Abstract

Abstract. The Advanced Baseline Imager (ABI) on board the Geostationary Operational Environmental Satellite-R (GOES-R) series enables retrieval of aerosol optical depth (AOD) from geostationary satellites using a multiband algorithm similar to those of polar-orbiting satellites' sensors, such as the Moderate Resolution Imaging Spectroradiometer (MODIS) and Visible Infrared Imaging Radiometer Suite (VIIRS). However, this work demonstrates that the current version of GOES-16 (GOES-East) ABI AOD has diurnally varying biases due to limitations in the land surface reflectance relationships between the 0.47 µm band and the 2.2 µm band and between the 0.64 µm band and 2.2 µm band used in the ABI AOD retrieval algorithm, which vary with the Sun–satellite geometry and NDVI (normalized difference vegetation index). To reduce these biases, an empirical bias correction algorithm has been developed based on the lowest observed ABI AOD of an adjacent 30 d period and the background AOD at each time step and at each pixel. The bias correction algorithm improves the performance of ABI AOD compared to AErosol RObotic NETwork (AERONET) AOD, especially for the high and medium (top 2) quality ABI AOD. AOD data for the period 6 August to 31 December 2018 are used to evaluate the bias correction algorithm. After bias correction, the correlation between the top 2 quality ABI AOD and AERONET AOD improves from 0.87 to 0.91, the mean bias improves from 0.04 to 0.00, and root-mean-square error (RMSE) improves from 0.09 to 0.05. These results for the bias-corrected top 2 qualities ABI AOD are comparable to those of the corrected high-quality ABI AOD. By using the top 2 qualities of ABI AOD in conjunction with the bias correction algorithm, the areal coverage of ABI AOD is increased by about 100 % without loss of data accuracy.

Highlights

  • Aerosols in the atmosphere such as dust, smoke, pollutants, volcanic ash, and sea spray can affect climate through scattering and absorption of radiation directly and through interaction with clouds indirectly (Albrecht, 1989; Rosenfeld and Lensky, 1998; Mahowald, 2011)

  • The problem may be caused by the errors in radiative transfer code that do not fully account for the curvature of the Earth. They claim that they did not find any systematic artifact over land, such an artifact is expected because it exists in dark target (DT) Advanced Baseline Imager (ABI) aerosol optical depth (AOD) over continental United States (CONUS), as shown in Fig. 16 at Tucson and City College of New York (CCNY)

  • In our validation work of Geostationary Operational Environmental Satellites (GOES)-16 ABI AOD, we noticed a substantial diurnal bias in AOD that needed to be fixed for our operational users

Read more

Summary

Introduction

Aerosols in the atmosphere such as dust, smoke, pollutants, volcanic ash, and sea spray can affect climate through scattering and absorption of radiation directly and through interaction with clouds indirectly (Albrecht, 1989; Rosenfeld and Lensky, 1998; Mahowald, 2011). AOD from polar-orbiting satellite sensors, such as the Moderate Resolution Imaging Spectroradiometer (MODIS) and Visible Infrared Imaging Radiometer Suite (VIIRS), is retrieved using multi-channel algorithms (Levy et al, 2007, 2010; Sayer et al, 2014; Jackson et al, 2013; Liu et al, 2014; Laszlo and Liu, 2016). H. Zhang et al.: ABI AOD bias correction algorithm error of 0.11 (Laszlo and Liu, 2016), but the low temporal resolution of polar-orbiting satellites limits the availability of observations for a given location. The Advanced Baseline Imager (ABI) on the new-generation GOES-R series of satellites is expected to provide AOD retrievals with accuracies similar to those from MODIS and VIIRS due to similar instrument design and algorithm science, combined with high temporal resolution. The resultant corrected ABI AOD shows little to no diurnal bias over a variety of surface types (e.g., urban, rural)

GOES-16 ABI AOD
AERONET AOD
GOES-16 ABI AOD diurnal bias
Bias correction algorithm
Application to NOAA ABI AOD data
Application to NASA DT ABI AOD data
Impact on particulate matter estimation
Analysis of surface reflectance and AOD biases
Surface reflectance model bias analysis
Radiative transfer simulation analysis
Findings
Summary and conclusions
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call