After passing the Fram Strait, the warm Atlantic inflow to the Arctic Ocean flows counter-clockwise along the rim of the basins. This warm boundary current looses mass and heat to the interior, so that a warm layer of Atlantic Water is found all across the Arctic at about 300-800 meter depth. Through DAMOCLES and the U.S. NABOS experiment, the boundary current will be monitored at about 5 longitudes, the first one being north of Spitsbergen (at 32°E), which, together with the Fram Strait mooring array, is intended to monitor the inflow of heat to the Arctic proper (the Fram Strait alone monitors a substantial amount of recirculation). In DAMOCLES, one mooring will be deployed at this site, and we seek in this proposal to extent the array with one mooring more, for completeness.