Calibrating in sheared-flow Sample Clauses

Calibrating in sheared-flow. All wind lidar calibrations occur in field conditions where it is impossible to control the wind conditions. In particular the wind shear varies constantly – no two wind shear profiles are ever precisely the same. From our understanding of the physics of lidars, we know that sheared-flows can give rise to wind speed errors since the lidar is performing a non-linear weighting of an often non-linear speed profile. Contemporary lidars make no attempt to mitigate these errors and in our current calibration procedure, these effects are essentially ignored. The intention of this sub-task is to examine alternative ways of describing the speed profile than the traditional power law alpha exponent in the hope that the shear induced errors can be better identified. For example whilst some errors (for example a sensing height error) will essentially depend on the first derivative of speed with height, others (eg. due to asymmetric and non-linear weighting) will be more related to the second derivative. The goal is through more sophisticated profile descriptions, to both reduce the shear induced scatter in our calibrations and provide correction methods for operational measurements.
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