Sea-salt aerosol source functions and emissions

作者: Michael Schulz , Gerrit de Leeuw , Yves Balkanski

DOI: 10.1007/978-1-4020-2167-1_9

关键词: Cloud condensation nucleiSea sprayAtmospheric sciencesRadiative forcingMass concentration (chemistry)ParticulatesAerosolEnvironmental scienceForcing (mathematics)Sea salt aerosol

摘要: Sea spray aerosols are important for a wide variety of processes. Part the current interest is their role in climate (Penner et al., 2001). aerosol contributes to atmospheric cooling because they scatter incoming solar radiation. It natural component system and therefore can not be regarded as forcing component. However, it often neglected global models may responsible feedback effects. Latham Smith (1990) suggested that changing would alter surface winds thus sea emissions. Although number concentrations very high compared those anthropogenic such ammonium sulphates, significant oceans cover 70% Earth, whereas rather locally produced. Sea-salt dominant submicrometer scatterer most ocean regions dominates marine boundary layer particulate mass concentration remote oceanic regions, with fraction occurring size range (IPCC., 44% optical depth. Estimates top-of-atmosphere, global-annual radiative due sea-salt -1.51 -5.03 Wm2 low emission values, respectively only affects by scattering radiation, also acts cloud condensation nuclei indirect effect (IAE).

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