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Airborne HSRL Assessment of CALIOP Aerosol Extinction Retrievals Constrained by Column AODCurrent operational CALIOP aerosol extinction profile retrievals usually rely on accurately specifying the relationship between aerosol extinction and backscattering (i.e. lidar ratio). Uncertainties in the assigned lidar ratios are typically the largest source of systematic error (~30-50%) in the CALIOP retrievals of aerosol extinction, backscatter, and aerosol optical depth. Alternatively, column aerosol optical depth (AOD) can be used to solve the lidar equation and obtain column-equivalent lidar ratios and retrieve aerosol extinction profiles from the CALIOP attenuated backscatter profiles. These derived lidar ratios correspond to the aerosols in the altitude range from 0-7 km.

We derive column-equivalent aerosol lidar ratios and aerosol extinction profiles from CALIOP attenuated backscatter profiles constrained using co-located column AODs provided by several instruments/techniques: Synergized Optical Depth of Aerosols (SODA), Ocean-Derived Column Optical Depths (ODCOD), MODIS (dark target), MODIS (Multi-Angle Implementation of Atmospheric Correction-MAIAC), and PARASOL (Generalized Retrieval of Aerosol and Surface Properties-GRASP). These various retrievals of AOD and the column-average aerosol lidar ratios and aerosol extinction profiles derived from CALIOP using these AOD constraints are evaluated using the extensive record of coincident and co-located airborne HSRL measurements of AOD, aerosol lidar ratio, and aerosol extinction profiles acquired during more than 140 HSRL underflights of CALIPSO since 2006. The HSRL technique allows for the independent measurement of extinction and backscatter without the need for external constraints or assumptions regarding the lidar ratios. Initial comparisons with these coincident HSRL aerosol extinction profiles show that the CALIOP aerosol extinction profiles retrieved using these various AOD constraints are generally in better agreement with the HSRL measurements than aerosol extinction profiles from the operational techniques. The quality of agreement depends on the accuracy and magnitude of the AOD constraint. We present these comparisons of AOD, column aerosol lidar ratio, and aerosol extinction profiles for each of the AOD constraints described above.
Document ID
20230017552
Acquisition Source
Langley Research Center
Document Type
Presentation
Authors
Richard Ferrare
(Langley Research Center Hampton, Virginia, United States)
John Hair
(Langley Research Center Hampton, Virginia, United States)
Chris Hostetler
(Langley Research Center Hampton, Virginia, United States)
Marian Clayton
(Coherent Applications, Inc - Psionic LLC Hampton, VA, USA)
Marta Fenn
(Coherent Applications, Inc - Psionic LLC Hampton, VA, USA)
Sharon Burton
(Langley Research Center Hampton, Virginia, United States)
Rob Ryan
(Coherent Applications, Inc - Psionic LLC Hampton, VA, USA)
Sharon Rodier
(Adnet Systems (United States) Bethesda, Maryland, United States)
Mark Vaughan
(Langley Research Center Hampton, Virginia, United States)
Date Acquired
December 1, 2023
Subject Category
Meteorology and Climatology
Meeting Information
Meeting: Fall AGU Meeting
Location: San Francisco, CA
Country: US
Start Date: December 11, 2023
End Date: December 15, 2023
Sponsors: American Geophysical Union
Funding Number(s)
WBS: 967701.02.01.02.85
Distribution Limits
Public
Copyright
Public Use Permitted.
Keywords
lidar
aerosol
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