Full metadata record
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Reddy, B. S. K. | en_US |
dc.contributor.author | Kumar, K. R. | en_US |
dc.contributor.author | Balakrishnaiah, G. | en_US |
dc.contributor.author | Gopal, K. R. | en_US |
dc.contributor.author | Reddy, R. R. | en_US |
dc.contributor.author | Sivakumar, V. | en_US |
dc.contributor.author | Arafath, S. Md. | en_US |
dc.contributor.author | Lingaswamy, A. P. | en_US |
dc.contributor.author | Pavankumari, S. | en_US |
dc.contributor.author | Umadevi, K. | en_US |
dc.contributor.author | Ahammed, Y. N. | en_US |
dc.date.accessioned | 2014-12-08T15:28:45Z | - |
dc.date.available | 2014-12-08T15:28:45Z | - |
dc.date.issued | 2013-01-01 | en_US |
dc.identifier.issn | 0256-1530 | en_US |
dc.identifier.uri | http://dx.doi.org/10.1007/s00376-012-1234-5 | en_US |
dc.identifier.uri | http://hdl.handle.net/11536/20807 | - |
dc.description.abstract | Surface measurements of aerosol physical properties were made at Anantapur (14.62A degrees N, 77.65A degrees E, 331 m a.s.l), a semiarid rural site in India, during August 2008-July 2009. Measurements included the segregated sizes of aerosolsas as well as total mass concentration and size distributions of aerosols measured at low relative humidity (RH < 75%) using a Quartz Crystal Microbalance (QCM) in the 25-0.05 mu m aerodynamic diameter range. The hourly average total surface aerosol mass concentration in a day varied from 15 to 70 mu g m(-3), with a mean value of 34.02 +/- 9.05 mu g m(-3) for the entire study period. A clear diurnal pattern appeared in coarse, accumulation and nucleation-mode particle concentrations, with two local maxima occurring in early morning and late evening hours. The concentration of coarse-mode particles was high during the summer season, with a maximum concentration of 11.81 +/- 0.98 mu g m(-3) in the month of April, whereas accumulationmode concentration was observed to be high in the winter period contributed > 68% to the total aerosol mass concentration. Accumulation aerosol mass fraction, A (f) (= M (a)/M (t)) was highest during winter (mean value of A (f) 0.80) and lowest (A (f) 0.64) during the monsoon season. The regression analysis shows that both R (eff) and R (m) are dependent on coarse-mode aerosols. The relationship between the simultaneous measurements of daily mean aerosol optical depth at 500 nm (AOD(500)) and PM2.5 mass concentration ([PM2.5]) shows that surface-level aerosol mass concentration increases with the increase in columnar aerosol optical depth over the observation period. | en_US |
dc.language.iso | en_US | en_US |
dc.subject | aerosols mass concentration | en_US |
dc.subject | size distribution | en_US |
dc.subject | effective radius | en_US |
dc.subject | backward trajectories | en_US |
dc.title | Ground-based in situ measurements of near-surface aerosol mass concentration over Anantapur: Heterogeneity in source impacts | en_US |
dc.type | Article | en_US |
dc.identifier.doi | 10.1007/s00376-012-1234-5 | en_US |
dc.identifier.journal | ADVANCES IN ATMOSPHERIC SCIENCES | en_US |
dc.citation.volume | 30 | en_US |
dc.citation.issue | 1 | en_US |
dc.citation.spage | 235 | en_US |
dc.citation.epage | 246 | en_US |
dc.contributor.department | 環境工程研究所 | zh_TW |
dc.contributor.department | Institute of Environmental Engineering | en_US |
dc.identifier.wosnumber | WOS:000312636500021 | - |
dc.citation.woscount | 0 | - |
Appears in Collections: | Articles |
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