- Timestamp:
- 2020-07-03T20:46:53+02:00 (4 years ago)
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NEMO/branches/2020/dev_r12558_HPC-08_epico_Extra_Halo/src/OCE/ZDF/zdfiwm.F90
r12960 r13248 51 51 !! * Substitutions 52 52 # include "do_loop_substitute.h90" 53 # include "domzgr_substitute.h90" 53 54 !!---------------------------------------------------------------------- 54 55 !! NEMO/OCE 4.0 , NEMO Consortium (2018) … … 94 95 !! 2. Pycnocline-intensified low-mode dissipation 95 96 !! zemx_iwm(z) = ( epyc_iwm / rho0 ) * ( sqrt(rn2(z))^nn_zpyc ) 96 !! / SUM( sqrt(rn2(z))^nn_zpyc * e3w (z) )97 !! / SUM( sqrt(rn2(z))^nn_zpyc * e3w[z) ) 97 98 !! where epyc_iwm is a map of available power, and nn_zpyc 98 99 !! is the chosen stratification-dependence of the internal wave … … 100 101 !! 3. WKB-height dependent high mode dissipation 101 102 !! zemx_iwm(z) = ( ebot_iwm / rho0 ) * rn2(z) * EXP(-z_wkb(z)/hbot_iwm) 102 !! / SUM( rn2(z) * EXP(-z_wkb(z)/hbot_iwm) * e3w (z) )103 !! / SUM( rn2(z) * EXP(-z_wkb(z)/hbot_iwm) * e3w[z) ) 103 104 !! where hbot_iwm is the characteristic length scale of the WKB bottom 104 105 !! intensification, ebot_iwm is a map of available power, and z_wkb is the 105 106 !! WKB-stretched height above bottom defined as 106 !! z_wkb(z) = H * SUM( sqrt(rn2(z'>=z)) * e3w (z'>=z) )107 !! / SUM( sqrt(rn2(z')) * e3w (z') )107 !! z_wkb(z) = H * SUM( sqrt(rn2(z'>=z)) * e3w[z'>=z) ) 108 !! / SUM( sqrt(rn2(z')) * e3w[z') ) 108 109 !! 109 110 !! - update the model vertical eddy viscosity and diffusivity:
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