We have shown that areas of the ESAS affected by thermokarst [permafrost melting],
submerged taliks and some other processes could serve as migration pathways for methane to escape to the water column and further to the atmosphere.»
Not exact matches
Shakhova and Nicolsky believe that the development of open
taliks — unfrozen regions — in the permafrost at sites where thaw lakes and river palaeo valleys were
submerged is enabling methane to escape.