Abstract

For reflected sunlight observed from space at visible and near-infrared wavelengths, particles suspended in Earth’s atmosphere provide contrast with vegetation or dark water at the surface. This is the physical motivation for the Dark Target (DT) aerosol retrieval algorithm developed for the Moderate Resolution Imaging Spectrometer (MODIS). To extend the data record of aerosol optical depth (AOD) beyond the expected 20-year lifespan of the MODIS sensors, DT must be adapted for other sensors. A version of the DT AOD retrieval for the Visible Infrared Imaging Radiometer Suite (VIIRS) on the Suomi-National Polar-Orbiting Partnership (SNPP) is now mature enough to be released as a standard data product, and includes some upgraded features from the MODIS version. Differences between MODIS Aqua and VIIRS SNPP lead to some inevitable disagreement between their respective AOD measurements, but the offset between the VIIRS SNPP and MODIS Aqua records is smaller than the offset between those of MODIS Aqua and MODIS Terra. The VIIRS SNPP retrieval shows good agreement with ground-based measurements. For most purposes, DT for VIIRS SNPP is consistent enough and in close enough agreement with MODIS to continue the record of satellite AOD. The reasons for the offset from MODIS Aqua, and its spatial and temporal variability, are investigated in this study.

Highlights

  • Aerosols suspended in the atmosphere exert a direct effect on the global radiative balance and climate system [1] and impact air quality as well as cloud and precipitation processes [2,3,4,5,6]

  • The coverage and spatial resolutions from Moderate Resolution Imaging Spectrometer (MODIS) (Terra and Aqua) are sufficient even if the temporal resolution is not. Advanced retrieval algorithms, such as those used for MODIS, derive aerosol optical depth (AOD) with uncertainty (±(0.03 + 10%) over ocean; ±(0.05 + 20%) over land) which approach the Global Climate Observing System (GCOS) requirements

  • Pixel resolution itself can affect the results of an AOD retrieval

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Summary

Introduction

Aerosols suspended in the atmosphere exert a direct effect on the global radiative balance and climate system [1] and impact air quality as well as cloud and precipitation processes [2,3,4,5,6]. These particles remain airborne for periods of days to weeks, vary greatly over regional scales, and do not mix uniformly through the atmosphere [7]. One major requirement remains: in order to qualify as a CDR, the AOD measurements must be maintained for at least three decades

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