Holding on a large amount of captured CO2 (carbon sinks) and possibly ancient virus strains, permafrost heating could be a real danger and acceleration-trigger for climate change and biosphere extreme stress.
Permafrost, a thick subsurface layer of soil that remains below freezing point throughout the year (occurring chiefly in polar regions for two consecutive years), contain sandy soil as stated in different studies case (International Soil Reference and Information Centre).
Although exact percentage and distribution data about sandy soil is missing (at least by my side) some well known bacteria do reinforce binding links in sandy soil, see :
Strengthening sandy soils by microbial methods
Comparison of the Ability of Two Bacteria to Improve the Behavior of Sandy Soil
The idea here is to use and propagate these bacteria to strengthen geomechanics of permafrost's sandy soils — possibly along the first one mentioned aiming at elevating the albédo level.
Geomechanics involve mechanical state studies of the Earth's crust and its reaction processes under the influence of natural physical factors.
Moreover and lastly, thermal effects (rapid or punctual warming) do provoke cracks in the permafrost, later filled naturally with water and sand. From a geomechanical point of view, winning back stability in these critical structural points with bacteria acting on sand filled cracks, could be useful.