1.2 Determination of ICESat-2 Aerosol Type and Cloud Phase Using MERRA-2 Reanalysis Data

Monday, 13 January 2025: 9:00 AM
336 (New Orleans Ernest N. Morial Convention Center)
Kenneth Christian, University of Maryland, Greenbelt, MD; and J. E. Yorks, E. P. Nowottnick, and S. P. Palm

In addition to the detailed altimetry products of the Ice, Cloud, and Land Elevation Satellite 2 (ICESat-2), basic atmospheric products have been developed, including calibrated backscatter profiles and cloud and aerosol layer detection. With being limited to a single 532nm wavelength without depolarization, feature subtyping and extinction retrievals are not feasible using heritage space-based lidar algorithms such as employed by NASA’s Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) (2006-2023) and Cloud-Aerosol Transport System (CATS) (2015-2017). To allow for the classification of cloud phase and aerosol type for detected ICESat-2 cloud and aerosol layers, we sample Modern-Era Retrospective analysis for Research and Applications, Version 2 (MERRA-2) reanalysis along the ICESat-2 orbit. Using cloud phase and aerosol type climatologies, we show MERRA-2-assisted feature subtypes can produce similar global distributions of cloud phase and aerosol type. Orbital coincidences between ICESat-2 and CALIOP show these model assisted feature subtypes compare favorably to those determined by CALIOP and its algorithms. Expanding the atmospheric products from ICESat-2 to include cloud phase and aerosol type will allow for lidar ratios to be assigned, facilitating the future development of layer optical depths.
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