Russia's weekly ice chart:
-1st year ice taking over the Beaufort hole
- Laptev all frozen up (thin/nilas) except that famous polynya just off the shelf break
![](https://forum.arctic-sea-ice.net/proxy.php?request=http%3A%2F%2Fwww.aari.ru%2Fresources%2Fd0015%2Farctic%2Fgif.en%2F2021%2F20211026.gif&hash=8dd68d3798584d5ced951d64adf51ebc4c7be899)
If I may phrase the polynya question another way... with all the warm WSC water flowing underneath, why is the *gap* of shelf break in between Svaalbard and the Laptev Polynya still so frequently ice covered?
I observe that said ice usually doesn't form in-place, and typically ice that crosses that region is thinner on the way out than the way in. So the Laptev Polynya is somehow not the beneficiary of so much imported ice?
Perhaps... the Laptev Polynya needs its own thread. It would be a good reference in future.