Case 1:
Tropical oceanic squall line
Two- and three-dimensional modeling of a squall
line on a time scale of a few hours. The initial conditions and
evaluation data sets were obtained as part of an intensive observation
period in TOGA COARE.
Case
1 description and results
Paper on
cloud-resolving model intercomparison results
Paper on single-column
model intercomparison results
Leader: Jean-Luc
Redelsperger
Case 2: Tropical oceanic deep convection
Two- and three-dimensional modeling of the evolution
of convection subjected to observed, time-dependent, large-scale
forcing on a time scale of a week. Initial conditions for the
simulations, the evolving large-scale forcing and the data used
in model evaluation are averages over the TOGA COARE Intensive
Flux Array (IFA).
Case 2 description
and results
Leader: Steve
Krueger
Case 2 radiation code offline intercomparison
The purpose of this exercise is to examine and compare
the surface heat fluxes, radiative heating rates and fluxes, and
microphysical fields from the CRM and SCM models at one instant
of time during the Case 2 period.
Description
Leaders: Wei-Kuo
Tao and Dan Johnson
Case
3: Continental deep convection
This model intercomparison case involves two new
aspects:
Case 3 description
and results
Leaders: Steve
Krueger and Kuan-Man Xu
EUROCS (EUROpean Cloud Systems):
The project EUROCS aims to improve the treatment
of cloud systems in global and regional climate models. EUROCS
concentrates its efforts on four major and well identified deficiencies
of climate models: i) stratocumulus over ocean, ii) diurnal cycle
of cumulus, iii) diurnal cycle of precipitating deep convection
over continents, and iv) sensitivity of deep convection development
to the moisture profile. The last two areas (diurnal cycle of
deep convection, led by Francoise Guichard and Jon Petch, and
sensitivity of deep convection to the moisture profile, led by
Stephen Derbyshire) are part of WG4 activities.
See the EUROCS
web page for case descriptions and results.
Proposed Case 4: Daytime convective development over land: an
idealized
case based on TRMM-LBA observations.
Wojciech W. Grabowski, NCAR
(with data provided by Steve Lang, NASA Goddard)
The purpose of this case is to investigate the development
of the daytime convective boundary layer over land and the transition
from shallow to deep convection.
Case 4 description
Procedures to submit Case 4 results
Example of Results
Results from benchmark set of simulations