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\\  Central to any isotope representation of ET requires parameterisation of the resistance terms:  \begin{itemize}  \item soil resistance ($\r^s_s$) ($r^s_s$)  - \citet{Lee_2009} used a value 500 s.m^{-1}. This value comes from \citet{Shuttleworth_1990}, where they define values of 0-2000s.m^{-1} for wet (standing water) to dry soils. The value used by \citet{Lee_2009} is the preferred value for intermediary soils stated \citet{Shuttleworth_1990}. \item   \end{itemize}  \end{itemize}