NASA Data May Help Improve Estimates of a Hurricane's Punch
As Tropical Storm Noel churns off Florida's east coast, NASA and university scientists have announced they have developed a promising new technique for estimating the intensity of tropical cyclones from space. The method could one day supplement existing techniques, assist in designing future tropical cyclone satellite observing systems, and improve disaster preparedness and recovery efforts.
The technique uses NASA satellite data, including simultaneous, accurate measurements of cloud-top temperatures from the Moderate Resolution Imaging Spectroradiometer on NASA's Aqua satellite, and cloud-top height and cloud profiling information from NASA's CloudSat satellite. Both satellites fly in formation as part of NASA's "A-Train" of Earth-observing satellites. This new technique was developed by scientists at NASA's Jet Propulsion Laboratory, Pasadena, Calif.; Colorado State University, Fort Collins, Colo.; and the Massachusetts Institute of Technology, Cambridge, Mass.
Scientists commonly use measurements of a tropical cyclone's maximum sustained winds to define their intensity and gauge their destructive potential. Maximum sustained winds are defined as the one-minute average wind speed at an altitude of 10 meters (33 feet).
The framework used by the team to estimate tropical cyclone intensity was developed by co-author Kerry Emanuel of the Massachusetts Institute of Technology and his colleague Valerie Wong. It requires cloud profiling information from over or near a storm's eye. Of the more than 150 tropical cyclones that CloudSat flew over during its first six months after launch in April 2006, nine of the storm overpasses met this criterion.
The team analyzed NASA satellite data from these nine storms and calculated their peak winds. The estimates were then compared with available weather data, including data from aircraft. Initial results show the technique's estimates agreed with available weather data, and the technique appeared to work better for stronger storms.
Emanuel and Wong's framework measures the intensity of tropical cyclones in relation to the total energy contained in both their eyewalls and the surrounding environment outside the storms, as well as other measurements. By coupling measurements of temperatures and cloud top heights from a storm's eyewall out to its outer regions with an estimated difference in temperature between the sea surface and the storm's cloud tops, a storm's intensity can be estimated.
"Our study represents a unique and first-of-a-kind test of a hurricane intensity theory that had not been verified against real-world data, one that relies on actual satellite data," said lead study author Zhengzhao "Johnny" Luo, now with the City College of New York. "While our analysis is not yet mature enough for this technique to be used operationally, we plan to further refine it as more tropical cyclone data become available."
Meteorological satellites have been used to monitor tropical cyclones since the mid 1960s. Relating measurements of storm intensity to existing satellite data has proven difficult. The primary technique used since the mid 1970s, developed by Vernon Dvorak of the National Oceanic and Atmospheric Administration, estimates a storm's maximum sustained winds by looking for recognizable patterns of clouds in visible and infrared satellite images and calibrating them against reconnaissance aircraft data.
CloudSat Principal Investigator and study co-author Graeme Stephens of Colorado State University, Fort Collins, Colo., said the latest results show the value of being able to look inside storms to reveal their inner structure. This information is unique to CloudSat. "Current hurricane intensity estimating techniques are generally effective but have higher wind speed errors than scientists would like," he said. "This new technique may reduce those error rates."
Results of the study are published in the September issue of the Institute of Electrical and Electronics Engineers publication, Geoscience and Remote Sensing Letters.