Atmospheric characterization systems and methods
US-11879981-B2 · Jan 23, 2024 · US
US2020400836A1 · US · A1
| Field | Value |
|---|---|
| Publication number | US-2020400836-A1 |
| Application number | US-202016906105-A |
| Country | US |
| Kind code | A1 |
| Filing date | Jun 19, 2020 |
| Priority date | Jun 19, 2019 |
| Publication date | Dec 24, 2020 |
| Grant date | — |
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The invention relates to a method of determining the vertical profile of the wind speed upstream from a wind turbine (1), wherein wind speed measurements are performed by means of a LiDAR sensor (2), then the exponent α of the power law is determined by means of an unscented Kalman filter and measurements, and this exponent α is applied to the power law in order to determine the vertical wind speed profile.
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1 . A method of determining the vertical profile of the wind speed upstream from a wind turbine, the wind turbine being equipped with a LiDAR sensor facing upstream of the wind turbine, wherein the following steps are carried out: a) measuring (MES) the wind speed in at least one measurement plane (PM) upstream from the wind turbine at least at two measurement points (PT 1 , PT 2 , PT 3 , PT 4 ) located at different heights by means of the LiDAR sensor, b) constructing a model of the vertical wind speed profile (MOD) by means of a power law of the form: v z v z 0 = ( z z 0 ) α with vz the longitudinal wind speed at the height z, z0 the reference height, vz0 the longitudinal wind speed at the reference height z0 and α the exponent of the power law, c) determining the exponent α of the power law by means of an unscented Kalman filter using the wind speed measurements at the two measurement points (PT 1 , PT 2 , PT 3 , PT 4 ), and d) determining the vertical wind speed profile (PRO) by applying the determined exponent α to the vertical wind speed profile model. 2 . A method of determining the vertical profile of the wind speed as claimed in claim 1 , wherein the unscented Kalman filter is applied to a state model comprising additive noise and multiplicative noise. 3 . A method of determining the vertical profile of the wind speed as claimed in claim 2 , wherein the state model is written: { x ( k ) = x ( k - 1 ) + η ( k - 1 ) , y ( k ) = ( v 2 ( k ) + ϵ 2 ( k ) ) ( z 1 z 2 ) x ( k ) - ϵ 1 ( k ) with x(k)=α(k) the state variable at time k, y(k)=v 1 (k) the output of the state model corresponding to the longitudinal wind speed measured at time k at measurement point 1, η(k−1) the variation of exponent α at time k−1, v 2 (k) the longitudinal wind speed measured at time k at measurement point 2, z1 the height of measurement point 1, z2 the height of measurement point 2, ε1(k) the noise of speed v 1 at time k, and ε2(k) the noise of speed v 2 at time k. 4 . A method of determining the vertical profile of the wind speed as claimed in claim 2 wherein, for applying the Kalman filter, the increasing random variable x a is considered: x a ( k ) = [
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