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Velocity-Azimuth Display×Thermal Wind×
FachgebietMeteorologieMeteorologie
FamilieProcess / pipelineProcess / pipeline
Entstehungsjahr19681920s
UrheberBrowning and WexlerJacobbian insights from geostrophic flow
TypRadar wind retrieval methodWind-temperature relationship
Wegweisende QuelleBrowning, K. A., & Wexler, R. (1968). The determination of kinematic properties of a wind field using Doppler radar. Journal of Applied Meteorology, 7(1), 105-113. DOI ↗Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press. link ↗
AliasnamenVAD, VAD analysis, Velocity-height profileThermal wind, Vertical wind shear, Barotropic
Verwandt33
ZusammenfassungThe Velocity-Azimuth Display (VAD) is a radar analysis technique that extracts the radial velocity of wind at a constant altitude as a function of azimuth angle around the radar. By fitting a sinusoidal pattern to these measurements, VAD retrieves the mean wind speed and direction at that altitude, providing wind profiles without requiring multiple radar observations.The thermal wind relationship is a fundamental meteorological principle that links vertical wind shear to horizontal temperature gradients. It states that wind speed increases with height in the direction of warming—a direct consequence of hydrostatic and geostrophic balance combined with the ideal gas law.
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ScholarGateMethoden vergleichen: Velocity-Azimuth Display · Thermal Wind. Abgerufen am 2026-06-18 von https://scholargate.app/de/compare