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Sensitivities in Satellite Lidar-Derived Estimates of Daytime Top-of-the-Atmosphere Optically Thin Cirrus Cloud Radiative Forcing: A Case Study
Journal article   Open access   Peer reviewed

Sensitivities in Satellite Lidar-Derived Estimates of Daytime Top-of-the-Atmosphere Optically Thin Cirrus Cloud Radiative Forcing: A Case Study

Erica K. Dolinar, James R. Campbell, Simone Lolli, Scott C. Ozog, John E. Yorks, Christopher Camacho, Yu Gu, Anthony Bucholtz and Matthew J. McGill
Geophysical research letters, Vol.47(17), p.e2020GL088871
09/16/2020
DOI: 10.1029/2020GL088871
url
https://doi.org/10.1029/2020GL088871View
Published (Version of record) Open Access

Abstract

An optically thin cirrus cloud was profiled concurrently with nadir-pointing 1,064 nm lidars on 11 August 2017 over eastern Texas, including NASA's airborne Cloud Physics Lidar (CPL) and space-borne Clouds and Aerosol Transport System (CATS) instruments. Despite resolving fewer (37% vs. 94%) and denser (i.e., more emissive) clouds (average cloud optical depth of 0.10 vs. 0.03, respectively), CATS data render a near-equal estimate of the top-of-atmosphere (TOA) net cloud radiative forcing (CRF) versus CPL. The sample-relative TOA net CRF solved from CPL is 1.39 W/m(2), which becomes 1.32 W/m(2)after normalizing by occurrence frequency. Since CATS overestimates extinction for this case, the sample-relative TOA net forcing is similar to 3.0 W/m(2)larger than CPL, with the absolute value reduced to within 0.3 W/m(2)of CPL due its underestimation of cloud occurrence. We discuss the ramifications of thin cirrus cloud detectability from satellite and its impact on attempts at TOA CRF closure.
Geology Physical Sciences Geosciences, Multidisciplinary Science & Technology

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