IIRC the Himalayas are still being pushed up, as the indian plate pushes against Eurasia. That makes me wonder if the loss of ice will result in taller mountains, with less ice to grind the upwelling rock.
The ice grinding primarily happens at the base of glaciers, in valleys.
Above the bergschrund (the head of the glacier), erosion in high mountains is accelerated by freeze-thaw cycles. Temps above freezing obviously contribute to this. But even well below freezing ambient temps, exposed dark rock in sunlight can absorb enough energy to cause local thawing, which results in rockfall.
The ice grinding primarily happens at the base of glaciers, in valleys.
Above the bergschrund (the head of the glacier), erosion in high mountains is accelerated by freeze-thaw cycles. Temps above freezing obviously contribute to this. But even well below freezing ambient temps, exposed dark rock in sunlight can absorb enough energy to cause local thawing, which results in rockfall.