My experience is from mountain(s) in more temperate climes (Mt. Rainier), but it seems to me an advancing glacier means more snow and has little to do with heat. The firn line can descend/ascend rather rapidly as more snow is added at the top even in an environment that is warming.
The leading edge of a glacier is of no real interest. The only thing that really counts is the firn line.
Petermann and Mt Rainier are both glaciers - but how different can two glaciers be ?
Mt Rainier, 25 glaciers sitting on a 14,000 foot active volcano with a volume of about 4.0 km3.
Petermann glacier is somewhat bigger, with an enormous catchment behind it containing ice up to over 2km thick.
I found a study from 2015 that used operation icebridge data to establish its complicated topography including bathymetry. Much too complex (for me) to try and summarise in a post.
(
https://www.sciencedirect.com/science/article/pii/S0012821X15002216 - "Bathymetry in Petermann fjord from Operation IceBridge aerogravity")
It looks like a sleeping(?) giant - I wonder if icebridge data since 2015 has identified significant change?
I guess the process by which Petermann and Mt Rainier will gain or (much more likely) lose mass is going to be very different.