Meso » Thu Feb 09, 2012 9:34 pm wrote:Meso wrote:Just watched the last couple hours of radar frames and that right mover. Just sat there for ages, then decided alright, thats it, im leaving. Lightning seemed to die as soon as it moved too. Wonder what the mechanics are behind something like that...
Hi Meso. One day l was watching a mesocyclone storm up in north central Queensland on national radar a few weeks ago and l had taken some snaps and marked the direction of cloud movement and noticed that this MESO had developed in the area of divergence where the cloud was splitting into two different directions
I have learnt that when an air mass diverges it creates a localized area of low pressure where the surrounding air in fills and probably creates quite an updraft
Hence a severe storm cell( of course dependent on the other factors for storm development)
of course you know this is not the only way severe storms are formed
This storm created a hook echo and winds of 173 km/hr at the surface
Now the Lang lang/pakenham storm yesterday had the same divergence pattern
See page 3 of this thread where l posted the cloud direction you can see the storm sat in the area of cloud divergence
with hook echo signature
Now as to why the storm was a right mover. I would suggest that the cloud flow and air stream flowing N/west to s/east was stronger and the storm was steered or dragged into this flow
I would imagine that is why you get storms spitting as they are in an area of divergence where on half goes left and the other goes right so to speak
Check it out yourself in the future and test this observation
Here is a diagram of the cloud flow and divergent area with the storm forming in the fork
As for the declining lightning, l would suggest that once the storm was pulled away from the fork it lost the added uplift from the low pressure area at the fork of the divergence, reducing the powerful convective forcing