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  2. Bulk Richardson number - Wikipedia

    en.wikipedia.org/wiki/Bulk_Richardson_number

    The Bulk Richardson Number (BRN) is an approximation of the Gradient Richardson number. [1] The BRN is a dimensionless ratio in meteorology related to the consumption of turbulence divided by the shear production (the generation of turbulence kinetic energy caused by wind shear) of turbulence.

  3. IEC 61400 - Wikipedia

    en.wikipedia.org/wiki/IEC_61400

    The extreme wind speeds are based on the 3 second average wind speed. Turbulence is measured at 15 m/s wind speed. This is the definition in IEC 61400-1 edition 2. For U.S. waters however, several hurricanes have already exceeded wind class Ia with speeds above the 70 m/s (156 mph), and efforts are being made to provide suitable standards. [8]

  4. Wind shear - Wikipedia

    en.wikipedia.org/wiki/Wind_shear

    Thermal wind is a meteorological term not referring to an actual wind, but a difference in the geostrophic wind between two pressure levels p 1 and p 0, with p 1 < p 0; in essence, wind shear. It is only present in an atmosphere with horizontal changes in temperature (or in an ocean with horizontal gradients of density ), i.e., baroclinicity .

  5. Downburst - Wikipedia

    en.wikipedia.org/wiki/Downburst

    Several fatal and historic crashes in past decades are attributed to the phenomenon and flight crew training goes to great lengths on how to properly recognize and recover from a downburst/wind shear event; wind shear recovery, among other adverse weather events, are standard topics across the world in flight simulator training that flight ...

  6. Monin–Obukhov length - Wikipedia

    en.wikipedia.org/wiki/Monin–Obukhov_length

    where is potential temperature, and is mixing ratio. By this definition, is usually negative in the daytime since ′ ′ ¯ is typically positive during the daytime over land, positive at night when ′ ′ ¯ is typically negative, and becomes infinite at dawn and dusk when ′ ′ ¯ passes through zero.

  7. Wind gradient - Wikipedia

    en.wikipedia.org/wiki/Wind_gradient

    In common usage, wind gradient, more specifically wind speed gradient [1] or wind velocity gradient, [2] or alternatively shear wind, [3] is the vertical component of the gradient of the mean horizontal wind speed in the lower atmosphere. [4] It is the rate of increase of wind strength with unit increase in height above ground level.

  8. Blade pitch - Wikipedia

    en.wikipedia.org/wiki/Blade_pitch

    Blade pitch control is a feature of nearly all large modern horizontal-axis wind turbines.It is used to adjust the rotation speed and the generated power. While operating, a wind turbine's control system adjusts the blade pitch to keep the rotor speed within operating limits as the wind speed changes.

  9. Von Kármán constant - Wikipedia

    en.wikipedia.org/wiki/Von_Kármán_constant

    where u is the mean flow velocity at height z above the boundary. The roughness height (also known as roughness length ) z 0 is where u {\displaystyle u} appears to go to zero. Further κ is the von Kármán constant being typically 0.41, and u ⋆ {\displaystyle u_{\star }} is the friction velocity which depends on the shear stress τ w at the ...