Zobrazeno 1 - 10
of 27
pro vyhledávání: '"Navid C. Constantinou"'
Autor:
Simone Silvestri, Gregory L. Wagner, Jean‐Michel Campin, Navid C. Constantinou, Christopher N. Hill, Andre Souza, Raffaele Ferrari
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 16, Iss 7, Pp n/a-n/a (2024)
Abstract Current eddy‐permitting and eddy‐resolving ocean models require dissipation to prevent a spurious accumulation of enstrophy at the grid scale. We introduce a new numerical scheme for momentum advection in large‐scale ocean models that
Externí odkaz:
https://doaj.org/article/e3e10bb8d7504948a089af508a6e39c0
Autor:
Josué Martínez‐Moreno, Andrew McC. Hogg, Andrew E. Kiss, Navid C. Constantinou, Adele K. Morrison
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 11, Iss 10, Pp 3090-3105 (2019)
Abstract The mesoscale eddy field plays a key role in the mixing and transport of physical and biological properties and redistribution of energy in the ocean. Eddy kinetic energy is commonly defined as the kinetic energy of the time‐varying compon
Externí odkaz:
https://doaj.org/article/193b3a8594c64a5993fbd15483f9a77f
Studies of ocean surface transport often invoke the "Eulerian-mean hypothesis": that wave-agnostic general circulation models neglecting explicit surface waves effects simulate the Eulerian-mean ocean velocity time-averaged over surface wave oscillat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5d3bab120746eb028b04b805f33da362
http://arxiv.org/abs/2210.08552
http://arxiv.org/abs/2210.08552
Autor:
Navid C. Constantinou, Andrew McC. Hogg, Matthew H. England, Andrew E. Kiss, Adele K. Morrison, Josué Martínez-Moreno
Publikováno v:
Nature Climate Change. 11:397-403
Oceanic eddies play a profound role in mixing tracers such as heat, carbon, and nutrients, thereby regulating regional and global climate. Yet, it remains unclear how global oceanic eddy kinetic energy has evolved over the past few decades. Furthermo
Autor:
Andrew McC. Hogg, Thierry Penduff, Sally E. Close, William K. Dewar, Navid C Constantinou, Josué Martínez-Moreno
Publikováno v:
Journal Of Geophysical Research-oceans (2169-9275) (American Geophysical Union (AGU)), 2022-05, Vol. 127, N. 5, P. e2022JC018440 (12p.)
Journal of Geophysical Research. Oceans
Journal of Geophysical Research. Oceans, 2022, 127 (5), ⟨10.1029/2022JC018440⟩
Journal of Geophysical Research. Oceans
Journal of Geophysical Research. Oceans, 2022, 127 (5), ⟨10.1029/2022JC018440⟩
Circulation in the Southern Ocean is unique. The strong wind stress forcing and buoyancy fluxes, in concert with the lack of continental boundaries, conspire to drive the Antarctic Circumpolar Current replete with an intense eddy field. The effect of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c98a4c98128088cc9572ecdd7818d97c
https://archimer.ifremer.fr/doc/00768/88028/
https://archimer.ifremer.fr/doc/00768/88028/
Arctic icebergs, unconstrained sea ice floes, oil slicks, mangrove drifters, lost cargo containers, and other flotsam are known to move at 2-4% of the prevailing wind velocity relative to the water, despite vast differences in the material properties
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::90016605abe582329d34bd896dafb4e3
http://arxiv.org/abs/2201.12688
http://arxiv.org/abs/2201.12688
Autor:
Navid C. Constantinou
Παρουσιάζεται μία θεωρία που αναπτύχθηκε πρόσφατα για το σχηματισμό και την συντήρηση αεροχείμαρρων στις ατμόσφαιρες πλανητών. Η καινο
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0cca118dc281fea25715a5c9aaa9a34e
https://doi.org/10.12681/eadd/35501
https://doi.org/10.12681/eadd/35501
Publikováno v:
Journal of Fluid Mechanics
Despite the nonlinear nature of turbulence, there is evidence that part of the energy-transfer mechanisms sustaining wall turbulence can be ascribed to linear processes. The different scenarios stem from linear stability theory and comprise exponenti
Atmosphere and ocean are coupled via air–sea interactions. The atmospheric conditions fuel the ocean circulation and its variability, but the extent to which ocean processes can affect the atmosphere at decadal time scales remains unclear. In parti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::65a04576408edd67215390f975db4b8e