Aerosol mass loading over the marine environment of Arabian Sea during ICARB: Sea-salt and non-sea-salt components

被引:0
作者
Susan K. George
Prabha R. Nair
机构
[1] Vikram Sarabhai Space Centre,Space Physics Laboratory
来源
Journal of Earth System Science | 2008年 / 117卷
关键词
Atmospheric sciences; aerosols; climate; geochemistry; chemical composition of aerosols; sea-salt and non-sea-salt aerosols;
D O I
暂无
中图分类号
学科分类号
摘要
Mass loading and chemical composition of atmospheric aerosols over the Arabian Sea during the pre-monsoon months of April and May have been studied as a part of the Integrated Campaign for Aerosols, gases and Radiation Budget (ICARB). These investigations show large spatial variabilities in total aerosol mass loading as well as that of individual chemical species. The mass loading is found to vary between 3.5 and 69.2 μg m−3, with higher loadings near the eastern and northern parts of Arabian Sea, which decreases steadily to reach its minimum value in the mid Arabian Sea. The decrease in mass loading from the coast of India towards west is estimated to have a linear gradient of 1.53 μg m−3/° longitude and an e−1 scale distance of ∼2300 km. SO42−, Cl− and Na+ are found to be the major ionic species present. Apart from these, other dominating watersoluble components of aerosols are NO3− (17%) and Ca2+ (6%). Over the marine environment of Arabian Sea, the non-sea-salt component dominates accounting to ∼76% of the total aerosol mass. The spatial variations of the various ions are examined in the light of prevailing meteorological conditions and airmass back trajectories.
引用
收藏
页码:333 / 344
页数:11
相关论文
共 177 条
[1]  
Andreae M. O.(2000)Soluble ion chemistry of the atmospheric aerosol and SO2 concentrations over the eastern North Atlantic during ACE-2 Tellus 52B 1066-1087
[2]  
Elbert W.(1996)Relationship among aerosol constituents from Asia and the North Pacific during PEM-West A J. Geophys. Res. 101 2011-2023
[3]  
Gabriel R.(2003)Bulk and size-segregated aerosol composition observed during INDOEX 1999: Overview of meteorology and continental impacts J. Geophys. Res. 108 8001-16,318
[4]  
Johnson D. W.(1998)International Global Atmospheric Chemistry (IGAC) Project’s First Aerosol Characterization Experiment (ACE 1): Overview J. Geophys. Res. 103 16,297-347
[5]  
Osborne S.(1980)The production, concentration, and vertical distribution of the sea-salt aerosol Ann. N. Y. Acad. Sci. 338 330-6061
[6]  
Wood R.(1997)Aerosol composition at Cheju Island, Korea J. Geophys. Res. 102 6047-661
[7]  
Arimoto R.(1987)Oceanic phytoplankton, atmospheric sulfur, cloud albedo and climate Nature 326 655-430
[8]  
Duce R. A.(1992)Climate forcing by anthropogenic aerosols Science 255 423-5342
[9]  
Savoie D. L.(1983)Atmospheric trace elements at Enewetak Atoll 1. concentrations, sources and temporal variability J. Geophys. Res. 88 5321-837
[10]  
Prospero J. M.(1985)The production and dispersal of marine aerosol Q. J. R. Meteorol. Soc. 111 817-39