Diapycnal nutrient mixing

• Main Authors: van Haren, Hans, Brussaard, Corina, Gerringa, Loes, van Manen, Mathijs, Middag, Rob, Groenewegen, Ruud
• Other Authors: loes gerringa, NIOZ Royal Netherlands Institute for Sea Research in cooperation with Utrecht University
• Language: unknown
• Published: NIOZ 2021
• Subjects: Earth and Environmental Sciences; stratification; vertical exchange; NE Atlantic Ocean; nutrients; dissolved Fe; Nutrient fluxes; Photic zone; Yoyo; Northeast Atlantic
• Online Access: https://doi.org/10.25850/nioz/7b.b.lb

In this data file nutrient, DFe and raw CTD data are available used for the paper "Diapycnal mixing across the photic zone of the NE-Atlantic". Variable physical conditions such as vertical turbulent exchange, internal wave and mesoscale eddy action, affect the availability of light and nutrients for phytoplankton (unicellular algae) growth. It is hypothesized that changes in ocean temperature may affect ocean vertical density stratification, which may hamper vertical exchange. In order to quantify variations in physical conditions in the Northeast Atlantic Ocean, we sampled a latitudinal transect along 17 degrees 5minutes W between 30 and 63 degrees N in summer. A shipborne Conductivity-Temperature-Depth CTD-instrumented package was used with a custom-made modification of the pump-inlet to minimize detrimental effects of ship motions on its data. Thorpe-scale analysis was used to establish turbulence values for the upper 500 m from 3 to 6 profiles obtained in a short CTD-yoyo, 3 to 5 h after local sunrise. From south to north, average temperature decreased together with stratification while turbulence values weakly increased or remained constant. Vertical turbulent nutrient fluxes did not vary significantly with stratification and latitude. This apparent lack of correspondence between turbulent mixing and temperature is likely due to internal waves breaking (increased stratification can support more internal waves), acting as a potential feed-back mechanism. As this feed-back mechanism mediates potential physical environment changes in temperature, global surface ocean warming may not affect the vertical nutrient fluxes to a large degree. We urge modelers to test this deduction as it could imply that the future summer phytoplankton productivity in stratified oligotrophic waters would experience little alterations in nutrient input from deeper waters.