Abstract

Abstract. In order to have a good estimate of the current forcing by anthropogenic aerosols, knowledge on past aerosol levels is needed. Aerosol optical depth (AOD) is a good measure for aerosol loading. However, dedicated measurements of AOD are only available from the 1990s onward. One option to lengthen the AOD time series beyond the 1990s is to retrieve AOD from surface solar radiation (SSR) measurements taken with pyranometers. In this work, we have evaluated several inversion methods designed for this task. We compared a look-up table method based on radiative transfer modelling, a non-linear regression method and four machine learning methods (Gaussian process, neural network, random forest and support vector machine) with AOD observations carried out with a sun photometer at an Aerosol Robotic Network (AERONET) site in Thessaloniki, Greece. Our results show that most of the machine learning methods produce AOD estimates comparable to the look-up table and non-linear regression methods. All of the applied methods produced AOD values that corresponded well to the AERONET observations with the lowest correlation coefficient value being 0.87 for the random forest method. While many of the methods tended to slightly overestimate low AODs and underestimate high AODs, neural network and support vector machine showed overall better correspondence for the whole AOD range. The differences in producing both ends of the AOD range seem to be caused by differences in the aerosol composition. High AODs were in most cases those with high water vapour content which might affect the aerosol single scattering albedo (SSA) through uptake of water into aerosols. Our study indicates that machine learning methods benefit from the fact that they do not constrain the aerosol SSA in the retrieval, whereas the LUT method assumes a constant value for it. This would also mean that machine learning methods could have potential in reproducing AOD from SSR even though SSA would have changed during the observation period.

Highlights

  • The Fifth Assessment Report of the Intergovernmental Panel on Climate Change states that the most significant source of uncertainty in the projections of climate is related to aerosols (IPCC, 2013)

  • One option to lengthen the Aerosol optical depth (AOD) time series beyond the 1990s is to retrieve AOD from surface solar radiation (SSR) measurements taken with pyranometers

  • We compared a look-up table method based on radiative transfer modelling, a non-linear regression method and four machine learning methods (Gaussian process, neural network, random forest and support vector machine) with AOD observations carried out with a sun photometer at an Aerosol Robotic Network (AERONET) site in Thessaloniki, Greece

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Summary

Introduction

The Fifth Assessment Report of the Intergovernmental Panel on Climate Change states that the most significant source of uncertainty in the projections of climate is related to aerosols (IPCC, 2013). One significant contribution to this uncertainty comes from the fact that without the knowledge of the aerosol burden in the past, we are not able to estimate. J. Huttunen et al.: Retrieval of aerosol optical depth from surface solar radiation measurements the current forcing of anthropogenic aerosol. The effect of changes in the current aerosol emissions on climate depends on the background aerosol load during the preindustrial era The current estimates of past aerosol emissions are highly uncertain (Granier et al, 2011), increased knowledge on historical aerosol levels would increase our ability to estimate the present day aerosol radiative forcing

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