Drizzle in Stratiform Boundary Layer Clouds. Part I: Vertical and Horizontal Structure
By R. Wood. 2005
196 citations recorded by the source corpus.
Subfields: Atmospheric Science, Earth-Surface Processes, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/d7acc5cf97fe6d1eb39f1fc5664a56b9d6a1f503
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- Bjorn Stevens
- Hugh Morrison
- Chris Bretherton
- G. Feingold
- R. Wood
- Wojciech W. Grabowski
- Hongli Jiang
- M. Khairoutdinov
In Earth-Surface Processes
- Bjorn Stevens
- Hugh Morrison
- G. Feingold
- Hongli Jiang
- Wojciech W. Grabowski
- R. Wood
- A. Lock
- J. Kirkby
In Global and Planetary Change
- Hugh Morrison
- Bjorn Stevens
- Chris Bretherton
- G. Feingold
- R. Wood
- Wojciech W. Grabowski
- Hongli Jiang
- M. Khairoutdinov
Citations in the corpus
- Cancellation of Aerosol Indirect Effects in Marine Stratocumulus through Cloud Thinning (2007, methodology): “The formulation used compares favorably with aircraft data (Wood 2005a).”
- Comparison of Bulk and Bin Warm-Rain Microphysics Models Using a Kinematic Framework (2007, background): “…5) This structure is consistent with observations of marine stratocumulus (e.g., Nicholls 1984; Duynkerke et al. 1995; Pawlowska and Brenguier 2000; Wood 2005a) The values of q c , N c , and cloud-base height vary considerably between the PRISTINE and POLLUTED simulations even though the overall…”
- An aircraft case study of the spatial transition from closed to open mesoscale cellular convection over the Southeast Pacific (2010, background): “This is typical behavior for overcast drizzling20 stratocumulus (Wood, 2005).”
- Large-Eddy Simulations of a Drizzling, Stratocumulus-Topped Marine Boundary Layer (2009, methodology): “In the mixed-layer modeling study of Wood (2007),”
- Spatial variability of liquid water path in marine low cloud : The importance of mesoscale cellular convection (2006, background): “…observations of boundary layer clouds indicate that the liquid water content is often an approximately linear function of height above cloud base, and that the cloud droplet concentration is approximately constant with height (e.g., Nicholls and Leighton 1986; Brenguier et al. 2000; Wood 2005).”
- Cosmic Rays and Climate (2005, background): “Cloud droplet concentrations of 100 cm−3 or less in boundary layer clouds produce substantial drizzle and CCN sedimentation [156].”
- The Influence of Entrainment and Mixing Assumption on Aerosol–Cloud Interactions in Marine Stratocumulus (2009, background): “6); however, observations of marine Sc (e.g., Noonkester 1984; Miles et al. 2000; Wood 2005) suggest TABLE 4.”