Observational evidence against strongly stabilizing tropical cloud feedbacks
We present a method to attribute cloud radiative feedbacks to convective processes, using sub-cloud layer buoyancy as a diagnostic of stable and deep convective regimes. Applying this approach to tropical remote-sensing measurements over years 2000-2016 shows that an inferred negative short-term clo...
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| Médium: | Journal article |
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American Geophysical Union
2017
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