Abstract

Abstract. Recent years have seen the increasing inclusion of per-retrieval prognostic (predictive) uncertainty estimates within satellite aerosol optical depth (AOD) data sets, providing users with quantitative tools to assist in the optimal use of these data. Prognostic estimates contrast with diagnostic (i.e. relative to some external truth) ones, which are typically obtained using sensitivity and/or validation analyses. Up to now, however, the quality of these uncertainty estimates has not been routinely assessed. This study presents a review of existing prognostic and diagnostic approaches for quantifying uncertainty in satellite AOD retrievals, and it presents a general framework to evaluate them based on the expected statistical properties of ensembles of estimated uncertainties and actual retrieval errors. It is hoped that this framework will be adopted as a complement to existing AOD validation exercises; it is not restricted to AOD and can in principle be applied to other quantities for which a reference validation data set is available. This framework is then applied to assess the uncertainties provided by several satellite data sets (seven over land, five over water), which draw on methods from the empirical to sensitivity analyses to formal error propagation, at 12 Aerosol Robotic Network (AERONET) sites. The AERONET sites are divided into those for which it is expected that the techniques will perform well and those for which some complexity about the site may provide a more severe test. Overall, all techniques show some skill in that larger estimated uncertainties are generally associated with larger observed errors, although they are sometimes poorly calibrated (i.e. too small or too large in magnitude). No technique uniformly performs best. For powerful formal uncertainty propagation approaches such as optimal estimation, the results illustrate some of the difficulties in appropriate population of the covariance matrices required by the technique. When the data sets are confronted by a situation strongly counter to the retrieval forward model (e.g. potentially mixed land–water surfaces or aerosol optical properties outside the family of assumptions), some algorithms fail to provide a retrieval, while others do but with a quantitatively unreliable uncertainty estimate. The discussion suggests paths forward for the refinement of these techniques.

Highlights

  • The capability to quantify atmospheric aerosols from spaceborne measurements arguably goes back to 1972 with the launch of the Multispectral Scanner System (MSS) aboard the first Landsat satellite

  • Earlier satellite-based solar reflectance measurements were either panchromatic or broadband. While it was realized from experience with similar sensors on Mars (Hanel et al, 1972) that some aerosols could contribute to signals in the thermal infrared, they were largely treated as a contaminant in temperature and water vapour retrievals and not routinely quantified (Weaver et al, 2003)

  • The cloud-masking approach is described by Frey et al (2008), with more recent updates listed in Sect. 3 of Baum et al (2012)

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Summary

Introduction

Panel (b) shows two distributions: in black is the distribution of the expected AOD uncertainty magnitude (often, as discussed before, called expected error or EE), assuming error characteristics of the MODIS DT land retrieval, S = ±(0.05+0.15τ ) (Levy et al, 2013). |τS − τA|), which would be expected to be seen in a validation exercise against AERONET if the expression for S holds true

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