2011
DOI: 10.1016/j.atmosenv.2010.12.002
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Analysis of optical properties of atmospheric aerosols inferred from spectral AODs and Ångström wavelength exponent

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Cited by 28 publications
(13 citation statements)
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“…The present study reveals (Fig. 4) a conspicuous evening peak (during 17:00 to 22:00 local time) in the diurnal variations of BC concentrations at the shorter timescales during February-May, and decrease gradually towards morning and become lowest during the early morning hours (05:00), again increases after the sunrise, typical to a continental site subjected to the dynamics of the atmospheric boundary layer (Nair et al, 2007;Balakrishnaiah et al, 2011). The diurnal variations remain inconspicuous from August to February, even though a less pronounced diurnal pattern similar to that in March-May is noticeable during June and October.…”
Section: Temporal Variation Of Bc Mass Concentrationmentioning
confidence: 99%
“…The present study reveals (Fig. 4) a conspicuous evening peak (during 17:00 to 22:00 local time) in the diurnal variations of BC concentrations at the shorter timescales during February-May, and decrease gradually towards morning and become lowest during the early morning hours (05:00), again increases after the sunrise, typical to a continental site subjected to the dynamics of the atmospheric boundary layer (Nair et al, 2007;Balakrishnaiah et al, 2011). The diurnal variations remain inconspicuous from August to February, even though a less pronounced diurnal pattern similar to that in March-May is noticeable during June and October.…”
Section: Temporal Variation Of Bc Mass Concentrationmentioning
confidence: 99%
“…There exists a well-defined seasonal variation in CWC, with the maximum value during the monsoon months and minimum during winter months. Similar variations in CWC have been observed from other locations in India (e.g., Moorthy et al, 1999;Balakrishnaiah et al, 2011).The validation of gridded products (MODIS) is important as they are used for assimilation in numerical weather prediction and global climate models (Prasad et al, 2009). For this purpose, detailed validation of MODIS water vapor product is attempted.…”
Section: Validation Of Modis Aerosol Optical Thicknessmentioning
confidence: 93%
“…The curvature can be an indicator of the aerosol particle size, with negative sign indicating the aerosol size distributions dominated by fine mode and the positive curvature is indicated by the size distributions with significant contribution by coarse mode aerosols (Schuster et al, 2006;Balakrishnaiah et al, 2011). In addition, the coefficients a 1 and a 2 are obtained from the second order polynomial fit to the AOD values at four channels (380, 500, 870 and 936 nm).…”
Section: Site Description Instrumentation and Methodologymentioning
confidence: 99%