Not exact matches
The study was focused on a form of turbulence known as
mesoscale eddies,
ocean swirls on the scale of tens to hundreds of kilometers across that last anywhere from a month to a year.
«
Mesoscale eddies are on the scale of hundreds of kilometers across, yet the
ocean is only four kilometers deep, which makes them essentially two - dimensional.
Mesoscale eddies in the global
ocean work the same way.»
Giant swirling masses of seawater known as
mesoscale eddies roam the world's
oceans.
Ocean mesoscale eddies are the «weather» of the ocean, with typical horizontal scales of less than 100 km and timescales on the order of a m
Ocean mesoscale eddies are the «weather» of the
ocean, with typical horizontal scales of less than 100 km and timescales on the order of a m
ocean, with typical horizontal scales of less than 100 km and timescales on the order of a month.
Knowledge of dominant scales associated with
mesoscale eddies enables a better understanding of the resolution requirements for the Coupled Model Intercomparison Project, the framework used for comparison of global coupled
ocean - atmosphere general circulation models.
The scientists conducted
ocean simulations in an idealized mid-latitude ocean basin to Simulate Mesoscale Ocean Activity (SOMA) and eddy mi
ocean simulations in an idealized mid-latitude
ocean basin to Simulate Mesoscale Ocean Activity (SOMA) and eddy mi
ocean basin to Simulate
Mesoscale Ocean Activity (SOMA) and eddy mi
Ocean Activity (SOMA) and
eddy mixing.
Deep
ocean heat and carbon storage are dependent on heat transfers driven by
mesoscale eddy mixing.
Griffies, S. M., M. Winton, W. G. Anderson, R. Benson, T. L. Delworth, C. O. Dufour, J. P. Dunne, P. B. Goddard, A. K. Morrison, A. Rosati, A. T. Wittenberg, J. Yin, R. Zhang, 2014: Impacts on
ocean heat from transient
mesoscale eddies in a hierarchy of climate models.
The US CLIVAR / OCB Southern
Ocean Working Group was formed to identify critical observational targets and develop data / model metrics based on the currently available observational data, both physical and tracer, and the assimilative modeling (re) analyses, and evaluate and develop our understanding of the importance of
mesoscale eddies in the heat and carbon uptake and of the response of the Southern
Ocean to a changing climate, using high - resolution numerical studies and theory.
Incorporate
mesoscale eddy - resolving
ocean models more fully into the toolkit used for AMOC mechanisms / prediction work, including long coupled GCM simulations, in order to address questions about the role of turbulence in controlling AMOC.
We characterize impacts on heat in the
ocean climate system from transient
ocean mesoscale eddies.