False color image of spray droplets being ejected from a breaking wave (left side of frame), taken in the laboratory. The droplets are moving from left to right in the air and the biggest drops are about 1-2 mm across. Credit: UM Rosenstiel School of Marine and Atmospheric Science – SUSTAIN laboratory, Ortiz-Suslow A University of Miami (UM) Rosenstiel School of Marine and Atmospheric Science research team is studying sea spray to help improve forecasting of hurricanes and tropical cyclones. In a recent study, the scientists found that in high winds conditions the amount of large sea spray droplets (over 0.5 milimeters in diameter) generated is as much as 1000 times more than previously thought.
Sea spray droplets are aerosol water particles that are ejected into the atmosphere as waves break at the ocean surface. The evaporation of sea spray is thought to contribute to the transfer of heat from the ocean to the atmosphere, which accelerate winds in a storm, potentially impacting its intensity.
To characterize the role these large droplets play at the air-sea surface, the researchers placed a high-resolution camera system outside of the Air-Sea Interaction Saltwater Tank (ASIST), one of the wind-wave basins in the UM SUSTAIN laboratory, to capture the silhouettes of water droplets flying through the air. For each image, an automatic identification algorithm was used to identify an individual droplet’s location in space and their two-dimensional surface area. More than 35,000 individual images were acquired and processed for this study as part of the experimental trials. The wind speeds in the laboratory ranged from 80 to 120 miles per hour.
In an analysis of how the droplet concentration changed with height above the ocean surface, they found that the vertical distribution of sea spray diverged from the existing theoretical distribution, which means the number of water droplets for a given air volume at a specific height above the ocean surface was significantly different than the predicted concentration. This information is critical to understanding the depth of the spray layer above the ocean surface and the overall impact of spray on storm intensity.
”Our work can be directly applied to a hurricane model to help improve hurricane intensity predictions, which will help people make more informed decisions with regard to their safety,” said David Ortiz-Suslow, a Ph.D. candidate at the UM Rosenstiel School and lead author of the study.
Over the last 10 years, scientists have made significant progress in predicting the track of tropical cyclones up to 72 hours. Three days before Hurricane Katrina made landfall in New Orleans, the National Weather Service predicted the hurricane would hit the Florida Panhandle, approximately 250 miles away. This year, Hurricane Matthew’s actual verses predicted paths were less than 50 miles apart in the 72-hour window. Intensity forecasting has not improved as sufficiently over the last 10 years.
The study, titled ”Sea Spray Generation in Very High Winds,” was published in the Oct. 2016 issue of the American Meteorological Society’s Journal of the Atmospheric Sciences.
Explore further:High-speed imagery captures new sea spray formation mechanism
More information: David G. Ortiz-Suslow et al, Sea Spray Generation in Very High Winds, Journal of the Atmospheric Sciences (2016). DOI: 10.1175/JAS-D-15-0249.1
Provided by:University of Miami