Do new sea spray aerosol source functions improve the results of a regional aerosol model?

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Date
2018
Volume
198
Issue
Journal
Series Titel
Book Title
Publisher
Amsterdam [u.a.] : Elsevier Science
Abstract

Sea spray aerosol particle is a dominating part of the global aerosol mass load of natural origin. Thus, it strongly influences the atmospheric radiation balance and cloud properties especially over the oceans. Uncertainties of the estimated climate impacts by this aerosol type are partly caused by the uncertainties in the particle size dependent emission fluxes of sea spray aerosol particle. We present simulations with a regional aerosol transport model system in two domains, for three months and compared the model results to measurements at four stations using various sea spray aerosol particle source source functions. Despite these limitations we found the results using different source functions are within the range of most model uncertainties. Especially the model's ability to produce realistic wind speeds is crucial. Furthermore, the model results are more affected by a function correcting the emission flux for the effect of the sea surface temperature than by the use of different source functions. © 2018 The Authors

Description
Keywords
Aerosols, Atmospheric radiation, Atmospheric temperature, Oceanography, Particle size, Submarine geophysics, Surface properties, Surface waters, Uncertainty, analysis, Aerosol modeling, Aerosol transport model, Cloud properties, Marine aerosols, Model uncertainties, Sea spray aerosols, Sea surface temperature (SST), Source functions, Atmospheric movements, aerosol, marine environment, measurement method, modeling, particle size, radiation balance, sea surface, temperature, simulation, uncertainty analysis, aerosol, article, sea surface temperature, simulation, uncertainty, wind speed
Citation
Barthel, S., Tegen, I., & Wolke, R. (2018). Do new sea spray aerosol source functions improve the results of a regional aerosol model? 198. https://doi.org//10.1016/j.atmosenv.2018.10.016
License
CC BY-NC-ND 4.0 Unported