Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/85136
Title: The effects of sea spray and atmosphere–wave coupling on air–sea exchange during a tropical cyclone
Authors: Garg, Nikhil
Ng, Eddie Yin Kwee
Narasimalu, Srikanth
Keywords: Sea Spray
Atmosphere
Issue Date: 2018
Source: Garg, N., Ng, E. Y. K., & Narasimalu, S. (2018). The effects of sea spray and atmosphere–wave coupling on air–sea exchange during a tropical cyclone. Atmospheric Chemistry and Physics, 18(8), 6001-6021.
Series/Report no.: Atmospheric Chemistry and Physics
Abstract: The study investigates the role of the air–sea interface using numerical simulations of Hurricane Arthur (2014) in the Atlantic. More specifically, the present study aims to discern the role ocean surface waves and sea spray play in modulating the intensity and structure of a tropical cyclone (TC). To investigate the effects of ocean surface waves and sea spray, numerical simulations were carried out using a coupled atmosphere–wave model, whereby a sea spray microphysical model was incorporated within the coupled model. Furthermore, this study also explores how sea spray generation can be modelled using wave energy dissipation due to whitecaps; whitecaps are considered as the primary mode of spray droplets generation at hurricane intensity wind speeds. Three different numerical simulations including the sea- state-dependent momentum flux, the sea-spray-mediated heat flux, and a combination of the former two processes with the sea-spray-mediated momentum flux were conducted. The foregoing numerical simulations were evaluated against the National Data Buoy Center (NDBC) buoy and satellite altimeter measurements as well as a control simulation using an uncoupled atmosphere model. The results indicate that the model simulations were able to capture the storm track and intensity: the surface wave coupling results in a stronger TC. Moreover, it is also noted that when only spray-mediated heat fluxes are applied in conjunction with the sea-state-dependent momentum flux, they result in a slightly weaker TC, albeit stronger compared to the control simulation. However, when a spray-mediated momentum flux is applied together with spray heat fluxes, it results in a comparably stronger TC. The results presented here allude to the role surface friction plays in the intensification of a TC.
URI: https://hdl.handle.net/10356/85136
http://hdl.handle.net/10220/45143
ISSN: 1680-7316
DOI: 10.5194/acp-18-6001-2018
Rights: © 2018 The Author(s). This work is distributed under the Creative Commons Attribution 4.0 License.
Fulltext Permission: open
Fulltext Availability: With Fulltext
Appears in Collections:MAE Journal Articles

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