Zobrazeno 1 - 10
of 37
pro vyhledávání: '"Alexander F. Shchepetkin"'
Autor:
M. Jeroen Molemaker, James C. McWilliams, Lionel Renault, Annalisa Bracco, Roy Barkan, Jun Choi, Alexander F. Shchepetkin
Publikováno v:
Journal of Physical Oceanography. 47:2325-2346
Realistic, submesoscale-resolving numerical simulations are used to characterize the flow’s statistics and the geography of surface submesoscale currents in the northern Gulf of Mexico. This study examines the role of the Mississippi–Atchafalaya
Autor:
Alexander F. Shchepetkin, Jun Choi, Kaushik Srinivasan, Roy Barkan, Annalisa Bracco, James C. McWilliams, M. Jeroen Molemaker
Publikováno v:
Journal of Physical Oceanography. 47:2347-2360
This paper, the second of three, investigates submesoscale dynamics in the northern Gulf of Mexico under the influence of the Mississippi–Atchafalaya River system, using numerical simulations at 500-m horizontal resolution with climatological atmos
Autor:
Serena Illig, Alex Hall, James C. McWilliams, Lionel Renault, Alexander F. Shchepetkin, M. Jeroen Molemaker, Florian Lemarié, Dudley B. Chelton
Publikováno v:
Journal of Physical Oceanography
Journal of Physical Oceanography, American Meteorological Society, 2016, 46 (6), pp.1685-1704. ⟨10.1175/JPO-D-15-0232.1⟩
Journal of Physical Oceanography, 2016, 46 (6), pp.1685-1704. ⟨10.1175/JPO-D-15-0232.1⟩
Journal of Physical Oceanography, American Meteorological Society, 2016, 46 (6), pp.1685-1704. ⟨10.1175/JPO-D-15-0232.1⟩
Journal of Physical Oceanography, 2016, 46 (6), pp.1685-1704. ⟨10.1175/JPO-D-15-0232.1⟩
In this study, uncoupled and coupled ocean–atmosphere simulations are carried out for the California Upwelling System to assess the dynamic ocean–atmosphere interactions, namely, the ocean surface current feedback to the atmosphere. The authors s
Autor:
M. Jeroen Molemaker, Jonathan Gula, Lionel Renault, James C. McWilliams, Alexander F. Shchepetkin
Publikováno v:
Journal of Physical Oceanography. 45:1988-2005
A submesoscale filament of dense water in the oceanic surface layer can undergo frontogenesis with a secondary circulation that has a surface horizontal convergence and downwelling in its center. This occurs either because of the mesoscale straining
Autor:
Alexander F. Shchepetkin
Publikováno v:
Ocean Modelling. 91:38-69
An oceanic model with an Eulerian vertical coordinate and an explicit vertical advection scheme is subject to the Courant–Friedrichs–Lewy (CFL) limitation. Depending on the horizontal grid spacing, the horizontal-to-vertical grid resolution ratio
Autor:
Satoshi Mitarai, Yuichi Nakajima, Alexander F. Shchepetkin, Hiromi Watanabe, James C. McWilliams
Hydrothermal vent fields in the western Pacific Ocean are mostly distributed along spreading centers in submarine basins behind convergent plate boundaries. Larval dispersal resulting from deep-ocean circulations is one of the major factors influenci
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::76751dc7b1624c7dacd37622f3017d5b
https://europepmc.org/articles/PMC4801315/
https://europepmc.org/articles/PMC4801315/
Publikováno v:
Ocean Modelling
Ocean Modelling, 2012, 52-53, pp.9-35. ⟨10.1016/j.ocemod.2012.04.007⟩
Ocean Modelling, Elsevier, 2012, 52-53, pp.9-35. ⟨10.1016/j.ocemod.2012.04.007⟩
Ocean Modelling, 2012, 52-53, pp.9-35. ⟨10.1016/j.ocemod.2012.04.007⟩
Ocean Modelling, Elsevier, 2012, 52-53, pp.9-35. ⟨10.1016/j.ocemod.2012.04.007⟩
International audience; Ocean models usually rely on a tracer mixing operator which diffuses along isoneutral directions. This requirement is imposed by the highly adiabatic nature of the oceanic interior, and a numerical simulation needs to respect
Are there inescapable issues prohibiting the use of terrain-following coordinates in climate models?
Autor:
Alexander F. Shchepetkin, James C. McWilliams, M. Jeroen Molemaker, Florian Lemarié, François Colas, Jaison Kurian
Publikováno v:
Ocean Modelling
Ocean Modelling, 2011, 42, pp.57-79. ⟨10.1016/j.ocemod.2011.11.007⟩
Ocean Modelling, Elsevier, 2011, 42, pp.57-79. ⟨10.1016/j.ocemod.2011.11.007⟩
Ocean Modelling, 2011, 42, pp.57-79. ⟨10.1016/j.ocemod.2011.11.007⟩
Ocean Modelling, Elsevier, 2011, 42, pp.57-79. ⟨10.1016/j.ocemod.2011.11.007⟩
International audience; The use of $\sigma$-coordinate ocean models has historically been considered a disadvantage for large-scale climate studies. The main reason resides in the non-alignment of the vertical coordinate isosurfaces with either geopo
Publikováno v:
Ocean Modelling. 38:41-70
The Equation of State of seawater (EOS) relates in situ density to temperature, salinity and pressure. Most of the effort in the EOS-related literature is to ensure an accurate fit of density measurements under the conditions of different temperature
Autor:
Evan Mason, Jeroen Molemaker, Alexander F. Shchepetkin, Pablo Sangrà, François Colas, James C. McWilliams
Publikováno v:
Ocean Modelling. 35:1-15
One-way offline nesting of a primitive-equation regional ocean numerical model (ROMS) is investigated, with special attention to the boundary forcing file creation process. The model has a modified open boundary condition which minimises false wave r