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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 12) Peer-ReviewedCloud droplet number concentration (N.sub.d) is of central importance to observation-based estimates of aerosol indirect effects, being used to quantify both the cloud sensitivity to aerosol and the base state of the...
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