We quite often see drivers having to cool their tyres down after a 'push lap'. This suggestes that something in the tyre structure is changing when the tyre gets too hot. I used a technique called 'Differential Scanning Calorimetry' (DSC) to look into this;
DSC looks at heat flow in a material - think of a kettle; energy is put into the water and the temperature goes up in relation to the energy input. However, at 100 deg C energy input does not increase the termperature, but is used to create a 'phase change' in the water as it goes from liquid to vapour.
The DSC instrument is able to detect phase changes very precisely.
The sample was heated from -80 to +250 deg C and cooled and then the process repeated again, the results were quite interesting;

At ~160 deg C there was a distinct phase change in the sample, but on the second cycle the phase change did not occur. However, if the sample was left to 'recover' for a period of time, the phase change came back.
The DSC does not provide any information about precisely what is changing, and I have not combined this with rheological measurements, but it was interesting that I was able to detect something which we observe on the track.
We don't see too much blistering this season, but I was able to look at decomposition temperature using the DSC.
Decomposition starts at ~260 deg C. This seems like a pretty high temperature for the compound to reach, but given the temperatures of the brakes under hard decelleration, it isn't out of the question.