Articles Tagged: #Weather Radar
Expert meteorological analysis, safety guides, and radar tracking related to weather radar.
The Ultimate Guide to NEXRAD WSR-88D Dual-Polarization Radar Architecture
A comprehensive technical examination of the 160-station US NEXRAD WSR-88D S-band radar network, dual-polarization beam physics, and multi-tilt volume coverage patterns.
How to Read Doppler Radar Reflectivity (dBZ) Like a Professional Meteorologist
Master the logarithmic decibel of Z scale from 5 to 75+ dBZ. Learn to identify stratiform rain, supercell hail cores, bright band freezing levels, and storm cell intensity.
Dual-Pol Hydrometeor Classification: Differentiating Rain, Hail, Snow, and Debris
Explore the mathematical algorithms behind Correlation Coefficient (CC), Differential Reflectivity (ZDR), and Specific Differential Phase (KDP) in atmospheric hydrometeor typing.
Understanding Ground Clutter, Anomalous Propagation & False Radar Echoes
Learn why non-precipitation targets appear on Doppler radar. Discover how sharp temperature inversions, beam ducting, wind farms, and biological migrations create false weather echoes.
Terminal Doppler Weather Radar (TDWR): Airport Microburst & Wind Shear Detection
How the FAA and NWS deploy 45 dedicated C-band TDWR radar installations across major commercial airports to prevent aviation wind shear accidents and catastrophic landing crashes.
Multi-Radar Multi-Sensor (MRMS) System: The Next Frontier in Precipitation Estimation
Explore NOAA’s high-resolution MRMS framework combining radar networks, rain gauges, satellite observations, and numerical forecast models into a 1-kilometer national precipitation mosaic.
GOES-16 and GOES-18 Geostationary Satellites: Space-Based Severe Storm Nowcasting
Discover the advanced baseline imager (ABI) spectral bands, geostationary lightning mappers (GLM), and rapid 30-second mesoscale scans tracking severe thunderstorms from 22,236 miles in space.
High-Resolution Rapid Refresh (HRRR) vs GFS and ECMWF: Comparing Weather Forecast Models
An expert evaluation of convection-allowing models vs global numerical prediction systems. Understand spatial resolution, parameterized convection, and ensemble forecasting.
Supercell Thunderstorm Mechanics: Low-Precipitation, Classic, and High-Precipitation Cells
Unpack the atmospheric thermodynamics of rotating supercells. Learn how vertical wind shear tilts horizontal vorticity into explosive, long-lived convective rotating updrafts.
Microbursts, Macrobursts, and Downbursts: Aviation Hazard Physics and Home Safety
Explore evaporative cooling downdrafts, dry vs wet microburst thermodynamics, damaging divergent surface winds, and structural impact loading during summer storm collapses.
Giant Hail Formation: Updraft Velocity, Supercooled Droplets, and Growth Layers
Learn how violent 100+ mph storm updrafts suspend ice pellets in subfreezing cloud layers, accumulating concentric growth rings to produce record-breaking baseball and softball hailstones.
Aircraft Reconnaissance in Hurricanes: How NOAA and USAF Hurricane Hunters Sample Storms
Step inside WP-3D Orion and WC-130J aircraft penetrating the turbulent eyewalls of major hurricanes, collecting real-time SFMR surface wind speeds and GPS dropsonde atmospheric soundings.
The Science of Nor'easters: Bombogenesis and Mid-Atlantic Coastal Cyclones
How baroclinic instability along the Gulf Stream boundary triggers explosive cyclogenesis (bomb cyclones) dropping 24+ millibars in 24 hours, generating hurricane-force blizzard conditions.
Lake-Effect Snow Dynamics: Fetch Length, Over-Water Instability, and Snow Bands
Analyze Great Lakes sensible and latent heat fluxes, 850 mb temperature differentials, capping inversions, and narrow mesoscale bands dumping 5+ feet of snow in Buffalo and Watertown.
The Thermodynamics of Freezing Rain, Sleet, Snow, and Cold-Air Damming (CAD)
Vertical atmospheric temperature profiles dictate winter precipitation types. Learn how Appalachian Cold-Air Damming (CAD) traps subfreezing surface air to create catastrophic ice storms.
Snow Water Equivalent (SWE) and Snow-to-Liquid Ratios: Why 1 Inch of Rain Isn't 10 Inches of Snow
Crystal habit thermodynamics in the Dendritic Growth Zone (-12°C to -18°C). How temperature and wind alter snow-to-liquid ratios from heavy 5:1 concrete to fluffy 30:1 champagne powder.
Atmospheric Pressure and Barometric Altimetry: How Storm Fronts Alter Local Pressure
Unpack millibars, hectopascals, and inches of mercury. Learn how rapid barometric pressure drops predict storm intensity and explore physiological joint pain claims vs meteorological facts.