[1]Zakey A S, Giorgi F, Bi X. Modeling of sea salt in a regional climate model: Fluxes and radiative[J]. J Geophys Res, 2008, 113, D14221, doi:10.1029/2007JD009209.
[2]Roth B, Okada K. On the modification of sea-salt particles in the coastal atmosphere[J]. Atmos Environ, 1998, 32: 1555-1569.
[3]Weis D D, Ewing G E. The reaction of nitrogen dioxide with sea salt aerosol[J]. J Phys Chem A, 1999, 103: 4865-4873.
[4]Blanchard D C, Woodcock A H. Bubble formation and modification in the sea and its meteorological significance[J]. Tellus, 1957, 9: 145-158.
[5]Seinfeld J H, Pandis S N. Atmospheric Chemistry and Physics, From Air Pollution to Climate Change[M]. New York: John Wiley and Sons, 1998: 1326.
[6]Tegen I N, Hollrig P, Chin M, et al. Contribution of different aerosol species to the global aerosol extinction optical thickness: Estimates from model results[J]. J Geophys Res, 1997, 102(D20), 23,895-23,915, doi:10.1029/97JD01864.
[7]罗燕, 吴涧, 王卫国. 利用MODIS2GOCART 气溶胶资料研究中国东部地区气溶胶直接辐射强迫[J]. 热带气象学报, 2006, 22(6): 638- 649.
[8]Sievering H, Cainey J, Harvey M, et al. Aerosol non-sea-salt sulfate in the remote marine boundary layer under clear-sky and normal cloudiness conditions: Ocean-derived biogenic alkalinity enhances sea-salt sulfate production by ozone oxidation[J]. J Geophys Res, 2004, 109, D19317, doi:10.1029/2003JD004315.
[9]Foltescu V L, Pryor S C, Bennet C. Sea salt generation, dispersion and removal on the regional scale[J]. Atmos Environ, 2005, 39(11): 2123-2133.
[10]Zhang K M, Eladio M K, Anthony S, et al. Size distribution of sea-salt emissions as a function of relative humidity[J]. Atmos Environ, 2005, 39(18): 3373-3379.
[11]Clarke A D, Owens S R, Zhou J. An ultrafine sea-salt flux from breaking waves: implications for cloud condensation nuclei in the remote marine atmosphere[J]. J Geophys Res, 2006, 111, D06202. doi:10.1029/ 2005JD006565.
[12]刘倩. 中国地区海盐气溶胶模拟及其对硫氮循环的影响研究[D]. 南京: 南京大学, 2008: 1-72.
[13]Steven D, Li Jiangnan, Richard H, et al. Sea-salt optical properties and GCM forcing at solar wavelengths[J]. Atmos Res, 2003, 65(3-4): 211-233.
[14]Pryor S C, Sorensen L L. Nitric acid-sea salt reactions: implications for nitrogen deposition to water surfaces[J]. J Appl Meteor, 2000, 39(5): 725-731.
[15]Ma X, Salzen K, Li J. Modelling sea salt aerosol and its direct and indirect effects on climate[J]. Atoms Chem Phys Discuss.2007, 7: 14939-14987.
[16]Elguindi N, Bi X, Giorgi F, et al. RegCM Version 3.0 User's Guide[Z]. http://users.ictp.it/RegCNET/model.html, 2007.
[17]王体健, 谢旻, 高丽洁, 等. 一个区域气候-化学耦合模式的研制及初步应用[J]. 南京大学学报: 自然科学版, 2004, 6: 711-727.
[18]Giorgi F, Bi X, Qian Y. Direct radiative forcing and regional climatic effects of anthropogenic aerosols over East Asia: A regional coupled climate-chemistry/aerosol model study[J]. J Geophys Res, 2002, 107(D20), 4439, doi:10.1029/2001JD001066.
[19]Qian Y, Leung L R, Ghan S J, et al. Regional climate effects of aerosols over China: Modeling and observation[J]. Tellus, 55B: 914-934.
[20]Pal J S, Giorgi F, Bi X. Consistency of recent European summer precipitation trends and extremes with future regional climate projectins[J]. Geophys Res Lett, 2004, 31, L13202, doi:10.1029/2004GL019, 836.
[21]Giorgi F, Bi X, Pal J S. Mean, interannual variability and trends in a regional climate experiment over Europe. II: Future climate (2070-2100)[J]. Climate Dyn, 23(7-8): 839-858.
[22]Gao X J, Pal J S, Giorgi F. Projected changes in mean and extreme precipitation over the Mediterranean region from a high resolution double nested RCM simulation[J]. J Geophys Res, 2006, 33, L03706, doi: 10.1029/2005GL024, 954.
[23]Li S, Wang T J, Zhuang B L, et al. Indirect radiative forcing and climatic effect of the anthropogenic nitrate aerosol on regional climate of China[J]. Adv Atmos Sci, 2009, 26(3): 543-552, doi: 10.1007/s00376-009-0543-9.
[24]庄炳亮, 王体健, 和李树. 中国地区黑碳气溶胶的第一间接辐射强迫与气候效应[J]. 高原气象, 2009, 28(5): 1095-1103.
[25]Wang T, Li S, Shen Y, et al. Investigations on direct and indirect effect of nitrate on temperature and precipitation in China using a regional climate chemistry modeling system[J]. J Geophys Res, 2010, 115, D00K26, doi: 10.1029/2009JD013264.
[26]Zhuang B L, Jiang F, Wang T J, et al. Investigation on the direct radiative effect of fossil fuel black-carbon aerosol over China[J]. Theor Appl Climatol, 2010, doi: 10.1007/s00704-010-0341-4.
[27]Zhuang B L, Liu L, Shen F H, et al. Semidirect radiative forcing of internal mixed black carbon cloud droplet and its regional climatic effect over China[J]. J Geophys Res, 2010, 115, D00K19, doi: 10.1029/2009JD013165.
[28]Erickson D J, Merrill J T, Duce R A. Seasonal Estimates of Global Atmospheric Sea-salt Distributions[J]. J Geophys Res, 1986, 91(D1): 1067-1072.
[29]李霞, 任宜勇, 吴彦, 等. 乌鲁木齐污染物浓度和大气气溶胶光学厚度的关系[J]. 高原气象, 2007, 26(3): 541-546.
[30]Murphy D M, Anderson J R, Quinn P K, et al. Influence of sea-salt on aerosol radiative properties in the Southern Ocean marine boundary layer[J]. Nature, 1998, 392: 62-65.
[31]郝丽, 杨文, 石广玉, 等. 黑碳硫酸盐混合气溶胶的辐射特性分析[J]. 高原气象, 2010, 29(5): 1238-1245.