Size segregated aerosol mass concentration measurements over the Arabian Sea during ICARB

被引:20
作者
Nair, Vijayakumar S. [1 ]
Moorthy, K. Krishna [1 ]
Babu, S. Suresh [1 ]
Narasimhulu, K. [2 ]
Reddy, L. Siva Sankara [2 ]
Reddy, R. Ramakrishna [2 ]
Gopal, K. Rama [2 ]
Sreekanth, V. [3 ]
Madhavan, B. L. [3 ]
Niranjan, K. [3 ]
机构
[1] Vikram Sarabhai Space Ctr, Space Phys Lab, Trivandrum 695022, Kerala, India
[2] Sri Krishnadevaraya Univ, Dept Phys, Anantapur 515003, Andhra Pradesh, India
[3] Andhra Univ, Dept Phys, Visakhapatnam 530003, Andhra Pradesh, India
关键词
aerosol mass concentration; Arabian sea; ICARB;
D O I
10.1007/s12040-008-0034-x
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Mass concentration and mass size distribution of total (composite) aerosols near the surface are essential inputs needed in developing aerosol models for radiative forcing estimation as well as to infer the environment and air quality. Using, extensive measurements onboard the oceanographic research vessel, Sagar Kanya, during its cruise SK223B in the second phase of the ocean seg ment of the Integrated Campaign for Aerosols, gases and Radiation Budget (ICARB), the spatial distribution of the mass concentration and mass size distribution of near-surface aerosols are examined for the first time over the entire Arabian Sea, going as far as 58 degrees E and 22 degrees N, within a span of 26 days. In general, the mass concentrations (M-T) were found to be low with the mean value for the entire Arabian Sea being 16.7 +/- 7 mu g m(-3); almost 1/2 of the values reported in some of the earlier campaigns. Coarse mode aerosols contributed, on an average, 58% to the total mass, even though at a few pockets accumulation mode contribution dominated. Spatially, significant variations were observed over central and northern Arabian Sea as well as close to the west coast of India. In central Arabian Sea, even though the M-T was quite low, contribution of accumulation aerosols to the total mass concentration was greater than 50%. Effective radius, a parameter important in determining scattering properties of aerosol size distribution, varied between 0.07 and 0.4 mu m with a mean value of 0.2 mu m. Number size distributions, deduced from the mass size distributions, were approximated to inverse power-law form and the size indices (nu) were estimated. It was found to vary in the range 3.9 to 4.2 with a mean value of 4.0 for the entire oceanic region. Extinction coefficients, estimated using the number-size distributions, were well-correlated with the accumulation mode mass concentration with a correlation coefficient of 0.82.
引用
收藏
页码:315 / 323
页数:9
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