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Event Time
3:30 p.m.
Atlantic Building Room 2400 & Zoom

AOSC Seminar by Dr. Allison Wing, 11/10/2022

AOSC Seminar

Dr. Allison Wing



Title: Acceleration of tropical cyclone development by cloud-radiative feedbacks


A complete understanding of the development of tropical cyclones (TC) remains elusive and forecasting TC intensification remains challenging. Furthermore, while global climate model (GCM) simulation of TCs has improved significantly in recent years, significant biases remain. This motivates further research into the physical processes that govern TC development as well as the development of process-oriented diagnostics for GCMs, to identify processes to target for model improvement. 

Here, I investigate the importance of radiative feedbacks in TC development and the mechanisms underlying their influence is investigated in a set of idealized convection-permitting simulations. Radiative feedbacks in the context of a TC arise from interactions between spatially and temporally varying radiative heating and cooling (driven by the dependence of radiative heating and cooling rate on clouds and water vapor) and the developing TC (the circulation of which shapes the structure of clouds and water vapor). Tropical storm formation is delayed by a factor of two or three when radiative feedbacks are removed and the TC’s intensification rate is greater when longwave radiative feedbacks are stronger.  Further analysis pinpoints the longwave radiative feedback contributed by ice clouds as the strongest influence. 

Improving the representation of cloud-radiative feedbacks in forecast models therefore has the potential to yield critical advancements in TC prediction, but this requires a better understanding of cloud-radiative feedbacks in observed TCs. I present ongoing work that investigates these processes in the CloudSat TC overpass dataset. We examine the vertical and radial structure of ice and liquid clouds and the implications of the heterogeneous cloud distribution for spatial variability in radiative heating rates. Radiative transfer calculations using the CloudSat cloud property retrievals indicate that most of the spatial variability in longwave heating rates comes from ice clouds, as in the idealized simulations. The longwave cloud radiative feedback is found to be strongest in TCs undergoing rapid intensification. 



Allison Wing is an Associate Professor in the Department of Earth, Ocean and Atmospheric Science (EOAS) at Florida State University (FSU). She received her B.S. in Atmospheric Science in 2008 from Cornell University and Ph.D. in Atmospheric Science in 2014 from MIT. After graduating from MIT, Prof. Wing was an NSF Postdoctoral Research Fellow at Lamont-Doherty Earth Observatory of Columbia University, where she retains an appointment as an Adjunct Associate Research Scientist. She joined FSU in December 2016, where she has developed a research program that uses theory, idealized numerical modeling, and analysis of observations and comprehensive climate models to study tropical convection, tropical cyclones and climate. In recognition of her achievements, Prof. Wing was awarded an Outstanding Early Career Award by the American Meteorological Society's Committee on Tropical Meteorology and Tropical Cyclones and was named one of the “Brilliant 10” young scientists and engineers by Popular Science magazine. 


Contact:Jonathan Poterjoy

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AOSC Seminar

Pre-seminar refreshment: N/A
Seminar: 3:30-4:30pm, Room: ATL 2400(only when in-person)
Meet-the-Speaker: 4:30-5:00pm, Room: ATL 3400(only when in-person) [For AOSC Students only]

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