- Timestamp:
- 2020-02-24T14:00:21+01:00 (4 years ago)
- File:
-
- 1 edited
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NEMO/branches/2020/KERNEL-03_Storkey_Coward_RK3_stage2/src/ICE/icethd_dh.F90
r10786 r12443 76 76 REAL(wp) :: zgrr ! bottom growth rate 77 77 REAL(wp) :: zt_i_new ! bottom formation temperature 78 REAL(wp) :: z1_rho ! 1/(rhos+r au0-rhoi)78 REAL(wp) :: z1_rho ! 1/(rhos+rho0-rhoi) 79 79 80 80 REAL(wp) :: zQm ! enthalpy exchanged with the ocean (J/m2), >0 towards the ocean … … 571 571 ! When snow load excesses Archimede's limit, snow-ice interface goes down under sea-level, 572 572 ! flooding of seawater transforms snow into ice dh_snowice is positive for the ice 573 z1_rho = 1._wp / ( rhos+r au0-rhoi )573 z1_rho = 1._wp / ( rhos+rho0-rhoi ) 574 574 DO ji = 1, npti 575 575 ! 576 dh_snowice(ji) = MAX( 0._wp , ( rhos * h_s_1d(ji) + (rhoi-r au0) * h_i_1d(ji) ) * z1_rho )576 dh_snowice(ji) = MAX( 0._wp , ( rhos * h_s_1d(ji) + (rhoi-rho0) * h_i_1d(ji) ) * z1_rho ) 577 577 578 578 h_i_1d(ji) = h_i_1d(ji) + dh_snowice(ji)
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