INTERFACE:
subroutine SnowCompaction (c)DESCRIPTION:
Determine the change in snow layer thickness due to compaction and settling. Three metamorphisms of changing snow characteristics are implemented, i.e., destructive, overburden, and melt. The treatments of the former two are from SNTHERM.89 and SNTHERM.99 (1991, 1999). The contribution due to melt metamorphism is simply taken as a ratio of snow ice fraction after the melting versus before the melting.USES:
use clmtype
use globals, only: dtime
use clm_varcon, only : denice, denh2o, tfrz
ARGUMENTS:
implicit none
type (column_type),target,intent(inout):: c !column derived type
CALLED FROM:
subroutine Hydrology2 in module Hydrology2ModREVISION HISTORY:
15 September 1999: Yongjiu Dai; Initial code 15 December 1999: Paul Houser and Jon Radakovich; F90 Revision 2/28/02, Peter Thornton: Migrated to new data structuresLOCAL VARIABLES:
local pointers to implicit in scalars
integer,pointer:: snl !number of snow layers
local pointers to implicit in arrays
integer,dimension(:),pointer:: imelt !flag for melting (=1), freezing (=2), Not=0
real(r8),dimension(:),pointer:: frac_iceold !fraction of ice relative to the tot water
real(r8),dimension(:),pointer:: t_soisno !soil temperature (Kelvin)
real(r8),dimension(:),pointer:: h2osoi_ice !ice lens (kg/m2)
real(r8),dimension(:),pointer:: h2osoi_liq !liquid water (kg/m2)
local pointers to implicit inout arrays
real(r8),dimension(:),pointer:: dz !layer depth (m)