International Journal of Remote Sensing · 2014 · 25 citations · 56 references
Natural SciencesEarth SciencesAtmospheric RadiationAtmospheric ScienceClimatologyAerosol PhysicsAerosol Radiative EffectsAerosol Remote SensingAerosol ScienceAtmospheric Sounding From SatellitesParticulate MatterAerosol Direct Radiative EffectAerosol Forcing EfficiencyAerosol Optical Depth RetrievalAerosol Optical PropertiesAerosol Vertical DistributionDepolarization RatioOptical DepthTop-of-atmosphere Radiative Flux
Multi-sensor aerosol data sets are analysed to examine the aerosol characteristics over the Delhi national capital region. Both the Multiple-angle Imaging Spectroradiometer (MISR) and Moderate Resolution Imaging Spectroradiometer (MODIS) capture the seasonal cycle of aerosol optical depth (AOD) as observed by ground-based measurements. However, AOD from MISR shows a low bias relative to AOD from MODIS, which increases linearly at high AOD conditions. A large difference (by >25 W m–2 per unit AOD) in the top-of-atmosphere direct radiative forcing efficiency derived from MODIS and MISR-retrieved AOD is observed during the winter and pre-monsoon seasons relative to the other seasons. The ubiquitous presence of dust (as indicated by non-spherical particle fraction to AOD and linear depolarization ratio values) is observed throughout the year. The aerosol layer is mostly confined to within 2 km of surface in the winter and post-monsoon seasons, while it expands beyond 6 km in the pre-monsoon and monsoon seasons. Columnar AOD is found to be highly sensitive to aerosol vertical distribution. The applicability of multi-sensor data sets and climatic implications are discussed.
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