Marine stratocumulus clouds (FIRE)

Case description

The FIRE (First ISCCP Regional Experiment) case simulates marine stratocumulus clouds off the coast of California. This is a classic case for testing cloud-radiation interactions and LES modeling of marine boundary layer clouds. The case exists in two configurations: 1D (single column) and 3D (LES).

Warning

The 3D configuration requires MPI parallelization and the 1D configuration can only be run on a single core.

Configuration

Parameter

1D (FIRE_1D)

3D (FIRE)

Category

Idealized cases

HPC cases

Dynamics

3D with 1D turbulence

3D LES

Horizontal grid spacing

2500 m (1x1)

50 m (50x50)

Integration length

90000 s (25 hours)

90000 s (25 hours)

Time step

120 s

1 s

Coriolis effect

enabled

enabled

Turbulence

TKEL (1D)

TKEL (3D)

Cloud scheme

KHKO

KHKO

Deep convection

NONE

NONE

Radiation

ECMWF

ECMW

LES diagnostics

enabled

enabled

Declination

Configuration

Cloud scheme

Radiation

FIRE_1D/KHKO

KHKO

ECMWF

FIRE_1D/KHKO_MALA

KHKO

MALA

FIRE_1D/LIMA_ECRAD

LIMA

ECRAD

FIRE_1D/LIMA_MALA

LIMA

MALA

FIRE/CEN4TH_RKC4

KHKO

ECMW

FIRE/CEN4TH_LEFR

KHKO

ECMW

FIRE/CEN4TH_RKC4_LIMA_ECRAD

LIMA

ECRAD

FIRE/WENO5

KHKO

ECMW

Steps

Step

Script

001_prep_ideal

run_prep_ideal_case_xyz / run_prep_ideal

002_mesonh

run_mesonh_xyz / run_mesonh

Specificities

Scientific specificities

  • Marine stratocumulus layer with cloud-top radiative cooling

  • Sea surface temperature: 289 K prescribed

  • July 14, 1987 initialization (25200s UTC)

  • Geostrophic forcing with vertical motion

  • Cloud-radiation interactions

  • Different turbulence length scales (BL89 for 1D, DEAR for 3D)

Technical specificities

  • 1D: single point domain with 120 vertical levels

  • 3D: 50x50 horizontal grid (2.5km x 2.5km domain)

  • Cyclic boundary conditions for 3D

  • Initial perturbation (0.1 m/s vertical for 3D)

Validation

  • Cloud fraction evolution

  • Liquid water path

  • Radiative fluxes

  • Turbulent fluxes

Numerical ressources

1D: Single CPU (1 node, 1 core) 3D: 4 nodes, 256 cores (MPI parallel)

References

  • Randall, D.A., et al. (1996): Intercomparison of stratocumulus cloud fields during FIRE. Mon. Wea. Rev., 124, 137-156.