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Atmospheric Measurement Techniques An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 9 | Copyright
Atmos. Meas. Tech., 9, 4167-4179, 2016
https://doi.org/10.5194/amt-9-4167-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 31 Aug 2016

Research article | 31 Aug 2016

Application of oxygen A-band equivalent width to disambiguate downwelling radiances for cloud optical depth measurement

Edward R. Niple1, Herman E. Scott1, John A. Conant1, Stephen H. Jones1, Frank J. Iannarilli1, and Wellesley E. Pereira2 Edward R. Niple et al.
  • 1Aerodyne Research, Inc., Billerica, MA, USA
  • 2Air Force Research Lab, Albuquerque, NM, USA

Abstract. This paper presents the three-waveband spectrally agile technique (TWST) for measuring cloud optical depth (COD). TWST is a portable field-proven sensor and retrieval method offering a unique combination of fast (1Hz) cloud-resolving (0.5° field of view) real-time-reported COD measurements. It entails ground-based measurement of visible and near-infrared (VNIR) zenith spectral radiances much like the Aerosol Robotic Network (AERONET) cloud-mode sensors. What is novel in our approach is that we employ absorption in the oxygen A-band as a means of resolving the COD ambiguity inherent in using up-looking spectral radiances. We describe the TWST sensor and algorithm, and assess their merits by comparison to AERONET cloud-mode measurements collected during the US Department of Energy's Atmospheric Radiation Measurements (ARM) Two-Column Aerosol Project (TCAP). Spectral radiance agreement was better than 1%, while a linear fit of COD yielded a slope of 0.905 (TWST reporting higher COD) and offset of −2.1.

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