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Changeset 11123 for NEMO/trunk/doc/latex/NEMO/subfiles/chap_DIU.tex – NEMO

Ignore:
Timestamp:
2019-06-17T14:22:27+02:00 (5 years ago)
Author:
nicolasmartin
Message:

Modification of LaTeX subfiles accordingly to new citations keys

Location:
NEMO/trunk/doc/latex/NEMO/subfiles
Files:
2 edited

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  • NEMO/trunk/doc/latex/NEMO/subfiles

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  • NEMO/trunk/doc/latex/NEMO/subfiles/chap_DIU.tex

    r10442 r11123  
    6060%=============================================================== 
    6161 
    62 The warm layer is calculated using the model of \citet{Takaya_al_JGR10} (TAKAYA10 model hereafter). 
     62The warm layer is calculated using the model of \citet{takaya.bidlot.ea_JGR10} (TAKAYA10 model hereafter). 
    6363This is a simple flux based model that is defined by the equations 
    6464\begin{align} 
     
    8787where $Q_{\rm{h}}$ is the sensible and latent heat flux, $Q_{\rm{lw}}$ is the long wave flux, 
    8888and $Q_{\rm{sol}}$ is the solar flux absorbed within the diurnal warm layer. 
    89 For $Q_{\rm{sol}}$ the 9 term representation of \citet{Gentemann_al_JGR09} is used. 
     89For $Q_{\rm{sol}}$ the 9 term representation of \citet{gentemann.minnett.ea_JGR09} is used. 
    9090In equation \autoref{eq:ecmwf1} the function $f(L_a)=\max(1,L_a^{\frac{2}{3}})$, 
    9191where $L_a=0.3$\footnote{ 
     
    118118%=============================================================== 
    119119 
    120 The cool skin is modelled using the framework of \citet{Saunders_JAS82} who used a formulation of the near surface temperature difference based upon the heat flux and the friction velocity $u^*_{w}$. 
     120The cool skin is modelled using the framework of \citet{saunders_JAS67} who used a formulation of the near surface temperature difference based upon the heat flux and the friction velocity $u^*_{w}$. 
    121121As the cool skin is so thin (~1\,mm) we ignore the solar flux component to the heat flux and the Saunders equation for the cool skin temperature difference $\Delta T_{\rm{cs}}$ becomes 
    122122\[ 
     
    132132\end{equation} 
    133133where $\mu$ is the kinematic viscosity of sea water and $\lambda$ is a constant of proportionality which 
    134 \citet{Saunders_JAS82} suggested varied between 5 and 10. 
     134\citet{saunders_JAS67} suggested varied between 5 and 10. 
    135135 
    136 The value of $\lambda$ used in equation (\autoref{eq:sunders_thick_eqn}) is that of \citet{Artale_al_JGR02}, 
    137 which is shown in \citet{Tu_Tsuang_GRL05} to outperform a number of other parametrisations at 
     136The value of $\lambda$ used in equation (\autoref{eq:sunders_thick_eqn}) is that of \citet{artale.iudicone.ea_JGR02}, 
     137which is shown in \citet{tu.tsuang_GRL05} to outperform a number of other parametrisations at 
    138138both low and high wind speeds. 
    139139Specifically, 
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