Turbulent heat and momentum fluxes in the upper ocean under Arctic sea ice

• Published in: Journal of Geophysical Research: Oceans
• Main Authors: Peterson, Algot Kristoffer, Fer, Ilker, McPhee, Miles G., Randelhoff, Achim
• Format: Article in Journal/Newspaper
• Language: English
• Published: AGU Publications 2017
• Subjects: VDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452; VDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452; Arktis / Arctic; Turbulens / Turbulence; Arctic; Yermak Plateau; Arctic Basin; Arktis; Arktis*; Nansen Basin; Sea ice; Yermak plateau; Spitsbergen
• Online Access: https://hdl.handle.net/10037/11410; https://doi.org/10.1002/2016JC012283

Source at http://dx.doi.org/10.1002/2016JC012283 We report observations of heat and momentum fluxes measured in the ice-ocean boundary layer from four drift stations between January and June 2015, covering from the typical Arctic basin conditions in the Nansen Basin to energetic spots of interaction with the warm Atlantic Water branches near the Yermak Plateau and over the North Spitsbergen slope. A wide range of oceanic turbulent heat flux values are observed, reflecting the variations in space and time over the five month duration of the experiment. Oceanic heat flux is weakly positive in winter over the Nansen Basin during quiescent conditions, increasing by an order of magnitude during storm events. An event of local upwelling and mixing in the winter-time Nansen basin highlights the importance of individual events. Spring-time drift is confined to the Yermak Plateau and its slopes, where vertical mixing is enhanced. Wind events cause an approximate doubling of oceanic heat fluxes compared to calm periods. In June, melting conditions near the ice edge lead to heat fluxes of O(100 W m−2). The combination of wind forcing with shallow Atlantic Water layer and proximity to open waters leads to maximum heat fluxes reaching 367 W m−2, concurrent with rapid melting. Observed ocean-to-ice heat fluxes agree well with those estimated from a bulk parameterization except when accumulated freshwater from sea ice melt in spring probably causes the bulk formula to overestimate the oceanic heat flux.