation of the probability density functions for MOST-related variables (e.g., friction velocity) and the statistics of the noise-corrupting perturbational amplitude found during an 82-day IJmuiden observational campaign. In the observational part of the study, 2D and HW parameter retrievals from floating Doppler wind lidar measurements are compared against those from a reference mast. Overall, the 2D algorithm outperformed the HW in the estimation of all the three parameters above. For instance, when assessing the friction-velocity retrieval performance with reference to sonic anemometers, determination coefficients of ρ2D2=0.77 and ρHW2=0.33 were found under unstable atmospheric stability conditions, and ρ2D2=0.81 and ρHW2=0.07 under stable conditions, which suggests the 2D algorithm as a prominent method for estimating the above-mentioned surface-layer parameters.

Publisher

MDPI AG

Subject

General Earth and Planetary Sciences

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