Hi all,
Its an odd feeling (for me) to hear that some chasers in Victoria have bagged several tornadoes. First thoughts are "why the hell did I move to QLD...I have been here for 4 years (read: seasons) now and have not seen one and if I stayed in Vic I could've seen this". Second thoughts are "I should check the set up cause I can probably learn something".
I remember flicking through the GFS and MesoLaps charts on the day and thinking to myself in the morning "there should be some nice storms around today. Shear is decent, instability is nice, but there is no cap and it looks like the trough is going to surge eastwards as storms develop and push out some decent outflow". Also during the day, I kept an eye on radar given that my parents live in north central Vic. I remember thinking to myself "gee...this is nothing special...bit of a shame really" so I was quite surprised to hear reports of multiple tornadoes.
I also remember opening the forum to read the reports of the tornadoes and to see the pictures and saw Michael Bath's post with the GFS analysis charts. My thoughts..."Wow. The shear on those charts is pretty nice. Imagine what could've been had there been deep, isolated convection".
Then there was the detailed analysis from John and his discussion with Harald Richter. I found it odd, to say the least, that there was mention of low-topped supercells with tops of about 15,000ft which had produced multiple tornadoes - some things weren't adding up (apart from the fact that the Yarrawonga doppler is starting to reach the upper end of its range at about 100km).
Then there was the first few photos. Photos showing what look to be outflow features and cloud bases at or near 5000ft (pretty likely given the obs ahead of the storm/s was 33/16 as per several BoM AWS's in the vicinity). The whole adding up thing was getting more confusing.
With bases of 5000ft and tops ot 15,000ft that only leaves 10,000ft of actual updraft to generate strong enough rotation to spawn several tornadoes. Now I would think that this may only be possible in the case of some extreme updrafts. So...how unstable was it? Not *that* unstable. "Low CAPE" as per John's description. Could the stretching of the updraft come from extreme shear (as opposed to extreme instability)? Probably not. With bases of 5000ft (lets say 850mb) and tops of 15,000ft (lets say 500mb for ease and conservatism) and looking at the GFS analysis charts posted by MB, we have northerly winds of 30-35knts at 850mb and north westerly winds of 40-45knts at 500mb. So really only 10knts difference between the two - not a huge amount of stretching going on here from shear (speed). Note that directional shear isn't overly useful in these situations - more on that in a separate post if people want me to go into it.
So no extreme CAPE, no significant speed shear...so where is this coming from?
My thoughts after reviewing ALL of the posted photos, reports, obs and data in quite a bit of detail...
I believe this to have been an outflow event. With the strength of the winds in the lower and mid levels, it wouldn't take much to drag these winds to the surface and generate some strong outflow. Couple this with some decent moisture (by Victorian standards), and you have some nice lowish outflow features (as shown in the pictures). Push this outflow across some slightly variable terrain and you have great potential for gustnadoes.
I chased a similar event (slightly further north) back in November 2003 which saw some strong outflow winds of up to 100km/h kick off some gustnadoes which I estimate had winds of up to and possibly more than 140km/h. I watched one of these significant gustnadoes (dust up to 500m in the air) hit a single tree in a paddock and the tree was reduced to a mess of mangled stumps with the branches thrown 100m up in the air and they came down at least that distance away from where they were previously rooted. This gustnado persisted for approximately 2.5-3km (which didn't take long as it was moving at 80+km/h. Photos of the chase (not the gustnado - was driving at the time) here (base levels and lowerings not dissimilar to Brad/John's photos)...
http://macca.bsch.au.com/gallery2/v/Chase-Season-03-04/20031120/Whilst I don't doubt the claims of sizeable ground level rotation, what I beleive is that these were gustnadoes - and some pretty strong ones at that. The damage photos indicate winds of up to and probably in excess of 100km/h.
This shouldn't take anything away from Brad and John who had one of the best chases in Victoria in recent times. To get that close to a strong gustnado and to get photos and video AND do damage assessments and observations, etc is certainly highly impressive (and given the complete lack of decent storms up here in recent times, I'd take it for sure). I really hope that this doesn't discourage anyone from posting reports or thoughts on this forum as this is what it is all about - seeing, reporting, analysing and concluding. What is important about these events is that there is this significant level of post-event analysis done to ensure that the correct outcome is reached - and in this case, I think it has been.
Macca