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Atmospheric Measurement Techniques An interactive open-access journal of the European Geosciences Union
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Short summary
The Atmospheric Infrared Sounder (AIRS) and the Moderate Resolution Imaging Spectroradiometer (MODIS) are instruments on the 1.30 pm polar orbiting Aqua spacecraft. We describe a daytime estimation of dust and volcanic ash layer heights, using a retrieval algorithm that uses the information in the AIRS L1B thermal infrared data, constrained by the MODIS L2 aerosol optical depths. CALIOP aerosol centroid heights are used for dust height comparisons, as are AATSR volcanic plume heights.
Preprints
https://doi.org/10.5194/amtd-8-443-2015
https://doi.org/10.5194/amtd-8-443-2015

  13 Jan 2015

13 Jan 2015

Review status: this preprint was under review for the journal AMT but the revision was not accepted.

A novel retrieval of daytime atmospheric dust and volcanic ash heights through a synergy of AIRS infrared radiances and MODIS L2 optical depths

S. DeSouza-Machado1, L. Strow1, E. Maddy2, O. Torres3, G. Thomas4,*, D. Grainger4, and A. Robinson5 S. DeSouza-Machado et al.
  • 1Joint Center for Earth Systems Technology/Physics Department, University of Maryland, Baltimore County, Baltimore, MD, USA
  • 2Riverside Technology, Inc, College Park, MD, USA
  • 3NASA Goddard, Greenbelt, MD, USA
  • 4Atmospheric, Oceanic and Planetary Physics, University of Oxford, Oxford, UK
  • 5Radiation Oncology and Molecular Radiation Sciences, Johns Hopkins Hospital, Baltimore, MD, USA
  • *now at: Rutherford Appleton Laboratory Space, STFC Rutherford Appleton Laboratory, Harwell Science and Innovation Campus, Oxford, UK

Abstract. We present a novel method to retrieve daytime atmospheric dust and ash plume heights using a synergy of infrared hyper-spectral radiances and retrieved visible optical depths. The method is developed using data from the Atmospheric Infrared Sounder (AIRS) and Moderate Resolution Imaging Spectroradiometer (MODIS), both of which are on NASA's Aqua platform, and lends itself to also a χ2 height derivation based on the smallest bias between observations and calculations in the thermal infrared window. The retrieval methodology is validated against almost 30 months of dust centroid heights obtained from the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIOP) data, and against ash plume heights obtained from the Advanced Along-Track Scanning Radiometer (AATSR) after the Puyehue Cordon Caulle volcanic eruption of June 2011. Comparisons are also made against Goddard Chemistry Aerosol Radiation and Transport (GOCART) climatological aerosol heights. In general there is good agreement between the heights from the CALIPSO data and the AIRS/MODIS retrieval, especially over the Atlantic and Mediterranean regions; over land one there are more noticeable differences. The AIRS/MODIS derived heights are within typically 25% of the CALIOP centroid heights.

S. DeSouza-Machado et al.

 
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Status: closed
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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

S. DeSouza-Machado et al.

S. DeSouza-Machado et al.

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Short summary
The Atmospheric Infrared Sounder (AIRS) and the Moderate Resolution Imaging Spectroradiometer (MODIS) are instruments on the 1.30 pm polar orbiting Aqua spacecraft. We describe a daytime estimation of dust and volcanic ash layer heights, using a retrieval algorithm that uses the information in the AIRS L1B thermal infrared data, constrained by the MODIS L2 aerosol optical depths. CALIOP aerosol centroid heights are used for dust height comparisons, as are AATSR volcanic plume heights.
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