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वेग-दिगंश प्रदर्शन (Velocity-Azimuth Display)×द्वि-ध्रुवीकरण रडार×WRF मॉडल×
क्षेत्रमौसम विज्ञानमौसम विज्ञानमौसम विज्ञान
परिवारProcess / pipelineProcess / pipelineProcess / pipeline
उद्भव वर्ष19681990s2000
प्रवर्तकBrowning and WexlerBringi, ChandrasekarSkamarock and Klemp
प्रकारRadar wind retrieval methodRadar measurement techniqueAtmospheric simulation system
मौलिक स्रोतBrowning, 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 ↗Kumjian, M. R. (2013). The impact of precipitation on supercell electrification: Lightning potential and storm structure changes. Journal of the Atmospheric Sciences, 69(11), 3353-3375. link ↗Skamarock, W. C., Klemp, J. B., Dudhia, J., et al. (2008). A Description of the Advanced Research WRF Version 3. NCAR Technical Note NCAR/TN-475+STR. link ↗
उपनामVAD, VAD analysis, Velocity-height profileDual-pol radar, Polarimetric radar, Dual-polarization, Dual-polWeather Research and Forecasting, WRF, ARW, NMM
संबंधित334
सारांशThe 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.Dual-polarization (dual-pol) radar is a weather radar system that transmits and receives electromagnetic waves in both horizontal and vertical polarizations simultaneously. This technique, operational in weather services since the 2010s, provides detailed information about precipitation particle type, shape, and size distribution, enabling improved rainfall estimates and better discrimination of hail, rain, and snow.The Weather Research and Forecasting (WRF) model is a mesoscale atmospheric simulation system used for weather forecasting, research, and climate applications. Developed cooperatively by NCAR, NOAA, and academic institutions, WRF became operational in 2004 and has become one of the most widely used atmospheric models worldwide.
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