Changeset 14616
- Timestamp:
- 2021-03-18T17:35:09+01:00 (3 years ago)
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- 1 edited
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NEMO/branches/UKMO/NEMO_4.0.4_penetrating_solar/src/OCE/SBC/sbccpl.F90
r14562 r14616 1883 1883 CASE( 'oce only' ) ! the required field is directly provided 1884 1884 1885 ! Get the sea ice non solar heat flux from conductive , melting and sublimationfluxes1885 ! Get the sea ice non solar heat flux from conductive and melting fluxes 1886 1886 IF( TRIM(sn_rcv_iceflx%cldes) == 'coupled' ) THEN 1887 1887 zqns_ice(:,:,:) = qml_ice(:,:,:) + qcn_ice(:,:,:) … … 1958 1958 ! --- heat content of evap over ice in W/m2 (to be used in 1D-thermo) --- ! 1959 1959 DO jl = 1, jpl 1960 zqevap_ice(:,:,jl) = 0._wp ! should be -evap * ( ( Tice - rt0 ) * rcpi ) but atm. does not take it into account 1960 ! zqevap_ice(:,:,jl) = 0._wp ! should be -evap * ( ( Tice - rt0 ) * rcpi ) but atm. does not take it into account 1961 1962 ! How much enthalpy is stored in sublimating snow and ice. At this stage we don't know if it is snow or ice that is 1963 ! sublimating so we will use the combined snow and ice layer temperature t1_ice. 1964 zqevap_ice(:,:,jl) = -zevap_ice(:,:,jl) * ( ( rt0 - t1_ice(:,:,jl) ) * rcpi + rLfus ) 1965 1966 ! This enthalpy change should always be negative as only positive sublimation is used (energy loss from the ice). 1967 WHERE( zqevap_ice(:,:,jl) > 0._wp ) zqevap_ice(:,:,jl) = 0._wp 1961 1968 END DO 1962 1969
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