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The first-ever conductivity–temperature–depth (CTD) observations on the Wandel Sea shelf in northeastern Greenland were collected in\udApril–May 2015. They were complemented by CTDs taken along the continental\udslope during the Norwegian FRAM 2014–2015 drift. The CTD profiles are used\udto reveal the origin of water masses and interactions with ambient water from\udthe continental slope and the tidewater glacier outlet. The subsurface water\udis associated with the Pacific water outflow from the Arctic Ocean. The\udunderlying halocline separates the Pacific water from a deeper layer of polar water that has interacted with the warm Atlantic water outflow through the Fram\udStrait, recorded below 140 m. Over the outer shelf, the halocline shows\udnumerous cold density-compensated intrusions indicating lateral interaction\udwith an ambient polar water mass across the continental slope. At the front\udof the tidewater glacier outlet, colder and turbid water intrusions were\udobserved at the base of the halocline. On the temperature–salinity plots\udthese stations indicate a mixing line that is different from the ambient\udwater and seems to be conditioned by the ocean–glacier interaction. Our\udobservations of Pacific water are set within the context of upstream\udobservations in the Beaufort Sea and downstream observations from the\udNortheast Water Polynya, and clearly show the modification of Pacific water\udduring its advection across the Arctic Ocean. Moreover, ambient water over\udthe Wandel Sea slope shows different thermohaline structures indicating the\uddifferent origin and pathways of the on-shore and off-shore branches of the\udArctic Ocean outflow through the western Fram Strait

Arctic Ocean outflow and glacier–ocean interactions modify water over the Wandel Sea shelf (northeastern Greenland)