Ok...after just typing most of a really nice post with some more details about this day, I was looking at more data and it (somehow) deleted everything I had types...ANNOYING! So I'll try again.
I decided to plough through some old GFS charts to see what the set up was like...so I loaded some data for the 22nd November 1968 and was a little confused....shear and instability wasn't that great...however...given that this memorial event (this weekend) went for 2 days I thought maybe the article had the date wrong. CORRECT! Macca: 1 vs ABC: 0. Of course this makes much more sense when looking at the data for the 23rd November 1968 (which was the Saturday).
The surface pattern on the 22nd showed a weak trough sitting across NE NSW and out into the Darling Downs and NW through the Maranoa & Warrego district with NE'lys feeding moisture into this trough. LI's were -2 to -3 (or thereabouts) on the 22nd and shear was enough to provide for some marginally severe storms across the region to the NE of the surface trough. 500mb temps on this day were around -9 to -10 across the whole region and winds at this level were healthy at 30-40knts.
However, on the day of interest (being the 23rd),a longwave upper trough was sliding across Bass Strait and the first of two little shortwave troughs moved over southern QLD overnight on the 22nd and a second moved into south central QLD on the afternoon of the 23rd. 500mb temps dropped from -9C to -11C by mid afternoon and with the pressure gradient at that level being quite strong, the mid level shear was very nice. In response to the second upper trough, the surface trough drifted westwards overnight on the 22nd to be lying across the western Darling Downs and down the western slopes of the NSW ranges and across the coast near Kempsey. A very warm airmass lay across much of QLD at the time with 850mb temps ranging from 20C along the southern border up to 27C through central QLD.
With moisture pumping into the trough overnight on the 22nd, DP's on the Darling Downs would've likely been in the mid-teens at least (not bad given the elevation). LI's in the area were around -4 to -5C and although this doesn't sound crazily unstable, the approaching upper trough and resultant lift generated from the diverging upper level winds were obviously enough for strong storms to develop.
Shear was pretty nice with the surface trough deepening as a result of the approaching upper level short wave trough. Surface analysis shows north to north easterly winds of 10-15knts which, after checking the 925mb winds which were the same at 15-20ktns, extended up a reasonable way (indicating moisture depth wasn't too bad). 850mb winds were NW'ly at 20-25knts and to prevent drying out, 850mb RH's were 45-50% which is not bad given the warm temperatures. 700mb winds were weak (around 20knts) anywhere north of about Kingaroy but down around the NSW/QLD border they were up to 35-40knts from the WNW. 500mb winds were very nice with a very tasty increase in speed shear hitting the Darling Downs in the afternoon of the 23rd with WNW'ly winds of 50-60knts. Sitting atop all of this was a very healthy 80knt+ jetstream.
Overall, conditions were pretty ripe for supercells (moreso closer to the coast given the better moisture) and with the moderate shear in the low levels and STRONG shear in the mid and upper levels, tornadoes were a distinct possibility - and unfortunately for the residents of Killarney, it was reality on the afternoon/evening of 23rd November 1968. I wouldn't be surprised to hear reports of other severe storms across northern NSW or SEQ on this day given the set up.
Macca