deletions | additions       diff --git a/textbf_Methodology_At_Melbourne_and__.tex b/textbf_Methodology_At_Melbourne_and__.tex  index 35bdf12..dba86fc 100644  --- a/textbf_Methodology_At_Melbourne_and__.tex  +++ b/textbf_Methodology_At_Melbourne_and__.tex 
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\item For Giles \textbf{37} between 23-00UTC, \textbf{117} between 11-12UTC (though no soundings at this time).  \end{itemize}  \textbf{Thoughts and Actions}  \textit{What analysis can I use if Era Int doesn't identify ETS in soundings?}  \textit{Question - Can I use existing Era Int 850hPa Fronts dataset?}  \begin{itemize}  \item Colman 1990a implied ETS existed above very shallow surface inversions well below 850hPa, and in 1990b below ~970hPa. Browning et al 2010 observed the depth of surface inversion to 900hPa where convective initiation occurred above.