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Prikaz brzine i azimuta×Toplinski vjetar×
PodručjeMeteorologijaMeteorologija
ObiteljProcess / pipelineProcess / pipeline
Godina nastanka19681920s
TvoracBrowning and WexlerJacobbian insights from geostrophic flow
VrstaRadar wind retrieval methodWind-temperature relationship
Temeljni izvorBrowning, 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 ↗
Drugi naziviVAD, VAD analysis, Velocity-height profileThermal wind, Vertical wind shear, Barotropic
Srodne33
SažetakThe 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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ScholarGateUsporedite metode: Velocity-Azimuth Display · Thermal Wind. Preuzeto 2026-06-19 s https://scholargate.app/hr/compare