The potential energy contained in gravity currents drives intense localized mixing, entrainment, and the circulation in the deep ocean. For the long-term goal of parameterizing gravity currents (see video below) in climate models, we need to understand different plume systems. In the first phase of the CRC, subproject T3 investigated energy transfers related to the Denmark Strait Overflow (DSO) plume, which is a key element of the global overturning’s northern limb. In this second phase, we investigate energy transfers associated with the Weddell Sea Bottom Water (WSBW) gravity current, which is part of the overturning’s southern limb and supplies the densest waters to the global ocean.
The energy transfers in the WSBW plume include processes that are missing in the DSO plume system: (1) they are more strongly influenced by the interaction with tides and tidally generated internal gravity waves (IGWs) and (2) they give rise to a feedback loop, in which energy fluxes from eddies created within the plume set the conditions for the dense water formation feeding the plume. Characterising energy transfers in such different types of plume systems will allow us to later combine the results from the first and second phase into a comprehensive parameterization for plume-induced mixing.
Video "Overflows easily explained":
Objectives of Phase 1
The gravity current immediately downstream of Denmark Strait is a known for rapid water mass transformation and vigorous mixing (see Figure 1); its current variability is dominated by eddies on timescales of 2–10 days. Using observational and numerical modeling efforts we aim to understand the pathways and processes by which kinetic energy is transferred from the mesoscale eddy field to dissipative turbulent scales within the Denmark Strain Overflow (DSO) plume.
Main results of Phase 1
Entrainment rates in the interfacial layer (separating plume and warmer ambient waters) were determined through the analysis of over 30 years of vertical profiles of temperature, salinity and horizontal velocity taken within 200 km downstream of the Denmark Strait sill. Flow type (high vs low transport flow) explains most of the variability in the entrainment rates but the area approximately 75 to 175 km downstream (light blue shading in the upper plot of Fig. 2) was identified as an entrainment hotspot related to high vertical shear in the interfacial layer. These results were corroborated with model simulations of the overflow, which showed that the largest energy transfers occurred in nearly the same downstream region (light blue shading in the lower plot of Fig. 2). Comparing model simulations with grid spacing (horizontal resolution) of 18, 9, 4, 2, and 1 km also implies that there is a convergence of energy transfers with higher resolution, as the computed transfers for the 1 and 2 km simulations display rather similar amplitudes with significantly larger values than those resulting from the 4 km simulation.
Mooring data collected in the DSO plume 120 km downstream of the Denmark Strait sill revealed that high (>1 m/s) plume velocities coincide with cyclonic eddying activity and low Richardson numbers (<0.25). Low Richardson numbers are a necessary condition for Kelvin-Helmholtz instabilities to occur, suggesting that the interplay of high plume velocities and cyclonic eddy activity provides favorable conditions for a downscale energy transfer toward turbulent mixing (Fig. 3).
The role of internal waves in the transfer of energy to turbulence in the DSO plume can be observed in consecutive conductivity-temperature-depth (CTD) casts (Fig. 4, top panels), which show the temporal evolution of overflow structure and dynamics. Internal wave energy (EIW) above the overflow (Fig. 4, bottom) was generally enhanced when the plume was thick and propagating slowly (Fig. 4, middle panels), and decreased when the plume thinned and flowed faster. Conversely, turbulent kinetic energy dissipation rates in the interfacial layer (IL) were highest when the overflow was thinner and velocities were high, most likely caused by shear-driven turbulent mixing. This suggests that when the overflow was thicker and less vertically sheared, relatively more large-scale mean kinetic energy was converted to internal wave energy than to shear driven dissipation. The source of the internal waves, and their role in transferring energy away from the overflow, cannot be determined by observations alone. Thus, modelling efforts will be used in the future to examine the generation and impact of internal waves on the overall energy of the DSO.
Objectives of Phase 2
In this second phase, we investigate energy transfers associated with the Weddell Sea Bottom Water (WSBW) gravity current, which is part of the overturning’s southern limb and supplies the densest waters to the global ocean.
Our main hypotheses are:
- Tides and topographic waves in the Weddell Sea contribute substantially to driving dense shelf water over the continental shelf break where it feeds the WSBW plume
- Both eddies and IGWs have first-order effects on energy conversions in the WSBW plume. Numerical models need to include these effects to realistically simulate the characteristics of the WSBW plume
- IGW-driven energy conversions in the plume substantially modify the feedback of eddy energy from the WSBW plume to the supply of Circumpolar Deep Water (CDW) to the shelf region, where dense water is formed
- The nonlinear IGWs generated near their critical latitude play an important role in energy transfers and mixing in the Weddell Sea
We address these hypotheses by analyses of new and historical observational data, accompanied by idealized and realistic model simulations that also take into account tides (see figures 1 & 2). Specific model configurations will be established in order to represent the topography and impact of mixing hot spots associated with enhanced turbulence in the WSBW plume. These simulations will also serve to study the performance of different parameterizations of eddy dissipation in both
high resolution grids and coarse grids used in climate modeling. The observations and model studies will contribute to understanding the energetics of mixing and plume dynamics.
To resolve or not to resolve?
I’m investigating effects of grid resolution on the modification of overflow and ocean energetics.
I am Deniz and I work on the T3 ‘Energy transfers in gravity plumes’ project as a PhD candidate at AWI. In particularly we are interested in the Denmark Strait Overflow (DSO) which is between Greenland and Iceland. This location is special because the DSO carries most of the dense and cold Arctic water entering the North Atlantic. Thus contributing to the deep southward flowing part of the Atlantic meridional overturning circulation.
As soon as the dense water on the sill starts descending, it undergoes a significant amount of mixing and entrainment of ambient water. By 200km downstream of the sill, volume and tracer properties of the overflow water are substantially modified due to combination of different processes. In our subproject we try to understand the interactions of all these different processes at different scales using observational and numerical modeling analysis.
It’s difficult to properly represent overflows in a global ocean model with the coarse resolution climate models generally have. For my part in this subproject, I use a general circulation model (MITgcm) in a regional setup with a 1year of simulation period. I’m investigating effects of grid resolution on the modification of overflow and ocean energetics. For this purpose I use 6 different horizontal resolutions ranging from eddy resolving (1km) to coarse resolution (36km). At the moment, I am analyzing the results from higher resolution simulations. Soon coarser resolutions will come into the picture and analysis of eddy parameterization schemes along with them. My research will contribute to a better understanding of consequences of lacking smaller scale processes and better representation of them in coarser models.
Energy transfers in gravity plumes
The next step will be connecting this mesoscale activity with high frequency variability and mixing parameters in the plume.
Hello everyone, my name is Stylianos Kritsotalakis and I am a PhD student in the subproject “Energy transfers in gravity plumes” at AWI/MARUM. The aim of the project is to understand the pathways and processes by which kinetic energy is transferred from the mesoscale eddy field to submesoscales and dissipative turbulent scales. Using observational and numerical modeling efforts the project focuses in tackling the above problem within the Denmark Strait Overflow plume.
I am working , primarily, with mooring data aquired ~120km downstream of the Denmark Strait in late summer 2018. I have identified the mesoscale field associated with the plume which consists of eddy pairs with opposing sense of rotation (Fig.1) and at the moment I am comparing these findings with the existing literature. The next step will be connecting this mesoscale activity with high frequency variability and mixing parameters in the plume.
Olbers, D., Pollmann, F., Patel, A. & Eden, C. (2023). A model of energy and spectral shape for the internal gravity wave field in the deep-sea – The parametric IDEMIX model. J. Phys.Oceanogr. 53(5), doi: https://doi.org/10.1175/JPO-D-22-0147.1.
Llanillo, P. J., Kanzow, T., Janout, M. A., & Rohardt, G. (2023). The deep-water plume in the northwestern Weddell Sea, Antarctica: Mean state, seasonal cycle and interannual variability influenced by climate modes. J. Geophys. Res. 128(2), e2022JC019375, doi: https://doi.org/10.1029/2022JC019375.
Moritz, M., Jochumsen, K., North, R. P., Quadfasel, D. & Valdimarsson, H. (2019). Mesoscale Eddies observed at the Denmark Strait sill. J. Geophys. Res.-Oceans, https://doi.org/10.1029/2019JC015273.
Liang, X., and Losch, M. (2018). On the effects of increased vertical mixing on the Arctic Ocean and sea ice. J. Geophys. Res.-Oceans.
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North, R. P., Jochumsen, K. & Moritz, M. (2018). Entrainment and Energy Transfer Variability Along the Descending Path of the Denmark Strait Overflow Plume. J. Geophys. Res.-Oceans, 123(4), 2795-2807, doi: https://doi.org/10.1002/2018JC013821.