Articles | Volume 19, issue 1
https://doi.org/10.5194/amt-19-277-2026
https://doi.org/10.5194/amt-19-277-2026
Research article
 | 
15 Jan 2026
Research article |  | 15 Jan 2026

CALIPSO 1064 nm calibration biases inferred from wavelength-dependent signal attenuation by stratospheric aerosols

Jayanta Kar, Mark A. Vaughan, Robert P. Damadeo, Mahesh Kovilakam, Jason L. Tackett, and Charles R. Trepte

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Cited articles

Cisewski, M., Zawodny, J., Gasbarre, J., Eckman, R., Topiwala, N., Rodriguez-Alvarez, O., Cheek, D., and Hall, S.: The Stratospheric Aerosol and Gas Experiment (SAGE III) on the International Space Station (ISS) Mission, in: Conference on Sensors, Systems, and Next-Generation Satellites XVIII, 22–25 September 2014, Amsterdam, the Netherlands, edited by: Meynart, R., Neeck, S. P., and Shimoda, H., Proceedings of SPIE 9241, SPIE, p. 924107, ISBN 978-1-62841-304-5, https://doi.org/10.1117/12.2073131, 2014. 
Damadeo, R. P., Zawodny, J. M., Thomason, L. W., and Iyer, N.: SAGE version 7.0 algorithm: application to SAGE II, Atmos. Meas. Tech., 6, 3539–3561, https://doi.org/10.5194/amt-6-3539-2013, 2013. 
Damadeo, R. P., Sofieva, V. F., Rozanov, A., and Thomason, L. W.: An empirical characterization of the aerosol Ångström exponent interpolation bias using SAGE III/ISS data, Atmos. Meas. Tech., 17, 3669–3678, https://doi.org/10.5194/amt-17-3669-2024, 2024. 
Duchamp, C., Wrana, F., Legras, B., Sellitto, P., Belhadji, R., and von Savigny, C.: Observation of the Aerosol Plume From the 2022 Hunga Tonga–Hunga Ha'apai Eruption With SAGE III/ISS, Geophys. Res. Lett., 50, e2023GL105076, https://doi.org/10.1029/2023GL105076, 2023. 
Garnier, A., Pelon, J., Vaughan, M. A., Winker, D. M., Trepte, C. R., and Dubuisson, P. : Lidar multiple scattering factors inferred from CALIPSO lidar and IIR retrievals of semi-transparent cirrus cloud optical depths over oceans, Atmos. Meas. Tech., 8, 2759–2774, https://doi.org/10.5194/amt-8-2759-2015, 2015. 
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Short summary
This paper assesses biases in the 1064 nm calibration of the Cloud Aerosol Lidar with Orthogonal Polarization (CALIOP) due to signal attenuation differences at 1064 and 532 nm caused by stratospheric aerosols. Multi-channel measurements from the Stratospheric Aerosol and Gas Experiment suggest the bias ranges from 1 %–2 % for background conditions to over 5 % for high aerosol loads. Implications for CALIOP 1064 nm extinction retrievals and cascading errors in multi-layer scenes are discussed.
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