CONCLUDING DISCUSSION
The development of isolated and intense storms within
the Australian environment is relatively common. Primarily known as 'pulse' storms, a
characteristic of such storms are their rapid development and ability to produce brief and
sometimes severe weather, including large hail, local severe winds, and even weak
tornadoes. Another characteristic and just as astonishing is their ability to decay or
collapse very rapidly. Such storms operate in what could be regarded as 'marginal'
conditions for storm activity, but despite this, can achieve severe proportions. The
Ingebyra storm appears to be a good example of an Australian pulse storm that may have
reached severe proportions.... developed rapidly and decayed abruptly.
From analysis of available
photographic coverage, radar returns and satellite imagery, and including other data it
appears the Ingebyra storm may have been triggered by a combination of forcing.
A...The arrival of a westward moving
sea breeze convergence line adding additional low level moisture,
B.. The geographical location of this
region providing a 'local ' hot spot of surface convection,
C..The additional arrival of a south
to southwest surge at about the time of convective triggering,
D.. also present was a larger scale
trough mechanism affecting much of inland New South Wales.
E.. The arrival of an upper trough
across the region near to the time of convection.
The analysis of this data and the
concluding discussion are the opinion of the author and I welcome the opinion or
discussion of all.
Clyve Herbert (ASWA Victoria) |