EGU25-16401, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-16401
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Friday, 02 May, 10:05–10:15 (CEST)
 
Room 1.34
Dynamics of Near-Bottom Currents in Cold-Water Coral and Sponge Areas along the Walvis Ridge.
Christian Mohn1, Franziska U. Schwarzkopf2, Patricia Jiménez García3, Covadonga Orejas4, Veerle A.I. Huvenne5, Mia Schumacher6, Irene Pérez-Rodríguez7, Roberto Sarralde Vizuete8, Luis J. López-Abellán9, Andrew C. Dale10, Colin Devey11, Jørgen L.S. Hansen12, Eva Friis Møller13, and Arne Biastoch14
Christian Mohn et al.
  • 1Hanse-Wissenschaftskolleg – Institute for Advanced Study (HWK), Lehmkuhlenbusch 4, 27753 Delmenhorst, Germany
  • 2GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany
  • 3Tragsatec, Balearic Islands, Spain
  • 4Centro Oceanográfico de Gijón, Instituto Español de Oceanografía, IEO-CSIC, Spain
  • 5Ocean BioGeosciences, National Oceanography Centre, Southampton, UK (NOC)
  • 6GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany
  • 7Centro Oceanográfico de Vigo, Instituto Español de Oceanografía, IEO-CSIC, Spain
  • 8Centro Oceanográfico de Vigo, Instituto Español de Oceanografía, IEO-CSIC, Spain
  • 9Centro Oceanográfico de Canarias, Instituto Español de Oceanografía, IEO-CSIC, Spain
  • 10Scottish Association for Marine Science, Oban, United Kingdom
  • 11GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany
  • 12Aarhus University, Department of Ecoscience, Denmark
  • 13Aarhus University, Department of Ecoscience, Denmark
  • 14Kiel University, Kiel, Germany

Cold-water corals and sponges form iconic and globally occurring benthic communities, provide important habitats for a diverse associated fauna and thrive in environmental conditions with often large temporal and spatial variations in near-bottom currents, food availability and other environmental parameters. We investigate the variability of near‐bottom currents and physical processes from simulations with a nested hydrodynamic modelling framework at two seamounts rich in benthic fauna along the Northeast Walvis Ridge, Valdivia Bank and Ewing Seamount. Our aim is to obtain new insights on physical drivers of observed occurrences and distribution of benthic suspension feeders (cnidarians and sponges) in this data‐poor area. We use dynamic downscaling of high-resolution implementations of the ROMS-AGRIF model in combination with high-resolution bathymetry and open boundary forcing from the basin-scale model INALT20 and the OSU inverse tidal model to explore the fine-scale physical processes and mechanisms that potentially drive a continuous or episodic food supply to the benthic communities.  Over a three-year period, we analysed how near-bottom currents vary in space and time and assess potential connections between the distribution of filter-feeding fauna and the surrounding physical marine environment. We identified a close link between flow dynamics, internal tide dynamics and faunal species distributions. We propose that physical processes such as kinetic energy dissipation and internal wave dynamics could serve as functional indicators of food supply and particle encounter rates in future species distribution and habitat suitability models for important deep-sea taxa, such as those that represent vulnerable marine ecosystems. Our results also show little impact of mesoscale eddies from the Agulhas Leakage as they propagate north-westward into the southeast Atlantic along a well-defined corridor, which only occasionally extends as far north as the Valdivia Bank and Ewing Seamount.

How to cite: Mohn, C., Schwarzkopf, F. U., Jiménez García, P., Orejas, C., Huvenne, V. A. I., Schumacher, M., Pérez-Rodríguez, I., Sarralde Vizuete, R., López-Abellán, L. J., Dale, A. C., Devey, C., Hansen, J. L. S., Møller, E. F., and Biastoch, A.: Dynamics of Near-Bottom Currents in Cold-Water Coral and Sponge Areas along the Walvis Ridge., EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-16401, https://doi.org/10.5194/egusphere-egu25-16401, 2025.