Causes of WRF surface energy fluxes biases in a stratocumulus region
Authors:
- 23 April 2015
- journal article
- research article
- Published by Springer Nature in Climate Dynamics
- Vol. 46 (1-2) , 571-584
Abstract
No abstract availableKeywords
This publication has 37 references indexed in Scilit:
- The VAMOS Ocean-Cloud-Atmosphere-Land Study Regional Experiment (VOCALS-REx): goals, platforms, and field operationsEGUsphere, 2010
- Performance of an Eddy Diffusivity–Mass Flux Scheme for Shallow Cumulus Boundary LayersMonthly Weather Review, 2010
- Marine boundary layer over the subtropical southeast Pacific during VOCALS-REx – Part 2: Synoptic variabilityAtmospheric Chemistry and Physics, 2010
- A Combined Eddy-Diffusivity Mass-Flux Approach for the Convective Boundary LayerJournal of the Atmospheric Sciences, 2007
- ‘Application of a New Spectral Theory of Stably Stratified Turbulence to the Atmospheric Boundary Layer over Sea Ice’Boundary-Layer Meteorology, 2005
- An eddy‐diffusivity/mass‐flux parametrization for dry and shallow cumulus convectionQuarterly Journal of the Royal Meteorological Society, 2004
- The Step-Mountain Eta Coordinate Model: Further Developments of the Convection, Viscous Sublayer, and Turbulence Closure SchemesMonthly Weather Review, 1994
- A One-Dimensional Entraining/Detraining Plume Model and Its Application in Convective ParameterizationJournal of the Atmospheric Sciences, 1990
- Numerical Study of Convection Observed during the Winter Monsoon Experiment Using a Mesoscale Two-Dimensional ModelJournal of the Atmospheric Sciences, 1989
- Development of a turbulence closure model for geophysical fluid problemsReviews of Geophysics, 1982