Hi Pete, yeah they were very slow moving cells thats for sure. Our vantage was good and quite elevated, however the distance to the storms was significant, possibly 70km's. Despite the distance we had a westerly view, hence the low sun provided some good back-lighting and contrast at times.
Below is a series of cropped and enhanced (contrast and gamma) photos that show the features of the storm that moved North through the areas west of Melbourne such as Ballan around 6-6.30 on Monday evening. (This storm followed behind a larger storm that was lightning active with visible CG's and a shelf cloud)
After the first storm had moved north and weakened John Allen and I had almost decided to leave the location when I noticed what appeared to be a VERY low cloud feature below a storm that could barely be made out through the hazy moisture-rich conditions out west. Within seconds it became clearer and was becoming more substantial even to the naked eye (despite the distance). We started taking photos straight away and discussed what the feature was but adding to the dilemma was the mid level cloud and anvil from the first storm that was blocking our view of the updraft towers connected to this new storm. At first I thought it was scud, then it looked way more substantial like a funnel, then I thought surely its only a shelf cloud feature. But over the next 10 minutes or so, the cloud base took on the appearance and behaviour of something more dynamic than a uni-directional shelfcloud. We saw funnel shaped lowerings of different sizes and shapes and several lowerings that appeared to be a wallcloud or wallclouds forming from scud. Based on the distance and several Qantas jets I captured in the foreground of my shots it can be said that the base features were certainly large.
Finally the mid level cloud cleared enough to show the towers above and there were multiple pulse updrafts with impressive pileus on each. One secondary overshoot was observed on one of the first pulses after several new pulses had already gone up behind it and John noted that there was obvious opposing flow through the low and mid levels and directional shear was probably quite good. The large lowering took on a cone shaped funnel appearance at this stage.
As this cone dissipated, several substantial and persistant semi-horizontal features (funnels?) became prominent and scud or the like appeared to be drawn in from right to left and it appeared a wallcloud was forming. You can see a Qantas jet landing at Tullamarine Airport in the foreground of one of the pics for some perspective.
By this stage the upper levels of the storm as well as the base were clearly in view and it was quite impressive - see the updrafts and the pileus below. Also note the opposing wind flow at different levels as indicated (approx).
The base feature (wallcloud?) persisted as the storm moved slowly north, grew in length (north-south) and then another funnel shape emerged from the base as can be seen below
We observed the updrafts had stopped pulsing and the storm weakened from this point before we were treated to some mammatus at sunset.
So there you go. Now I will check my video and if there is anything of note I will post some stills.
Brad.