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. Author manuscript; available in PMC: 2011 Dec 7.
Published in final edited form as: Int J Remote Sens. 2008 Jun;29(12):3383–3405. doi: 10.1080/01431160701474545

Figure 3.

Figure 3

Collocating 5 km AOD and point level PM data: AOD and PM estimates on 1 October 2003. AOD (τa) = ln(Io/I) where lo = intensity of radiation from the earth surface, ls = intensity of radiation reaching the sensor, τa = optical depth in the presence of aerosols.