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Bibliografías temáticas / Sea spray generation

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Artículos de revistas

Literatura académica sobre el tema "Sea spray generation"

Autor: Grafiati

Publicado: 25 de mayo de 2024

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Artículos de revistas sobre el tema "Sea spray generation"

1

Smith, M. H., and N. M. Harrison. "The sea spray generation function." Journal of Aerosol Science 29 (September 1998): S189—S190. http://dx.doi.org/10.1016/s0021-8502(98)00280-8.

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2

Andreas, Edgar L. "Sea Spray Generation at a Rocky Shoreline." Journal of Applied Meteorology and Climatology 55, no. 9 (2016): 2037–52. http://dx.doi.org/10.1175/jamc-d-15-0211.1.

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AbstractWith sea ice in the Arctic continuing to shrink, the Arctic Ocean and the surrounding marginal seas will become more like the ocean at lower latitudes. In particular, with more open water, air–sea exchange will be more intense and storms will be stronger and more frequent. The longer fetches over open water and the more energetic storms will combine to produce higher waves and more sea spray. Offshore structures—such as oil drilling, exploration, and production platforms—will face increased hazards from freezing sea spray. On the basis of sea spray observations made with a cloud-imagin

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3

Ortiz-Suslow, David G., Brian K. Haus, Sanchit Mehta, and Nathan J. M. Laxague. "Sea Spray Generation in Very High Winds." Journal of the Atmospheric Sciences 73, no. 10 (2016): 3975–95. http://dx.doi.org/10.1175/jas-d-15-0249.1.

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Abstract Quantifying the amount and rate of sea spray production at the ocean surface is critical to understanding the effect spray has on atmospheric boundary layer processes (e.g., tropical cyclones). Currently, only limited observational data exist that can be used to validate available droplet production models. To help fill this gap, a laboratory experiment was conducted that directly observed the vertical distribution of spume droplets above actively breaking waves. The experiments were carried out in hurricane-force conditions (10-m equivalent wind speed of 36–54 m s−1), and the observe

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4

Mueller, James A., and Fabrice Veron. "A Sea State–Dependent Spume Generation Function." Journal of Physical Oceanography 39, no. 9 (2009): 2363–72. http://dx.doi.org/10.1175/2009jpo4113.1.

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Abstract The uncertainty of the sea spray generation function continues to obscure spray-mediated momentum and scalar fluxes, especially for intense wind conditions. Most previous studies assume a constant form (spectral shape) for the droplet distribution, even though a shift to smaller drops with increased wind forcing is expected. In this paper, a new generation function for spume drops is derived, but unlike previous studies, both its form and magnitude change with wind forcing. Fairly good agreement is found between this spume generation function and the limited data available. A potentia

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5

Mueller, James A., and Fabrice Veron. "Impact of Sea Spray on Air–Sea Fluxes. Part II: Feedback Effects." Journal of Physical Oceanography 44, no. 11 (2014): 2835–53. http://dx.doi.org/10.1175/jpo-d-13-0246.1.

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Abstract This paper presents estimations for the transfer of momentum, heat, and water mass between the air and the sea. The results from Lagrangian stochastic simulations of sea spray drops (see Part I), along with two sea spray generation functions, are used to calculate the spray-mediated flux components of the air–sea fluxes. When the spray-mediated fluxes constitute a significant fraction of the total fluxes under certain conditions, their feedback effect on the atmosphere cannot be neglected. The authors derive a simplified feedback model to investigate such cases, finding that the spray

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6

Garg, Nikhil, Eddie Yin Kwee Ng, and Srikanth Narasimalu. "The effects of sea spray and atmosphere–wave coupling on air–sea exchange during a tropical cyclone." Atmospheric Chemistry and Physics 18, no. 8 (2018): 6001–21. http://dx.doi.org/10.5194/acp-18-6001-2018.

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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 c

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7

Wan, Zhanhong, Luping Li, Zhigen Wu, Jiawang Chen, and Xiuyang Lü. "The impact of ocean waves on spray stress and surface drag coefficient." International Journal of Numerical Methods for Heat & Fluid Flow 29, no. 2 (2019): 523–35. http://dx.doi.org/10.1108/hff-05-2018-0237.

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Purpose The behaviors of sea surface drag coefficient should be well understood for an accurate hurricane prediction. The speed of wind has been applied to characterize the spray production; however, this could result in inaccurate spray productions compared to the experimental or field data if the influence of wave state is not considered. This paper aims to integrate a new sea spray generation function, described by windsea Reynolds number, into the spray momentum flux formula to calculate the spray momentum. Design/methodology/approach On the basis of this spray momentum, this study propose

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8

Bao, J. W., C. W. Fairall, S. A. Michelson, and L. Bianco. "Parameterizations of Sea-Spray Impact on the Air–Sea Momentum and Heat Fluxes." Monthly Weather Review 139, no. 12 (2011): 3781–97. http://dx.doi.org/10.1175/mwr-d-11-00007.1.

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Abstract This paper focuses on parameterizing the effect of sea spray at hurricane-strength winds on the momentum and heat fluxes in weather prediction models using the Monin–Obukhov similarity theory (a common framework for the parameterizations of air–sea fluxes). In this scheme, the mass-density effect of sea spray is considered as an additional modification to the stratification of the near-surface profiles of wind, temperature, and moisture in the marine surface boundary layer (MSBL). The overall impact of sea-spray droplets on the mean profiles of wind, temperature, and moisture depends

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9

Piazzola, J., P. Forget, and S. Despiau. "A sea spray generation function for fetch-limited conditions." Annales Geophysicae 20, no. 1 (2002): 121–31. http://dx.doi.org/10.5194/angeo-20-121-2002.

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Abstract. This paper presents a sea spray generation function for aerosols produced by bubbles bursting that accounts for the effects of fetch. This is achieved by introducing a fetch-dependent model for the whitecap fraction, which is valid for fetch-limited conditions, i.e. steady-state conditions of the wave field in the whitecap droplet flux derived by Monahan et al. (1986). The aerosol generation fluxes calculated by this method show an enhancement of the aerosol production with increasing fetch. However, the predicted generation fluxes are lower than those calculated by using the classic

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10

Zhang, Ting. "The Impact of Surface Waves and Spray Injection Velocities on Air–Sea Momentum and Heat Fluxes." Atmosphere 14, no. 10 (2023): 1500. http://dx.doi.org/10.3390/atmos14101500.

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Surface waves and sea spray play a significant role in air–sea fluxes in high winds. The present study used a marine atmosphere surface layer (MASL), which couples the traditional Monin–Obukhov similarity theory, sea spray generation function, the balance of turbulent kinetic budget, and momentum/enthalpy conservation equations. Based on this model, the effects of wave states and spray injection velocities on air–sea momentum/enthalpy fluxes and near-surface wind/temperature profiles were theoretically investigated. Based on the assumption that the velocity of injected spray is the same as tha

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