Abstract

Satellite remote sensing aerosol monitoring products are readily available but limited to regional and global scales due to low spatial resolutions making them unsuitable for city-level monitoring. Freely available satellite images such as Sentinel -2 at relatively high spatial (10m) and temporal (5 days) resolutions offer the chance to map aerosol distribution at local scales. In the first stage of this study, we retrieve Aerosol Optical Depth (AOD) from Sentinel -2 imagery for the Munich region and assess the accuracy against ground AOD measurements obtained from two Aerosol Robotic Network (AERONET) stations. Sen2Cor, iCOR and MAJA algorithms which retrieve AOD using Look-up-Tables (LUT) pre-calculated using radiative transfer (RT) equations and SARA algorithm that applies RT equations directly to satellite images were used in the study. Sen2Cor, iCOR and MAJA retrieved AOD at 550nm show strong consistency with AERONET measurements with average correlation coefficients of 0.91, 0.89 and 0.73 respectively. However, MAJA algorithm gives better and detailed variations of AOD at 10m spatial resolution which is suitable for identifying varying aerosol conditions over urban environments at a local scale. In the second stage, we performed multiple linear regression to estimate surface Particulate Matter (PM2.5) concentrations using the satellite retrieved AOD and meteorological data as independent variables and ground-measured PM2.5 data as the dependent variable. The predicted PM2.5 concentrations exhibited agreement with ground measurements, with an overall coefficient (R2) of 0.59.

Highlights

  • The study of aerosol concentrations in the atmosphere is essential due to the role they play in Earth's climate

  • The risk is higher in urban regions where an estimated 55% of the World's population live [1] which is as a result of higher anthropogenic aerosols emissions from transport, industries, power plants and household sources

  • In the present paper we extend our work to include Particulate Matter (PM) estimation from satellite retrieved Aerosol Optical D epth (AOD)

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Summary

Introduction

The study of aerosol concentrations in the atmosphere is essential due to the role they play in Earth's climate. Satellite remote sensing has been used to determine the aerosol concentration in the atmosphere based on the inversion of radiative transfer (RT) equations which model the scattering and absorption of solar radiation by aerosols, gas and water molecules in the atmosphere. The retrieval of columnar aerosol optical depth/thickness (AOD/AOT) forms a crucial step in the atmospheric correction of satellite images to generate surface reflectance products. By using the top-of-atmosphere (TOA) reflectance received by the satellite sensors and known surface reflectances/ bottom-of-atmosphere (BOA), the optical thickness of the atmosphere can be determined. The RT equations generate Look-up-Tables (LUT) which model the relationship between TOA reflectances and AOD in the required electromagnetic spectrum range. TOA reflectances follow the RT equation as expressed in Equation 1

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