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From:Atmospheric Measurement Techniques (Vol. 15, Issue 12) Peer-ReviewedClouds warm the surface in the longwave (LW), and this warming effect can be quantified through the surface LW cloud radiative effect (CRE). The global surface LW CRE has been estimated over more than 2 decades using...
From:Atmospheric Measurement Techniques (Vol. 15, Issue 6) Peer-ReviewedThe features detected in monolayer atmospheric columns sounded by the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) and classified as cloud or aerosol layers by the CALIOP version 4 (V4) cloud and aerosol...
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