| 1 | !----------------------------------------------------------------------- |
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| 2 | &namsbc_isf ! Top boundary layer (ISF) |
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| 3 | !----------------------------------------------------------------------- |
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| 4 | ! ! file name ! frequency (hours) ! variable ! time interpol. ! clim ! 'yearly'/ ! weights ! rotation ! |
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| 5 | ! ! ! (if <0 months) ! name ! (logical) ! (T/F) ! 'monthly' ! filename ! pairing ! |
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| 6 | ! nn_isf == 4 |
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| 7 | sn_qisf = 'rnfisf' , -12 ,'sohflisf', .false. , .true. , 'yearly' , '' , '' |
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| 8 | sn_fwfisf = 'rnfisf' , -12 ,'sowflisf', .false. , .true. , 'yearly' , '' , '' |
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| 9 | ! nn_isf == 3 |
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| 10 | sn_rnfisf = 'runoffs' , -12 ,'sofwfisf', .false. , .true. , 'yearly' , '' , '' |
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| 11 | ! nn_isf == 2 and 3 |
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| 12 | sn_depmax_isf = 'runoffs' , -12 ,'sozisfmax' , .false. , .true. , 'yearly' , '' , '' |
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| 13 | sn_depmin_isf = 'runoffs' , -12 ,'sozisfmin' , .false. , .true. , 'yearly' , '' , '' |
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| 14 | ! nn_isf == 2 |
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| 15 | sn_Leff_isf = 'rnfisf' , 0 ,'Leff' , .false. , .true. , 'yearly' , '' , '' |
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| 16 | ! for all case |
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| 17 | ln_divisf = .true. ! apply isf melting as a mass flux or in the salinity trend. (maybe I should remove this option as for runoff?) |
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| 18 | ! only for nn_isf = 1 or 2 |
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| 19 | rn_gammat0 = 1.0e-4 ! gammat coefficient used in blk formula |
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| 20 | rn_gammas0 = 1.0e-4 ! gammas coefficient used in blk formula |
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| 21 | ! only for nn_isf = 1 |
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| 22 | nn_isfblk = 1 ! 1 ISOMIP ; 2 conservative (3 equation formulation, Jenkins et al. 1991 ??) |
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| 23 | rn_hisf_tbl = 30. ! thickness of the top boundary layer (Losh et al. 2008) |
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| 24 | ! 0 => thickness of the tbl = thickness of the first wet cell |
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| 25 | ln_conserve = .true. ! conservative case (take into account meltwater advection) |
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| 26 | nn_gammablk = 1 ! 0 = cst Gammat (= gammat/s) |
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| 27 | ! 1 = velocity dependend Gamma (u* * gammat/s) (Jenkins et al. 2010) |
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| 28 | ! if you want to keep the cd as in global config, adjust rn_gammat0 to compensate |
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| 29 | ! 2 = velocity and stability dependent Gamma Holland et al. 1999 |
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| 30 | / |
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