NAM_ISBAn

Warning

This namelist comes from SURFEX 9.0.0 user guide https://www.umr-cnrm.fr/surfex/IMG/pdf/surfex_tecdoc.pdf.

NAM_ISBAn content

Fortran name

Fortran type

Default value

CC1DRY

CHARACTER(LEN=4)

‘DEF’

CSCOND

CHARACTER(LEN=4)

‘PL98’

CSOILFRZ

CHARACTER(LEN=3)

‘DEF’

CDIFSFCOND

CHARACTER(LEN=4)

‘DEF’

CSNOWRES

CHARACTER(LEN=3)

‘DEF’

CCPSURF

CHARACTER(LEN=3)

‘DRY’

CZ0HEAT

CHARACTER(LEN=3)

‘DEF’

XTSTEP

REAL

none

XCVHEATF

REAL

0.20

XCGMAX

REAL

2.E-5

XCDRAG

REAL

0.15

XZ0HEAT

REAL

0.0

LGLACIER

LOGICAL

.FALSE.

LCANOPY_DRAG

LOGICAL

.FALSE.

LVEGUPD

LOGICAL

.TRUE.

LPERTSURF

LOGICAL

.TRUE.

  • CC1DRY : type of C1 formulation for dry soils. The following options are currently available:

    • ‘DEF’ : Giard-Bazile formulation

    • ‘GB93’ : Giordani 1993, Braud 1993

  • CSCOND : type of thermal conductivity. The following options are currently available:

    • ‘NP89’ : Noilhan and Planton (1989) formula

    • ‘PL98’ : Peters-Lidard et al. (1998) formula

  • CSOILFRZ : type of soil freezing-physics option. The following options are currently available:

    • ‘DEF’ : Boone et al. 2000; Giard and Bazile 2000

    • ‘LWT’ : Phase changes as above, but relation between unfrozen water and temperature considered

  • CDIFSFCOND : type of Mulch effects. The following options are currently available:

    • ‘DEF’ : no mulch effect

    • ‘MLCH’ : include the insulating effect of leaf litter/mulch on the surf. thermal cond.

  • CSNOWRES : type of turbulent exchanges over snow. The following options are currently available:

    • ‘DEF’ : Louis

    • ‘RIL’ : Maximum Richardson number limit for stable conditions ISBA-SNOW3L turbulent exchange option

    • ‘M98’ : Martin et Lejeune 1998: older computation for turbulent fluxes coefficents in Crocus

  • CZ0HEAT : roughness length for heat

  • CCPSURF : type of specific heat at surface. The following options are currently available:

    • ‘DRY’ : specific heat does not depend on humidity at surface

    • ‘HUM’ : specific heat depends on humidity at surface.

  • XTSTEP : time step for ISBA. Default is to use the time-step given by the atmospheric coupling (seconds).

  • XCVHEATF : Modify Cv to compensate biases in ground temperature

  • XCGMAX : maximum value for soil heat capacity.

  • XCDRAG : drag coefficient in canopy.

  • XZ0HEAT : factor to calculate Z0H when CZ0HEAT=”Z95”

  • LGLACIER : If activated, specific treatment (as in Arpege) over permanent snow/ice regions. Snow depth initialised to 10m and soil ice to porosity. During the run, snow albedo ranges from 0.8 to 0.85

  • LCANOPY_DRAG : drag activated in SBL scheme within the canopy

  • LVEGUPD : True = update vegetation parameters every decade

  • LPERTSURF : if T modification of surface fluxes for ensemble forecasting