Validation of MODIS and MISR Based Satellite AOT Data with In- Situ Data for Lahore, Pakistan

Satellite data is important for determination of variations in aerosolsin space and time. The accuracy and validation of satellite data is necessary to evaluate theaccuracy for air quality in a particular region. Satellite derived air pollution measures offer the advantage of providing global coverage. The aerosol optical thickness (AOT) measured from satellite data was validated with the ground based sun photometer AERONETmeasured AOT for Lahore metropolitan city of Pakistan. The satellite based AOT data of MODISand MISR sensors on board TERRA satellite were extracted inradial spatial regions of 25 Km and 44 Km respectively from the AERONET station. The level 2 satellite data and AERONET data products were used for the validation purpose. The green wavelength bands had higher values and good correlation for both MISR and MODIS satellites, having values of coefficient of correlation as 0.86 and 0.84 with RMSE of 0.08 and 0.22 respectively with AERONET mean AOT data measured for 2 hour (± 1hour) time interval centered at satellite pass time.Thus proving the validity of aerosol satellite data as proxy to ground measurements.

[1]  Brent N. Holben,et al.  Seasonal variability of the aerosol parameters over Kanpur, an urban site in Indo-Gangetic basin , 2005 .

[2]  S. Twomey The Influence of Pollution on the Shortwave Albedo of Clouds , 1977 .

[3]  K. Iyer,et al.  Spectral Variation of Total Column Aerosol Optical Depth over Rajkot: A Tropical Semi-arid Indian Station , 2007 .

[4]  J. Seinfeld,et al.  Atmospheric Chemistry and Physics: From Air Pollution to Climate Change , 1997 .

[5]  M. Andreae Chapter 10 – Climatic effects of changing atmospheric aerosol levels , 1995 .

[6]  T. Blaschke,et al.  Monitoring spatio-temporal variations in aerosols and aerosol-cloud interactions over Pakistan using MODIS data , 2010 .

[7]  T. Eck,et al.  Wavelength dependence of the optical depth of biomass burning, urban, and desert dust aerosols , 1999 .

[8]  Toby N. Carlson,et al.  Reflected Radiance Measured by NOAA 3 VHRR as a Function of Optical Depth for Saharan Dust , 1977 .

[9]  L. Chen,et al.  Origins of fine aerosol mass in the Baltimore–Washington corridor: implications from observation, factor analysis, and ensemble air parcel back trajectories , 2002 .

[10]  H. Quenzel,et al.  Relative atmospheric aerosol content from erts observations , 1977 .

[11]  David J. Diner,et al.  Comparison of coincident Multiangle Imaging Spectroradiometer and Moderate Resolution Imaging Spectroradiometer aerosol optical depths over land and ocean scenes containing Aerosol Robotic Network sites , 2005 .

[12]  David A. Santek,et al.  A model for calculating desert aerosol turbidity over the oceans from geostationary satellite data. , 1980 .

[13]  I. Vardavas,et al.  Assessment of the MODIS Collections C005 and C004 aerosol optical depth products over the Mediterranean basin , 2008 .

[14]  Alexander Ignatov,et al.  Development, validation, and potential enhancements to the second‐generation operational aerosol product at the National Environmental Satellite, Data, and Information Service of the National Oceanic and Atmospheric Administration , 1997 .

[15]  Larry L. Stowe,et al.  Characterization of tropospheric aerosols over the oceans with the NOAA advanced very high resolution radiometer optical thickness operational product , 1997 .

[16]  R. S. Fraser Satellite measurement of mass of Sahara dust in the atmosphere. , 1976, Applied optics.

[17]  D. R. Jensen,et al.  The relationship between marine aerosol particles and satellite‐detected radiance , 1986 .

[18]  P. J. Rasch,et al.  Radiative forcing due to sulfate aerosols from simulations with the National Center for Atmospheric Research Community Climate Model, Version 3 , 2000 .

[19]  Y. Kaufman,et al.  Passive remote sensing of tropospheric aerosol and atmospheric , 1997 .

[20]  Thomas Blaschke,et al.  Aerosol size distribution and mass concentration measurements in various cities of Pakistan. , 2011, Journal of environmental monitoring : JEM.

[21]  Itamar M. Lensky,et al.  Satellite-Based Insights into Precipitation Formation Processes in Continental and Maritime Convective Clouds , 1998 .

[22]  M. Griggs,et al.  Satellite Observations of Atmospheric Aerosols During the E0MET Cruise , 1979 .

[23]  Thomas Blaschke,et al.  Aerosol Optical Properties and radiative forcing over mega-city Karachi , 2011 .

[24]  Xin Jiang,et al.  Comparison of MISR aerosol optical thickness with AERONET measurements in Beijing metropolitan area , 2007 .

[25]  Anup K. Prasad,et al.  Aerosol radiative forcing over the Indo-Gangetic plains during major dust storms , 2007 .

[26]  A. Kokhanovsky,et al.  Aerosol remote sensing over land: A comparison of satellite retrievals using different algorithms and instruments , 2007, Atmospheric Research.

[27]  Teruyuki Nakajima,et al.  AVHRR remote sensing of aerosol optical properties in the Persian Gulf region, summer 1991 , 1997 .

[28]  Teruyuki Nakajima,et al.  Development of a Two-Channel Aerosol Retrieval Algorithm on a Global Scale Using NOAA AVHRR , 1999 .