Changeset 11551 for NEMO/trunk/doc/latex/NEMO/subfiles/chap_SBC.tex
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- 2019-09-16T16:53:24+02:00 (5 years ago)
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NEMO/trunk/doc/latex/NEMO/subfiles/chap_SBC.tex
r11543 r11551 1063 1063 \item[\np{nn\_gammablk}\forcode{=0}]: 1064 1064 The salt and heat exchange coefficients are constant and defined by \np{rn\_gammas0} and \np{rn\_gammat0}. 1065 \[ 1066 % \label{eq:SBC_isf_gamma_iso} 1067 \gamma^{T} = \np{rn\_gammat0} 1068 \] 1069 \[ 1070 \gamma^{S} = \np{rn\_gammas0} 1071 \] 1065 \begin{gather*} 1066 % \label{eq:SBC_isf_gamma_iso} 1067 \gamma^{T} = rn\_gammat0 \\ 1068 \gamma^{S} = rn\_gammas0 1069 \end{gather*} 1072 1070 This is the recommended formulation for ISOMIP. 1073 1071 \item[\np{nn\_gammablk}\forcode{=1}]: 1074 1072 The salt and heat exchange coefficients are velocity dependent and defined as 1075 \[ 1076 \gamma^{T} = \np{rn\_gammat0} \times u_{*} 1077 \] 1078 \[ 1079 \gamma^{S} = \np{rn\_gammas0} \times u_{*} 1080 \] 1073 \begin{gather*} 1074 \gamma^{T} = rn\_gammat0 \times u_{*} \\ 1075 \gamma^{S} = rn\_gammas0 \times u_{*} 1076 \end{gather*} 1081 1077 where $u_{*}$ is the friction velocity in the top boundary layer (ie first \np{rn\_hisf\_tbl} meters). 1082 1078 See \citet{jenkins.nicholls.ea_JPO10} for all the details on this formulation. It is the recommended formulation for realistic application.
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