Comparison of MODIS and AERONET derived aerosol optical depth over the Ganga Basin, India

Abstract. The Moderate Resolution Imaging Spectroradiometer (MODIS) onboard EOS Terra measures global aerosol optical depth and optical properties since 2000. MODIS aerosol products are freely available and are being used for numerous studies. In this paper, we present a comparison of aerosol optical depth (AOD) retrieved from MODIS with Aerosol Robotic Network (AERONET) data for the year 2004 over Kanpur, an industrial city lying in the Ganga Basin in the northern part of India. AOD retrieved from MODIS (τaMODIS) at 0.55µm wavelength has been compared with the AERONET derived AOD (τaAERONET), within an optimum space-time window. Although the correlation between τaMODIS and τaAERONET during the post-monsoon and winter seasons (R2~0.71) is almost equal to that during the pre-monsoon and monsoon seasons (R2~0.72), MODIS is found to overestimate AOD during the pre-monsoon and monsoon period (characterized by severe dust loading) and underestimate during the post-monsoon and winter seasons. The absolute difference between τaMODIS and τaAERONET is found to be low (0.12±0.11) during the non-dust loading season and much higher (0.4±0.2) during dust-loading seasons. The absolute error in τaMODIS is found to be about ~25% of the absolute values of τaMODIS. Our comparison shows the importance of modifying the existing MODIS algorithm during the dust-loading seasons, especially in the Ganga Basin in northern part of India.

[1]  B. Holben,et al.  Validation of MODIS aerosol optical depth retrieval over land , 2002 .

[2]  Lorraine Remer,et al.  The MODIS 2.1-μm channel-correlation with visible reflectance for use in remote sensing of aerosol , 1997, IEEE Trans. Geosci. Remote. Sens..

[3]  Alexander Smirnov,et al.  Cloud-Screening and Quality Control Algorithms for the AERONET Database , 2000 .

[4]  B. Holben,et al.  MODIS observation of aerosols and estimation of aerosol radiative forcing over southern Africa during SAFARI 2000 , 2003 .

[5]  P. Bhartia,et al.  Global distribution of UV-absorbing aerosols from Nimbus 7/TOMS data , 1997 .

[6]  Didier Tanré,et al.  Estimate of the aerosol properties over the ocean with POLDER , 2000 .

[7]  D. Tanré,et al.  Remote Sensing of Tropospheric Aerosols from Space: Past, Present, and Future. , 1999 .

[8]  Yoram J. Kaufman,et al.  Size distribution and scattering phase function of aerosol particles retrieved from sky brightness measurements , 1994 .

[9]  T. Eck,et al.  Effect of dry‐season biomass burning on Amazon basin aerosol concentrations and optical properties, 1992–1994 , 1996 .

[10]  Kaushik K. Shandilya,et al.  Investigations into formation of atmospheric sulfate under high PM10 concentration , 2003 .

[11]  A. Smirnov,et al.  AERONET-a federated instrument network and data archive for aerosol Characterization , 1998 .

[12]  B. Holben,et al.  Validation of MODIS aerosol retrieval over ocean , 2002 .

[13]  B. Holben,et al.  Remote sensing of smoke from MODIS airborne simulator during the SCAR‐B experiment , 1998 .

[14]  J. Hansen,et al.  Radiative forcing and climate response , 1997 .

[15]  Brent N. Holben,et al.  Influence of dust storms on the aerosol optical properties over the Indo‐Gangetic basin , 2004 .

[16]  Christine A. O'Neill,et al.  Effects of Aerosol from Biomass Burning on the Global Radiation Budget , 1992, Science.

[17]  D. Tanré,et al.  Remote sensing of aerosol properties over oceans using the MODIS/EOS spectral radiances , 1997 .

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

[19]  E. Vermote,et al.  Operational remote sensing of tropospheric aerosol over land from EOS moderate resolution imaging spectroradiometer , 1997 .

[20]  Y. J. Kaufman,et al.  Measurements Of The Aerosol Optical Thickness And The Path Radiance - Implication On Aerosol Remote Sensing And Atmospheric Corrections , 1990, 10th Annual International Symposium on Geoscience and Remote Sensing.

[21]  Y. Kaufman Aerosol optical thickness and atmospheric path radiance , 1993 .

[22]  O. Boucher,et al.  Estimation of the aerosol perturbation to the Earth's Radiative Budget over oceans using POLDER satellite aerosol retrievals , 2000 .

[23]  Brent N. Holben,et al.  Variability of aerosol parameters over Kanpur, northern India , 2004 .

[24]  Alexander Smirnov,et al.  Development of a Global Validation Package for Satellite Oceanic Aerosol Optical Thickness Retrieval Based on AERONET Observations and Its Application to NOAA/NESDIS Operational Aerosol Retrievals. , 2002 .

[25]  J. Coakley,et al.  Climate Forcing by Anthropogenic Aerosols , 1992, Science.

[26]  P. Bhartia,et al.  Detection of biomass burning smoke from TOMS measurements , 1996 .

[27]  A. Lacis,et al.  The influence on climate forcing of mineral aerosols from disturbed soils , 1996, Nature.

[28]  O. Boucher,et al.  Estimates of the direct and indirect radiative forcing due to tropospheric aerosols: A review , 2000 .

[29]  S. K. Satheesh,et al.  Large differences in tropical aerosol forcing at the top of the atmosphere and Earth's surface , 2000, Nature.

[30]  Yoram J. Kaufman,et al.  Relationship between surface reflectance in the visible and mid‐IR used in MODIS aerosol algorithm ‐ theory , 2002 .

[31]  Yoram J. Kaufman,et al.  Radiative forcing by aerosols over the Bay of Bengal region derived from shipborne, island‐based, and satellite (Moderate‐Resolution Imaging Spectroradiometer) observations , 2004 .

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

[33]  J. Haywood,et al.  On summing the components of radiative forcing of climate change , 2001 .

[34]  B. Holben,et al.  A spatio‐temporal approach for global validation and analysis of MODIS aerosol products , 2002 .

[35]  O. Boucher,et al.  A satellite view of aerosols in the climate system , 2002, Nature.