Outcome:
This fizzed, obviously, except many places seem to have scored about 10 cm of snow on the tail, which is better than a kick in the guts. The Bureau of Meteorology’s excellent winterised automatic weather station at Perisher Valley saw it like this (at 1738 m; click for link):
![]() BOM Perisher Valley precipitation |
![]() BOM Perisher Valley temperature (red) and dew point |
So the ‘second wave’ system brought ample precipitation (that 40 mm!), but the cold I was anticipating, perhaps hoping for, arrived too late — about mid afternoon Friday. Two degrees Celsius is occasionally cold enough for snow in Australia, but not from a warm, wet lower atmosphere. It’s instructive to check the thickness and freezing level for Thursday; this from the US GFS model’s ‘analysis’ (model initialisation) at 10:00am local time, as plotted by Weather Online in the UK:
![]() GFS MSL pressure, 500 hPa geopotential height contours, and |
![]() GFS freezing level for Thursday morning, |
So the ACCESS-R prediction was a tiny bit out — the 500-1000 hPa atmospheric thickness over the alps looks to have been about 5460 m Thursday morning (the colour shading labelled ‘546’) rather than less than 5440 m. The freezing level was about 2000 m.
Not to labour the point, but the fusion temperature of water is immutable. From the point of view of snowfall, 1 °C too warm might as well be 10 °C. And for our marginal snow weather, a couple of degrees temperature increase will be pretty much enough to end it.
Update #4 (7 June):
Maybe this isn’t quite dead. BOM’s ACCESS-R is showing just about enough cold air around from early Thursday for mid level snow. It’s touch and go though, like so much of our snow weather. Why do people fail to notice how fragile it is.
![]() …And ECMWF via Levi Cowan |
![]() BOM ACCESS 200 hPa level (~12 km height) for Saturday |
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