Sentences with phrase «mesoscale ocean eddies»

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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 mOcean mesoscale eddies are the «weather» of the ocean, with typical horizontal scales of less than 100 km and timescales on the order of a mocean, 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 miocean simulations in an idealized mid-latitude ocean basin to Simulate Mesoscale Ocean Activity (SOMA) and eddy miocean basin to Simulate Mesoscale Ocean Activity (SOMA) and eddy miOcean 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.
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