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Investigation of the Diurnal Variation of Marine Boundary Layer Cloud Microphysical Properties at the Azores
Author(s) -
Xiquan Dong,
Baike Xi,
Peng Wu
Publication year - 2014
Publication title -
journal of climate
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 3.315
H-Index - 287
eISSN - 1520-0442
pISSN - 0894-8755
DOI - 10.1175/jcli-d-14-00434.1
Subject(s) - environmental science , daytime , atmospheric sciences , cloud height , liquid water path , diurnal temperature variation , sunrise , boundary layer , cloud base , cloud cover , climatology , longwave , cloud condensation nuclei , meteorology , convective boundary layer , planetary boundary layer , liquid water content , radiative transfer , cloud computing , precipitation , aerosol , geology , turbulence , geography , physics , quantum mechanics , computer science , thermodynamics , operating system
A new method has been developed to retrieve the nighttime marine boundary layer (MBL) cloud microphysical properties, which provides a complete 19-month dataset to investigate the diurnal variation of MBL cloud microphysical properties at the Azores. Compared to the corresponding daytime results presented in the authors' previous study over the Azores region, all nighttime monthly means of cloud liquid water path (LWP) exceed their daytime counterparts with an annual-mean LWP of 140 g m−2, which is ~30.9 g m−2 larger than daytime. Because the MBL clouds are primarily driven by convective instabilities caused by cloud-top longwave (LW) radiative cooling, more MBL clouds are well mixed and coupled with the surface during the night; thus, its cloud layer is deeper and its LWP is higher. During the day, the cloud layer is warmed by the absorption of solar radiation and partially offsets the cloud-top LW cooling, which makes the cloud layer thinner with less LWP. The seasonal and diurnal variations of ...

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