Published May 15, 2026 | Version v1

Global Above-cloud Aerosol Optical Depth Dataset from CALIOP Depolarization Ratio Method

  • 1. ROR icon Morgan State University
  • 2. ROR icon Science and Technology Corporation (United States)
  • 3. ROR icon Goddard Space Flight Center
  • 4. ROR icon Langley Research Center

Description

The Depolarization Ratio (DR) method, developed by Hu et al. (2007), was applied to the long term (2006-2022) CALIOP global, cloud-sky observations to retrieve aerosol optical depth above clouds (ACAOD) at 532 nm. The DR method was among the first lidar-based remote sensing technique to quantify the aerosol loading over clouds without involving any specific assumptions about detailed vertical profiles of aerosols and their optical-microphysical properties, except for the lidar ratio of the cloud layer. Physically based on the two-way transmission of lidar signal, the DR method uses 1) layer-integrated attenuated backscatter at 532 nm, γ'532, and 2) layer-integrated attenuated depolarization ratio at 532 nm, d'532, along with CALIOP Level-2 aerosol and cloud layer products for identifying respective layers, to deduce the optical depth of aerosols above opaque water clouds (OWCs).  

The validation of DR-retrieved ACAOD against the direct airborne measurements acquired from HSRL-2 lidar and 4STAR sun photometer operated during the ORACLES field campaign in 2016-2018 over the southeastern Atlantic Ocean showed that both datasets correlate well (R2~0.95 for HSRL-2 and R2~0.75 for 4STAR) against airborne measurements. However, DR ACAOD retrievals were biased high by ~0.088.

The Extinction Ångström Exponent was derived from the combination of DR method ACAOD and measured color ratio (1064-532 nm) information from CALIOP. Taking advantage of extinction optical depth and backscatter measurements, the above-cloud aerosol lidar ratio was also calculated.

The multiyear (2006-2022) dataset of optical properties of above-cloud aerosol derived from CALIOP daytime and nighttime observations is presented here.

This dataset is associated with the following publication:

Jethva, H., Kayetha, V., Torres. O., Hu, Y.: Global Retrieval Dataset of UV-VIS Extinction and Absorption of Above-cloud Aerosols from Synergy of A-train Active-Passive measurements: Part I—Above-cloud Aerosol Optical Depth from CALIOP Depolarization Ratio Method, Frontiers Environmental Science, Enivronmental Informatics and Remote Sensing, Accepted, 2026.

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CALIOP-DR-ACAOD-Dataset-v1.zip

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Additional details

Funding

National Aeronautics and Space Administration
A one-and-half decade long global characterization of absorbing aerosols over clouds and sea-ice/snow using a synergy of A-train sensors OMI, CALIOP, MODIS, and CERES