An investigation of the effects of wave state and sea spray on an idealized typhoon using an air-sea coupled modeling system |
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Authors: | Bin Liu Changlong Guan Li’an Xie Dongliang Zhao |
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Institution: | Department of Marine, Earth and Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695, USA,
Physical Oceanography Laboratory, Ocean University of China, Qingdao 266100;Physical Oceanography Laboratory, Ocean University of China, Qingdao 266100;Department of Marine, Earth and Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695, USA;Physical Oceanography Laboratory, Ocean University of China, Qingdao 266100 |
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Abstract: | In this study, the impact of atmosphere--wave coupling on typhoon intensity
was investigated using numerical simulations of an idealized typhoon in a
coupled atmosphere--wave--ocean modeling system. The coupling between
atmosphere and sea surface waves considered the effects of wave state and
sea sprays on air--sea momentum flux, the atmospheric low-level dissipative
heating, and the wave-state-affected sea-spray heat flux. Several
experiments were conducted to examine the impacts of wave state, sea sprays,
and dissipative heating on an idealized typhoon system. Results show that
considering the wave state and sea-spray-affected sea-surface roughness
reduces typhoon intensity, while including dissipative heating intensifies
the typhoon system. Taking into account sea spray heat flux also strengthens
the typhoon system with increasing maximum wind speed and significant wave
height. The overall impact of atmosphere--wave coupling makes a positive
contribution to the intensification of the idealized typhoon system. The
minimum central pressure simulated by the coupled atmosphere--wave
experiment was 16.4 hPa deeper than that of the control run, and the maximum
wind speed and significant wave height increased by 31% and 4%,
respectively. Meanwhile, within the area beneath the typhoon center, the
average total upward air--sea heat flux increased by 22%, and the
averaged latent heat flux increased more significantly by 31% compared to
the uncoupled run. |
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Keywords: | wave state sea spray dissipative heating tropical cyclone |
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