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ARM Releases New Cloud Optical Depth Product

Published: 8 July 2026

Three vertically stacked plots show mean Doppler velocity, reflectivity, and a comparison of multifilter rotating shadowband radiometer and sunphotometer product data.
Ka-Band ARM Zenith Radar (KAZR) mean Doppler velocity (a) and KAZR radar reflectivity factor (b) are shown for a September 10, 2017, stratocumulus cloud event at ARM’s Eastern North Atlantic atmospheric observatory. The lower panel (c) plots examples of cloud optical depth retrievals for this event from the SPHOTCOD value-added product (red) and the one-minute version of ARM’s Cloud Optical Properties from the Multifilter Rotating Shadowband Radiometer (MFRSRCLDOD1MIN) value-added product (blue). Image was adapted from the journal Atmospheric Measurement Techniques (Sookdar et al. 2025).

At its fixed-location atmospheric observatories and mobile sites, the Atmospheric Radiation Measurement (ARM) User Facility operates Cimel sunphotometers, multi-channel scanning photometers for passive remote sensing of the atmosphere. The sunphotometers are calibrated and maintained by the AErosol RObotic NETwork (AERONET), which also processes certain data as part of its global archive.

ARM has developed the Three-Channel Sunphotometer Cloud Mode value-added product (SPHOTCOD VAP) to provide information on cloud properties for process studies, including insights on the cloud droplet effective radius, cloud optical depth, and/or liquid water path.

SPHOTCOD retrieves cloud properties from sunphotometer data at three channels (wavelengths of 440, 870, and 1640 nanometers) following published methods of Chiu et al. (2012) and Sookdar et al. (2025). For its inputs, the VAP uses zenith radiance measurements at the three wavelengths from AERONET, solar constant values, and surface albedo data from the satellite-based Moderate Resolution Imaging Spectroradiometer (MODIS).

The VAP retrieves two cloud quantities, the cloud optical depth and cloud droplet effective radius, and estimates liquid water path based on these quantities. Scientists can use the data for studies of cloud processes, cloud-aerosol interactions, and cloud radiative impacts.

More information about the VAP, including the technical report, can be found on the SPHOTCOD web page.

SPHOTCOD is available in daily netCDF files for the following ARM sites and date ranges:

Additional VAP data will be processed from the SGP and ENA along with data from the Bankhead National Forest observatory in Alabama and the 2018–2019 Cloud, Aerosol, and Complex Terrain Interactions (CACTI) campaign in Argentina.

Access the SPHOTCOD data in the ARM Data Center. (To download the data, first create an ARM account.)

For questions or to report data issues, please contact ARM translator Min Deng, science sponsors Christine Chiu and Scott Giangrande, and/or VAP developer Lynn Ma.

Data can be referenced as doi:10.5439/1668057.

References:

Chiu JC, A Marshak, CH Huang, T Varnai, RJ Hogan, DM Giles, BN Holben, EJ O’Connor, Y Knyazikhin, and WJ Wiscombe. 2012. “Cloud droplet size and liquid water path retrievals from zenith radiance measurements: examples from the Atmospheric Radiation Measurement Program and the Aerosol Robotic Network.” Atmospheric Chemistry and Physics, 12(21):10313-10329, https://doi.org/10.5194/acp-12-10313-2012

Sookdar K, S Giangrande, J Rausch, L Ma, M Wang, D Wang, M Jensen, C Hung, and J Chiu. 2025. “Marine and continental stratocumulus cloud microphysical properties obtained from routine ARM Cimel sunphotometer observations.” Atmospheric Measurement Techniques, 18(21):6271-6289, https://doi.org/10.5194/amt-18-6271-2025

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ARM is a DOE Office of Science user facility operated by nine DOE national laboratories.

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Atmospheric Radiation Measurement (ARM) | Reviewed March 2025