Author: AOML Communications

Sally Intensifies Near the Gulf Coast as Observed by NOAA Reconnaissance

NOAA’s G-IV and two P-3 Hurricane Hunter aircraft took off from Lakeland, FL at 10:30 AM, 1:30 PM and 4:30 PM EDT on September 14th to investigate Hurricane Sally’s circulation. AOML scientists providing onboard and remote support for these missions ensure that Tail Doppler Radar, dropsonde, and Stepped Frequency Microwave Radiometer (SFMR) measurements allow for adequate coverage of the storm environment.

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Testing the Trade Wind Charging Mechanism and Its Influence on ENSO Variability

In a new article published in the Journal of Climate, scientists at AOML and the Cooperative Institute for Marine and Atmospheric Science, with collaborators at Boston University, Texas A&M, and North Carolina State University, document the role of ocean dynamics in linking Pacific atmospheric variability to El Niño-Southern Oscillation (ENSO) event generation. The results of the study could be used as a potential predictor of ENSO events up to a year in advance.

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Update to the BEACHES Study: Children Visiting Beaches with Open Wounds are More Susceptible to Bacterial Infection

A new paper appearing in the International Journal of Environmental Research and Public Health examines how the presence of children’s open wounds and abrasions during play at the beach may put them at greater risk of skin infections from marine bacteria and other pathogens they encounter. The study finds that children with existing or newly-acquired wounds while at the beach are more susceptible to infection.

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NOAA’s Multi-Storm HWRF-B Model Uses Atmosphere/Ocean Interactions to Improve Tropical Cyclone Forecasts

A recent paper published in Atmosphere introduces a new update to the Basin-Scale Hurricane Weather Research and Forecasting (HWRF-B) model, which pairs an atmospheric model with an ocean model via new coupling technology to forecast several tropical cyclones simultaneously. This model, shown to improve forecast skill, was developed at AOML in collaboration with NOAA’s Environmental Modeling Center and the Developmental Testbed Center.

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The Atlantic Niño: El Niño’s Little Brother

Despite their differences, it is still widely thought that Atlantic Niño is analogous to El Niño in many ways. Specifically, the atmosphere-ocean feedback responsible for the onset of Atlantic Niño is believed to be similar to that of El Niño, a process known as Bjerknes feedback. The near-surface trade winds blow steadily from east to west along the equator. When weaker-than-normal trade winds develop in the western Atlantic basin, downwelling equatorial Kelvin waves propagate to the eastern basin, deepening the thermocline and making it harder for the colder, deeper water to affect the surface.

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