Research: Damaging Winds

There are a variety of types of damaging winds formed by different thunderstorm processes, but thunderstorms produce some straight-line winds when the thunderstorm downdraft hits the ground and flows outward. Anyone living in thunderstorm-prone areas of the world is at risk for experiencing this phenomenon. Winds can cause damage when they reach 50 mph.

Damaging Wind Research Areas

Types of Damaging Wind Events

We are working on simulations of derecho events, widespread, long-lived windstorms that are associated with bands of rapidly moving showers or thunderstorms. Derechos can produce widespread straight-line winds up to 100 mph over long periods of time. Our simulations allow us to dissect the storms that produce derechos to better understand how to forecast and warn for them.

Damaging Wind Evolution

A downburst is a strong downdraft which induces an outburst of damaging winds on or near the ground, and a microburst is a small but powerful downburst. Microburst winds can cause significant damage, and are a concern for forecasters because of their rapid onset and noted relevance for aircraft safety. It is difficult for a forecaster to anticipate which storm will produce a microburst. NSSL's dual-polarized mobile Doppler radar is used to collect data on microbursts and dust storms to compare with the Phoenix NWS dual-polarized radar data. NSSL and the NWS hope combining both data sets will reveal clues about their existence. NSSL also uses the National Weather Radar Testbed Phased Array Radar to capture of the evolution of damaging wind mechanisms when thunderstorms are within the sight of the radar.

Predicting Damaging Winds

NSSL developed an algorithm in collaboration with Arizona's Salt River Project (SRP) to alert the power company of the potential for a dust storm called a haboob. A haboob is a wall of dust that is pushed out along the ground from a thunderstorm downdraft at high speeds. The algorithm runs on NSSL's Multi-Radar Multi-Sensor (MRMS) system and automatically monitors the radar for thunderstorms reaching thresholds that could result in outflows producing strong surface winds and blowing dust. When thresholds are reached, SRP operational personnel receive an alert to prepare for the impact of wind loading on SRP power poles and substations.

While radar remains the number one tool for forecasters evaluating storms, lightning data may be able to provide additional clues because electrical charge generation in the storm updraft and ice microphysics are linked. NSSL is working to provide a physical understanding how three-dimensional lightning data may be used by forecasters for microburst or downburst prediction. Due to the rapid updates and high spatial resolution of both the phased array radar and the Oklahoma Lightning Mapping Array (LMA), both of these systems are able to capture the quick generation and evolution of microbursts.

Past Damaging Wind Research

Bow Echo and MCV Experiment (BAMEX)

BAMEX (Bow Echo and MCV Experiment) was a field experiment involving scientists from NSSL, NCAR, the NWS and OU that was designed to gather data to understand bow echoes and their resulting high damaging surface winds. The mobile project tried to understand and improve prediction of mesoscale and storm-scale processes that produce severe winds in bowing convective systems lasting at least four hours. The project used aircraft and mobile ground-based instruments to map the thermodynamic and environmental structure of thunderstorm complexes and mature mesoscale convective vortices.


An NSSL scientist studied low-altitude “mesovortices,” (atmospheric spin on the scale of a few km to several hundred km) and learned that they may be the one of the causes of damaging straight-line winds. These results helped motivate the objectives for the BAMEX program defined above.

Damaging Downburst Prediction and Detection Algorithm (DDPDA)

To help NWS forecasters, NSSL developed the Damaging Downburst Prediction and Detection Algorithm using radar-detectable features. The DDPDA works best predicting the onset of damaging downburst winds from high-reflectivity storm cells that develop in an environment of weak vertical shear.