Effects of environment forcing on marine boundary layer cloud-drizzle processes

Author:

Wu Peng1,Dong Xiquan1ORCID,Xi Baike2ORCID,Liu Yangang3ORCID,Thieman Mandana4,Minnis Patrick5ORCID

Affiliation:

1. Department of Hydrology and Atmospheric Sciences; University of Arizona; Tucson Arizona USA

2. Department of Atmospheric Sciences; University of North Dakota; Grand Forks North Dakota USA

3. Brookhaven National Laboratory; Upton New York USA

4. Science Systems, and Applications, Inc.; Hampton Virginia USA

5. NASA Langley Research Center; Hampton Virginia USA

Funder

DOE CESM

NASA CERES

DOE ASR program

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

Reference83 articles.

1. Large-eddy simulations of a drizzling, stratocumulus-topped marine boundary layer;Ackerman;Mon. Weather Rev.,2009

2. Surface-based remote sensing of the observed and the adiabatic liquid water content of stratocumulus clouds;Albrecht;Geophys. Res. Lett.,1990

3. Precipitation in stratocumulus clouds: Observations and modelling results;Austin;J. Atmos. Sci.,1995

4. Variability in concentrations of cloud condensation nuclei in the marine cloud-topped boundary layer;Baker;Tellus,1993

5. A general formulation of collection rates of cloud and raindrops using the kinetic equation and comparison with parameterizations;Beheng;Beitr. Phys. Atmos.,1986

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