So I've just read 111 posts in this amazing thread. Huge kudos to uniquorn and SimonF92 for analyzing and cracking the data of the mass balance buoys. I should have tracked the thread in real-time but my mind was elsewhere.
Before I turn to trying to analyze the data myself using the tools you have created, which surely will not be easy with my limited time and skills, I have one request right off the bat which I hope you can implement easily.
I consider the ice as some sort of capacitor, dampening the air temperature signal and integrating it on its way to the water interface. I can easily understand how the wild swings in the air signal are not immediately apparent when looking at the thickness growth curve. And I think there is an easy way of visualizing what goes on under the hood so to speak.
Add to the standardized thickness/temperature charts posted herein another temperature plot - that of the thermistor found 50cm below the upper ice surface, i.e. 50cm below the air or snow interface. Consider this the "core temp" of the ice. This variable is driven by the air temp above, and drives the thickening below, via a temp gradient through the ice. Later in the season this variable will rise above some threshold (is that -1.8o?) and will no longer be able to drive thickening, but will enable bottom melt instead.
Ideally I would add another plot, of the thermistor that is 100cm below the upper ice surface, as long as it is at least 20cm above the bottom ice surface (ice-water interface) to avoid noise and meaningless data. This would be the "deep core temp".
Looking at these two plots together with the air temp plot and the thickening rate will hopefully enable a visually intuitive understanding of the processes governing bottom freezing and bottom melt.
Later I hope to calculate season FDDs over the buoy and compare to the theoretical plots of ice thickening.
I also want to examine the effect of thick/thin/zero snow on the air temp to core temp coupling. Theoretically the effect should be quite strong.
I hope to find the date(s) on which thickening stops and bottom melting begins. I hope a rule of thumb will be found to enable estimating this date even when no buoy is available
And of course, to try and find ways to compare the buoy data to PIOMAS, SMOS/SMAP and even to the dubious DMI thickness map.
Big hopes...