Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Ryan P. Abernathey"'
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 16, Iss 8, Pp n/a-n/a (2024)
Abstract Atlantic time‐mean heat transport is northward at all latitudes and exhibits strong multidecadal variability between about 30°N and 55°N. Atlantic heat transport variability influences many aspects of the climate system, including region
Externí odkaz:
https://doaj.org/article/b2195c2578d64b71894f376bb3a691c2
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 15, Iss 4, Pp n/a-n/a (2023)
Abstract The Surface Water and Ocean Topography satellite will measure altimetry on scales down to about 15 km: at these scales, the sea‐surface‐height signature of inertia‐gravity waves, including barotropic tides and internal tides, will be v
Externí odkaz:
https://doaj.org/article/61ed93062f6848c7aa5b704739c48390
Autor:
Takaya Uchida, Dhruv Balwada, Ryan P. Abernathey, Galen A. McKinley, Shafer K. Smith, Marina Lévy
Publikováno v:
Nature Communications, Vol 11, Iss 1, Pp 1-8 (2020)
The Southern Ocean is an important sink of carbon via the biological pump. Here authors run high-resolution physical/biogeochemical simulations of an open-Southern Ocean ecosystem forced with a realistic seasonal cycle and confirm that (sub)mesoscale
Externí odkaz:
https://doaj.org/article/b2a6003fac1a456e9306c1a7ca47f68d
Autor:
Sjoerd Groeskamp, Paul M. Barker, Trevor J. McDougall, Ryan P. Abernathey, Stephen M. Griffies
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 11, Iss 7, Pp 1917-1939 (2019)
Abstract Mesoscale eddies stir along the neutral plane, and the resulting neutral diffusion is a fundamental aspect of subgrid‐scale tracer transport in ocean models. Calculating neutral diffusion traditionally involves calculating neutral slopes a
Externí odkaz:
https://doaj.org/article/8b8b3686037e427daceea0ec89b1a580
Publikováno v:
Journal of Physical Oceanography. 52:1677-1691
Oceanic mesoscale motions including eddies, meanders, fronts, and filaments comprise a dominant fraction of oceanic kinetic energy and contribute to the redistribution of tracers in the ocean such as heat, salt, and nutrients. This reservoir of mesos
Publikováno v:
eISSN
This study investigates the variability of water mass transformation (WMT) within the Weddell Gyre (WG). The WG serves as a pivotal site for the Meridional Overturning Circulation (MOC) and ocean ventilation because it is the primary origin of the la
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::61a1baa39ffe7b47e1e096ffbe15d7e4
https://doi.org/10.5194/egusphere-2022-129
https://doi.org/10.5194/egusphere-2022-129
Autor:
Takaya Uchida, Julien Le Sommer, Charles Stern, Ryan P. Abernathey, Chris Holdgraf, Aurélie Albert, Laurent Brodeau, Eric P. Chassignet, Xiaobiao Xu, Jonathan Gula, Guillaume Roullet, Nikolay Koldunov, Sergey Danilov, Qiang Wang, Dimitris Menemenlis, Clément Bricaud, Brian K. Arbic, Jay F. Shriver, Fangli Qiao, Bin Xiao, Arne Biastoch, René Schubert, Baylor Fox-Kemper, William K. Dewar, Alan Wallcraft
Publikováno v:
Geoscientific Model Development
Geoscientific Model Development, 2022, 15, pp.5829-5856. ⟨10.5194/gmd-15-5829-2022⟩
Geoscientific Model Development (1991-959X) (Copernicus GmbH), 2022-07, Vol. 15, N. 14, P. 5829-5856
EPIC3Geoscientific Model Development, 15(14), pp. 5829-5856, ISSN: 1991-9603
Geoscientific Model Development, 2022, 15, pp.5829-5856. ⟨10.5194/gmd-15-5829-2022⟩
Geoscientific Model Development (1991-959X) (Copernicus GmbH), 2022-07, Vol. 15, N. 14, P. 5829-5856
EPIC3Geoscientific Model Development, 15(14), pp. 5829-5856, ISSN: 1991-9603
With the increase in computational power, ocean models with kilometer-scale resolution have emerged over the last decade. These models have been used for quantifying the energetic exchanges between spatial scales, informing the design of eddy paramet
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aeac204ffa8bb8c52f0a692f70568400
https://hal-insu.archives-ouvertes.fr/insu-03779396
https://hal-insu.archives-ouvertes.fr/insu-03779396