Im just curious of your collective thoughts as to why is it that the east coast of Aus tends to generate a hell of a lot of lightning activity? It seems to occur as convection over Brisbane to Sydney, and off into the sea further south along polar fronts. I know the SST's are fairly high near the coast, but would this affect storms forming over the deserts? Can someone explain the conditions over that area, and why its so good for Cb formation? Or is it such a great location that even the TCu's produce good lightning? If so, why?
Also, in regards to the polar fronts, why is it that the similar fronts dont produce similar levels of lightning 15o of longitude nearer to us? Tasmania/NSW gets the good stuff
i think its:
warm sea temperatures
and different airmasses coliding...continental semi tropical and maritime semi tropical (i.e higher dew points and lower temperature than over the land)
and
the fact you get a venturi effect offering downwind of the east ausralian divide (strong upper level westerlies, and a strong surge up the eastern australian coastline of cooler air too (one the system deepens ) (same thing happens with storm enhancement east of Gisborne)
Also to add, diurnal convection over the sea at night will usually keep these storms firing and peaking just as the sun returns. Quite an impressive squall line there right now! It will most likely die within the next couple of hours.
so really they are just extremely lucky to get the tropical N-NNW from SE asia, combined with a dry desert like landmass supportive of nighttime cooling? does this promote development as far south as tasmania, or out in the southern tasman?
I recall living in Sydney seeing lightning out of just about any Cb cloud where as over Ak Cb clouds dont like producing lightning , Sydney having better surface conditions for convection resulting in more cloud hieght I guess.
You get airmass modification over continents, the mid level lapse rates steepen during the warm season due to warming in the lower layers. Add some moisture to this and you end up with big CAPE numbers. The more CAPE, the more pronounced the lightning activity.
sea surface temperature in the Tasman sea is still 19oC
but soil temperature over the land is now only 15oC
so that is one consideration
also though alot of the action moved SSE over the western waikato, northern taranaki, rotating around the low
hey , cool, a tornado was produced on that front last night...met service did have a severe thunderstorm watch out for the BOP, and a chance of tornadoes
I am not suprised they got one in that area when you look at the sat image animation, as it looks like a small low developed as it moved across the rotorua area...
ps, this should really be in the other thread about the NI weather event though....