!----------------------------------------------------------------------- &namzgr_sco ! s-coordinate or hybrid z-s-coordinate !----------------------------------------------------------------------- ln_s_sh94 = .false. ! Song & Haidvogel 1994 hybrid S-sigma (T)| ln_s_sf12 = .true. ! Siddorn & Furner 2012 hybrid S-z-sigma (T)| if both are false the NEMO tanh stretching is applied ln_sigcrit = .true. ! use sigma coordinates below critical depth (T) or Z coordinates (F) for Siddorn & Furner stretch ! stretching coefficients for all functions rn_jpk = 51 ! Number of S levels ln_eq_taper = .false. ! Tapering of S coords near equator cn_coord_hgr = 'coordinates.nc' ! File containing gphit (latitude) coordinate for use if ln_eq_taper=.true. rn_sbot_min = 10.0 ! minimum depth of s-bottom surface (>0) (m) rn_sbot_max = 7000.0 ! maximum depth of s-bottom surface (= ocean depth) (>0) (m) rn_hc = 50.0 ! critical depth for transition to stretched coordinates !!!!!!! Envelop bathymetry rn_rmax = 0.3 ! maximum cut-off r-value allowed (0<r_max<1) !!!!!!! SH94 stretching coefficients (ln_s_sh94 = .true.) rn_theta = 6.0 ! surface control parameter (0<=theta<=20) rn_bb = 0.8 ! stretching with SH94 s-sigma !!!!!!! SF12 stretching coefficient (ln_s_sf12 = .true.) rn_alpha = 4.4 ! stretching with SF12 s-sigma rn_efold = 0.0 ! efold length scale for transition to stretched coord rn_zs = 1.0 ! depth of surface grid box ! bottom cell depth (Zb) is a linear function of water depth Zb = H*a + b rn_zb_a = 0.024 ! bathymetry scaling factor for calculating Zb rn_zb_b = -0.2 ! offset for calculating Zb !!!!!!!! Other stretching (not SH94 or SF12) [also uses rn_theta above] rn_thetb = 1.0 ! bottom control parameter (0<=thetb<= 1) /