Jacobshavn during the dark season in 16 Sentinel 1B images.
Another long animation of JH, this one from 2018.
What I found the most interesting when I watched these animations is how the whole terrain is flowing, and quite fast. It's not just the ice in the main channel.
Also of note is that the calving front has not moved since ~2013. I guess the flow is too fast, so that any calving is quickly replaced with new ice. The current front is in a narrow chokepoint, in order to recede further it needs a location where the channel widens, which is what brought about the retreat in the 2000s.
I do wonder if the forward speed has changed during the last decade with the static front.