Understanding of involved processes is poor partly because of lack of direct observations. During SWERUS-C3, the Arctic Clouds in Summer Experiment (ACSE) studied these processes in detail.
Thawing coastal and subsea permafrost and collapsing shallow methane hydrates could potentially add carbon dioxide and methane to the atmosphere this century, yet there is presently poor understanding of these systems and processes.
Geological sediment coring and geophysical mapping was done during Leg 2 of SWERUS-C3 in order to study the history of Arctic sea ice, methane release, past and present bottom temperatures and the conversion and transport of carbon from the East Siberian shelf to the deep sea.
SWERUS-C3, a multi-disciplinary international research program investigating the contemporary and historical functioning of the climate-cryosphere-carbon (C3) system of the East Siberian Arctic Ocean.