deletions | additions       diff --git a/subsection_Melbourne_Melbourne_events_coincide__.tex b/subsection_Melbourne_Melbourne_events_coincide__.tex  index 713bce3..2f7636f 100644  --- a/subsection_Melbourne_Melbourne_events_coincide__.tex  +++ b/subsection_Melbourne_Melbourne_events_coincide__.tex 
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\subsection{Melbourne} \subsection{Site Summaries}  Melbourne events coincide with low pressure fronts and cut-off lows.  Using our filter on 675 profiles between 2004 and 2014 found 73 events transferring at least B(TODO) Ozone molecules(C\% of tropospheric column TODO). The seasonal distribution can be seen in panel two(clockwise) of figure \ref{fig:SummaryMelbourne}.  Tropopause height is generally 1km lower during an event, even though the majority of events occur in late summer, when the tropopause is higher(TODO: SOURCE). Macquarie events are more strongly associated with late Summer early Autumn(JFM), and the tropopause height is not different to the general Macquarie tropopause height.  Davis events are more evenly distributed.