Articles | Volume 21, issue 17
Atmos. Chem. Phys., 21, 13207–13225, 2021
https://doi.org/10.5194/acp-21-13207-2021
Atmos. Chem. Phys., 21, 13207–13225, 2021
https://doi.org/10.5194/acp-21-13207-2021

Research article 06 Sep 2021

Research article | 06 Sep 2021

Morning boundary layer conditions for shallow to deep convective cloud evolution during the dry season in the central Amazon

Alice Henkes et al.

Data sets

Observations and Modeling of the Green Ocean Amazon (GoAmazon) 2014/5 ARM Climate Research Facility https://www.arm.gov/research/campaigns/amf2014goamazon

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Short summary
The Amazonian boundary layer is investigated during the dry season in order to better understand the processes that occur between night and day until the stage where shallow cumulus clouds become deep. Observations show that shallow to deep clouds are characterized by a shorter morning transition stage (e.g., the time needed to eliminate the stable boundary layer inversion), while higher humidity above the boundary layer favors the evolution from shallow to deep cumulus clouds.
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