Tornado Map Live Doppler Radar & Warning Loop
Tornado map live interactive view provides real-time vector warning polygons, NEXRAD Doppler radar reflectivity, and supercell rotation scans.
How to Track Severe Weather on the Interactive Tornado Map
Follow these actionable steps to locate active rotation, evaluate radar reflectivity, and monitor storm trajectories in real time.
Locate Your Area
Pan across the interactive map or use zoom gestures to center on your specific county, city, or neighborhood.
Inspect Warning Polygons
Click or tap on any red polygon (Tornado Warning) or amber polygon (Tornado Watch) to view official emergency timing, affected communities, and sheltering advice.
Animate Radar Loop
Press the Play button on the timeline controller at the bottom of the map to animate past radar scans and determine storm speed and directional heading.
Decode Radar Colors (dBZ)
Cross-reference the radar colors on the map against the dBZ scale below to spot heavy rain, destructive hail cores, or hook echo rotation.
Doppler Radar Reflectivity (dBZ) Guide
NEXRAD Doppler weather radar measures the microwave energy reflected back by precipitation particles (measured in decibels of reflectivity, or dBZ). Higher dBZ values signify heavier precipitation, destructive hail, or tornadic debris lofted thousands of feet into the sky.
Very Light Rain
Mist, drizzle, or light virga evaporating before reaching the surface.
Moderate Rain
Steady stratiform rainfall and early convective thunder initiation.
Heavy Rain / Hail
Intense torrential downpours, lightning cores, and small pea-sized hail.
Severe Core / Hail
Violent supercell updrafts, golf-ball or baseball hail, and intense downdrafts.
Tornadic Debris Ball
Extreme reflectivity signature indicating lofted structural debris inside the vortex.
Critical Tornadic Radar Signatures
How National Weather Service meteorologists identify rotating mesocyclones and confirm ground touchdowns on Doppler radar.
The Classic Hook Echo
A hook echo is a distinctive curved reflectivity pattern extending from the southwest flank of a supercell. It forms when precipitation is swept around the storm's rotating mesocyclone updraft by the Rear Flank Downdraft (RFD), indicating where a tornado is actively forming or touching down.
Tornadic Debris Signature (TDS)
When a tornado touches down, it lofts trees, shingles, and structural debris into the vortex. Dual-polarization radar detects this as a Tornadic Debris Signature (TDS)—characterized by high reflectivity paired with a sharp drop in Correlation Coefficient (CC < 0.8), confirming a damaging tornado on the ground.
Tornado Radar Map FAQ
Common questions regarding interactive radar tracking and polygon overlays.
Explore Severe Weather Intelligence
Access nationwide emergency metrics, live outbreak tables, and historical state climatology.