\hypertarget{interfacemom__eos__teos10_1_1calculate__density__teos10}{}\section{mom\+\_\+eos\+\_\+teos10\+:\+:calculate\+\_\+density\+\_\+teos10 Interface Reference} \label{interfacemom__eos__teos10_1_1calculate__density__teos10}\index{mom\+\_\+eos\+\_\+teos10\+::calculate\+\_\+density\+\_\+teos10@{mom\+\_\+eos\+\_\+teos10\+::calculate\+\_\+density\+\_\+teos10}} \subsection{Detailed Description} Compute the in situ density of sea water (\mbox{[}kg m-\/3\mbox{]}), or its anomaly with respect to a reference density, from absolute salinity (g/kg), conservative temperature (in deg C), and pressure \mbox{[}Pa\mbox{]}, using the T\+E\+O\+S10 expressions. Definition at line 28 of file M\+O\+M\+\_\+\+E\+O\+S\+\_\+\+T\+E\+O\+S10.\+F90. \subsection*{Private functions} \begin{DoxyCompactItemize} \item subroutine \mbox{\hyperlink{interfacemom__eos__teos10_1_1calculate__density__teos10_a83d2f50d5a2bc0a2d4f95fcb02d0cbf5}{calculate\+\_\+density\+\_\+scalar\+\_\+teos10}} (T, S, pressure, rho, rho\+\_\+ref) \begin{DoxyCompactList}\small\item\em This subroutine computes the in situ density of sea water (rho in \mbox{[}kg m-\/3\mbox{]}) from absolute salinity (S \mbox{[}g kg-\/1\mbox{]}), conservative temperature (T \mbox{[}degC\mbox{]}), and pressure \mbox{[}Pa\mbox{]}. It uses the expression from the T\+E\+O\+S10 website. \end{DoxyCompactList}\item subroutine \mbox{\hyperlink{interfacemom__eos__teos10_1_1calculate__density__teos10_a2ab737753cfcb32c4181a656c30c07fd}{calculate\+\_\+density\+\_\+array\+\_\+teos10}} (T, S, pressure, rho, start, npts, rho\+\_\+ref) \begin{DoxyCompactList}\small\item\em This subroutine computes the in situ density of sea water (rho in \mbox{[}kg m-\/3\mbox{]}) from absolute salinity (S \mbox{[}g kg-\/1\mbox{]}), conservative temperature (T \mbox{[}degC\mbox{]}), and pressure \mbox{[}Pa\mbox{]}. It uses the expression from the T\+E\+O\+S10 website. \end{DoxyCompactList}\end{DoxyCompactItemize} \subsection{Detailed Description} Compute the in situ density of sea water (\mbox{[}kg m-\/3\mbox{]}), or its anomaly with respect to a reference density, from absolute salinity (g/kg), conservative temperature (in deg C), and pressure \mbox{[}Pa\mbox{]}, using the T\+E\+O\+S10 expressions. Definition at line 28 of file M\+O\+M\+\_\+\+E\+O\+S\+\_\+\+T\+E\+O\+S10.\+F90. \subsection{Functions and subroutines} \mbox{\Hypertarget{interfacemom__eos__teos10_1_1calculate__density__teos10_a2ab737753cfcb32c4181a656c30c07fd}\label{interfacemom__eos__teos10_1_1calculate__density__teos10_a2ab737753cfcb32c4181a656c30c07fd}} \index{mom\+\_\+eos\+\_\+teos10\+::calculate\+\_\+density\+\_\+teos10@{mom\+\_\+eos\+\_\+teos10\+::calculate\+\_\+density\+\_\+teos10}!calculate\+\_\+density\+\_\+array\+\_\+teos10@{calculate\+\_\+density\+\_\+array\+\_\+teos10}} \index{calculate\+\_\+density\+\_\+array\+\_\+teos10@{calculate\+\_\+density\+\_\+array\+\_\+teos10}!mom\+\_\+eos\+\_\+teos10\+::calculate\+\_\+density\+\_\+teos10@{mom\+\_\+eos\+\_\+teos10\+::calculate\+\_\+density\+\_\+teos10}} \subsubsection{\texorpdfstring{calculate\+\_\+density\+\_\+array\+\_\+teos10()}{calculate\_density\_array\_teos10()}} {\footnotesize\ttfamily subroutine mom\+\_\+eos\+\_\+teos10\+::calculate\+\_\+density\+\_\+teos10\+::calculate\+\_\+density\+\_\+array\+\_\+teos10 (\begin{DoxyParamCaption}\item[{real, dimension(\+:), intent(in)}]{T, }\item[{real, dimension(\+:), intent(in)}]{S, }\item[{real, dimension(\+:), intent(in)}]{pressure, }\item[{real, dimension(\+:), intent(out)}]{rho, }\item[{integer, intent(in)}]{start, }\item[{integer, intent(in)}]{npts, }\item[{real, intent(in), optional}]{rho\+\_\+ref }\end{DoxyParamCaption})\hspace{0.3cm}{\ttfamily [private]}} This subroutine computes the in situ density of sea water (rho in \mbox{[}kg m-\/3\mbox{]}) from absolute salinity (S \mbox{[}g kg-\/1\mbox{]}), conservative temperature (T \mbox{[}degC\mbox{]}), and pressure \mbox{[}Pa\mbox{]}. It uses the expression from the T\+E\+O\+S10 website. \begin{DoxyParams}[1]{Parameters} \mbox{\tt in} & {\em t} & Conservative temperature \mbox{[}degC\mbox{]}.\\ \hline \mbox{\tt in} & {\em s} & Absolute salinity \mbox{[}g kg-\/1\mbox{]}\\ \hline \mbox{\tt in} & {\em pressure} & pressure \mbox{[}Pa\mbox{]}.\\ \hline \mbox{\tt out} & {\em rho} & in situ density \mbox{[}kg m-\/3\mbox{]}.\\ \hline \mbox{\tt in} & {\em start} & the starting point in the arrays.\\ \hline \mbox{\tt in} & {\em npts} & the number of values to calculate.\\ \hline \mbox{\tt in} & {\em rho\+\_\+ref} & A reference density \mbox{[}kg m-\/3\mbox{]}. \\ \hline \end{DoxyParams} Definition at line 84 of file M\+O\+M\+\_\+\+E\+O\+S\+\_\+\+T\+E\+O\+S10.\+F90. \begin{DoxyCode} 84 \textcolor{keywordtype}{real}, \textcolor{keywordtype}{dimension(:)}, \textcolor{keywordtype}{intent(in)} :: T\textcolor{comment}{ !< Conservative temperature [degC].} 85 \textcolor{keywordtype}{real}, \textcolor{keywordtype}{dimension(:)}, \textcolor{keywordtype}{intent(in)} :: S\textcolor{comment}{ !< Absolute salinity [g kg-1]} 86 \textcolor{keywordtype}{real}, \textcolor{keywordtype}{dimension(:)}, \textcolor{keywordtype}{intent(in)} :: pressure\textcolor{comment}{ !< pressure [Pa].} 87 \textcolor{keywordtype}{real}, \textcolor{keywordtype}{dimension(:)}, \textcolor{keywordtype}{intent(out)} :: rho\textcolor{comment}{ !< in situ density [kg m-3].} 88 \textcolor{keywordtype}{integer}, \textcolor{keywordtype}{intent(in)} :: start\textcolor{comment}{ !< the starting point in the arrays.} 89 \textcolor{keywordtype}{integer}, \textcolor{keywordtype}{intent(in)} :: npts\textcolor{comment}{ !< the number of values to calculate.} 90 \textcolor{keywordtype}{real}, \textcolor{keywordtype}{optional}, \textcolor{keywordtype}{intent(in)} :: rho\_ref\textcolor{comment}{ !< A reference density [kg m-3].} 91 92 \textcolor{comment}{! Local variables} 93 \textcolor{keywordtype}{real} :: zs, zt, zp 94 \textcolor{keywordtype}{integer} :: j 95 96 \textcolor{keywordflow}{do} j=start,start+npts-1 97 \textcolor{comment}{!Conversions} 98 zs = s(j) \textcolor{comment}{!gsw\_sr\_from\_sp(S(j)) !Convert practical salinity to absolute salinity} 99 zt = t(j) \textcolor{comment}{!gsw\_ct\_from\_pt(S(j),T(j)) !Convert potantial temp to conservative temp} 100 zp = pressure(j)* pa2db \textcolor{comment}{!Convert pressure from Pascal to decibar} 101 102 \textcolor{keywordflow}{if} (s(j) < -1.0e-10) \textcolor{keywordflow}{then} \textcolor{comment}{!Can we assume safely that this is a missing value?} 103 rho(j) = 1000.0 104 \textcolor{keywordflow}{else} 105 rho(j) = gsw\_rho(zs,zt,zp) 106 \textcolor{keywordflow}{ endif} 107 \textcolor{keywordflow}{if} (\textcolor{keyword}{present}(rho\_ref)) rho(j) = rho(j) - rho\_ref 108 \textcolor{keywordflow}{ enddo} \end{DoxyCode} \mbox{\Hypertarget{interfacemom__eos__teos10_1_1calculate__density__teos10_a83d2f50d5a2bc0a2d4f95fcb02d0cbf5}\label{interfacemom__eos__teos10_1_1calculate__density__teos10_a83d2f50d5a2bc0a2d4f95fcb02d0cbf5}} \index{mom\+\_\+eos\+\_\+teos10\+::calculate\+\_\+density\+\_\+teos10@{mom\+\_\+eos\+\_\+teos10\+::calculate\+\_\+density\+\_\+teos10}!calculate\+\_\+density\+\_\+scalar\+\_\+teos10@{calculate\+\_\+density\+\_\+scalar\+\_\+teos10}} \index{calculate\+\_\+density\+\_\+scalar\+\_\+teos10@{calculate\+\_\+density\+\_\+scalar\+\_\+teos10}!mom\+\_\+eos\+\_\+teos10\+::calculate\+\_\+density\+\_\+teos10@{mom\+\_\+eos\+\_\+teos10\+::calculate\+\_\+density\+\_\+teos10}} \subsubsection{\texorpdfstring{calculate\+\_\+density\+\_\+scalar\+\_\+teos10()}{calculate\_density\_scalar\_teos10()}} {\footnotesize\ttfamily subroutine mom\+\_\+eos\+\_\+teos10\+::calculate\+\_\+density\+\_\+teos10\+::calculate\+\_\+density\+\_\+scalar\+\_\+teos10 (\begin{DoxyParamCaption}\item[{real, intent(in)}]{T, }\item[{real, intent(in)}]{S, }\item[{real, intent(in)}]{pressure, }\item[{real, intent(out)}]{rho, }\item[{real, intent(in), optional}]{rho\+\_\+ref }\end{DoxyParamCaption})\hspace{0.3cm}{\ttfamily [private]}} This subroutine computes the in situ density of sea water (rho in \mbox{[}kg m-\/3\mbox{]}) from absolute salinity (S \mbox{[}g kg-\/1\mbox{]}), conservative temperature (T \mbox{[}degC\mbox{]}), and pressure \mbox{[}Pa\mbox{]}. It uses the expression from the T\+E\+O\+S10 website. \begin{DoxyParams}[1]{Parameters} \mbox{\tt in} & {\em t} & Conservative temperature \mbox{[}degC\mbox{]}.\\ \hline \mbox{\tt in} & {\em s} & Absolute salinity \mbox{[}g kg-\/1\mbox{]}.\\ \hline \mbox{\tt in} & {\em pressure} & pressure \mbox{[}Pa\mbox{]}.\\ \hline \mbox{\tt out} & {\em rho} & In situ density \mbox{[}kg m-\/3\mbox{]}.\\ \hline \mbox{\tt in} & {\em rho\+\_\+ref} & A reference density \mbox{[}kg m-\/3\mbox{]}. \\ \hline \end{DoxyParams} Definition at line 60 of file M\+O\+M\+\_\+\+E\+O\+S\+\_\+\+T\+E\+O\+S10.\+F90. \begin{DoxyCode} 60 \textcolor{keywordtype}{real}, \textcolor{keywordtype}{intent(in)} :: T\textcolor{comment}{ !< Conservative temperature [degC].} 61 \textcolor{keywordtype}{real}, \textcolor{keywordtype}{intent(in)} :: S\textcolor{comment}{ !< Absolute salinity [g kg-1].} 62 \textcolor{keywordtype}{real}, \textcolor{keywordtype}{intent(in)} :: pressure\textcolor{comment}{ !< pressure [Pa].} 63 \textcolor{keywordtype}{real}, \textcolor{keywordtype}{intent(out)} :: rho\textcolor{comment}{ !< In situ density [kg m-3].} 64 \textcolor{keywordtype}{real}, \textcolor{keywordtype}{optional}, \textcolor{keywordtype}{intent(in)} :: rho\_ref\textcolor{comment}{ !< A reference density [kg m-3].} 65 66 \textcolor{comment}{! Local variables} 67 \textcolor{keywordtype}{real}, \textcolor{keywordtype}{dimension(1)} :: T0, S0, pressure0 68 \textcolor{keywordtype}{real}, \textcolor{keywordtype}{dimension(1)} :: rho0 69 70 t0(1) = t 71 s0(1) = s 72 pressure0(1) = pressure 73 74 \textcolor{keyword}{call }calculate\_density\_array\_teos10(t0, s0, pressure0, rho0, 1, 1, rho\_ref) 75 rho = rho0(1) 76 \end{DoxyCode} The documentation for this interface was generated from the following file\+:\begin{DoxyCompactItemize} \item /home/cermak/src/\+M\+O\+M6.\+devrob/src/equation\+\_\+of\+\_\+state/M\+O\+M\+\_\+\+E\+O\+S\+\_\+\+T\+E\+O\+S10.\+F90\end{DoxyCompactItemize}