Giant Sea-Salt Aerosols and Warm Rain Formation in Marine Stratocumulus Export

@article{jensen2008, abstract = {The concentrations and sizes of smaller aerosols (radius smaller than 0.5 \&\#956;m) in the marine atmosphere vary owing to natural and anthropogenic factors. The concentrations and sizes of giant and ultragiant aerosols vary primarily due to wind-speed-dependent wave breaking. In climate models the formation of warm rain from marine stratocumulus clouds is usually parameterized based on the drops that form on the smaller aerosols. The present process study, using a stochastic Monte Carlo cloud model, shows that the variability of giant sea-salt aerosols and the variability of smaller aerosol cloud condensation nuclei are equally important in determining precipitation flux in marine stratocumulus. This strongly suggests that the effects of giant sea-salt aerosols should be included in the parameterization of warm rain formation in climate and other large-scale models.The above results are based on highly detailed calculations of droplet growth in an idealized marine stratocumulus cloud; the authors believe that other marine stratus cloud conditions may change the calculated rain rates but that the conclusions regarding the relative importance of small and giant aerosols are robust.}, author = {Jensen, J\&\#248;rgen B. and Lee, Sunhee}, citeulike-article-id = {4135569}, citeulike-linkout-0 = {http://dx.doi.org/10.1175/2008JAS2617.1}, day = {1}, doi = {10.1175/2008JAS2617.1}, journal = {Journal of the Atmospheric Sciences}, keywords = {giant, rain, sea-salt, stratocumulus, warm}, month = {December}, number = {12}, pages = {3678--3694}, posted-at = {2009-03-05 13:08:54}, priority = {2}, title = {Giant Sea-Salt Aerosols and Warm Rain Formation in Marine Stratocumulus}, url = {http://dx.doi.org/10.1175/2008JAS2617.1}, volume = {65}, year = {2008} }

TY - JOUR ID - jensen2008 L3 - citeulike-article-id:4135569 N2 - The concentrations and sizes of smaller aerosols (radius smaller than 0.5 μm) in the marine atmosphere vary owing to natural and anthropogenic factors. The concentrations and sizes of giant and ultragiant aerosols vary primarily due to wind-speed-dependent wave breaking. In climate models the formation of warm rain from marine stratocumulus clouds is usually parameterized based on the drops that form on the smaller aerosols. The present process study, using a stochastic Monte Carlo cloud model, shows that the variability of giant sea-salt aerosols and the variability of smaller aerosol cloud condensation nuclei are equally important in determining precipitation flux in marine stratocumulus. This strongly suggests that the effects of giant sea-salt aerosols should be included in the parameterization of warm rain formation in climate and other large-scale models.The above results are based on highly detailed calculations of droplet growth in an idealized marine stratocumulus cloud; the authors believe that other marine stratus cloud conditions may change the calculated rain rates but that the conclusions regarding the relative importance of small and giant aerosols are robust. IS - 12 JF - Journal of the Atmospheric Sciences EP - 3694 TI - Giant Sea-Salt Aerosols and Warm Rain Formation in Marine Stratocumulus VL - 65 SP - 3678 KW - giant KW - rain KW - sea-salt KW - stratocumulus KW - warm AU - Jensen, Jørgen AU - Lee, Sunhee PY - 2008/12/01/ UR - http://dx.doi.org/10.1175/2008JAS2617.1 ER -