Zobrazeno 1 - 10
of 226
pro vyhledávání: '"P. Marsaleix"'
Publikováno v:
Geoscientific Model Development, Vol 17, Pp 6967-6986 (2024)
The role of mixing between layers of different densities is key to how the ocean works and interacts with other components of the Earth's system. Correctly accounting for its effect in numerical simulations is therefore of utmost importance. However,
Externí odkaz:
https://doaj.org/article/5425dbdd442446f3a82a7d83e3728cab
Publikováno v:
Ocean Science, Vol 20, Pp 1013-1033 (2024)
Summer monsoon southwest wind induces the South Vietnam Upwelling (SVU) over four main areas along the southern and central Vietnamese coast: upwelling offshore of the Mekong shelf (MKU), along the southern and northern coasts (SCU and NCU), and offs
Externí odkaz:
https://doaj.org/article/53571ab4def0482c90f8a40f300ad945
Autor:
N. B. Trinh, M. Herrmann, C. Ulses, P. Marsaleix, T. Duhaut, T. To Duy, C. Estournel, R. K. Shearman
Publikováno v:
Geoscientific Model Development, Vol 17, Pp 1831-1867 (2024)
The South China Sea throughflow (SCSTF) connects the South China Sea (SCS) with neighboring seas and oceans, transferring surface water of the global thermohaline circulation between the Pacific and Indian oceans. A configuration of the SYMPHONIE oce
Externí odkaz:
https://doaj.org/article/61edd714385a490a9dc6e63ce8b89b18
Autor:
C. Ulses, C. Estournel, P. Marsaleix, K. Soetaert, M. Fourrier, L. Coppola, D. Lefèvre, F. Touratier, C. Goyet, V. Guglielmi, F. Kessouri, P. Testor, X. Durrieu de Madron
Publikováno v:
Biogeosciences, Vol 20, Pp 4683-4710 (2023)
Deep convection plays a key role in the circulation, thermodynamics, and biogeochemical cycles in the Mediterranean Sea, which is considered to be a hotspot of biodiversity and climate change. In the framework of the DEWEX (Dense Water Experiment) pr
Externí odkaz:
https://doaj.org/article/2abfa6599b494cb181bce5c95e13c58f
Autor:
J. Habib, C. Ulses, C. Estournel, M. Fakhri, P. Marsaleix, M. Pujo-Pay, M. Fourrier, L. Coppola, A. Mignot, L. Mortier, P. Conan
Publikováno v:
Biogeosciences, Vol 20, Pp 3203-3228 (2023)
The Rhodes Gyre is a cyclonic persistent feature of the general circulation of the Levantine Basin in the eastern Mediterranean Sea. Although it is located in the most oligotrophic basin of the Mediterranean Sea, it is a relatively high primary produ
Externí odkaz:
https://doaj.org/article/549c106fc55f4de39bee8ec574d87de0
Publikováno v:
Ocean Science, Vol 18, Pp 1131-1161 (2022)
The South Vietnam Upwelling (SVU) develops in the South China Sea (SCS) under the influence of southwest monsoon winds. To study the role of small spatiotemporal scales on the SVU functioning and variability, a simulation was performed over 2009–20
Externí odkaz:
https://doaj.org/article/e87838836baa4e948953073dbe780a6c
Publikováno v:
Biogeosciences, Vol 18, Pp 5513-5538 (2021)
The Gulf of Lion shelf (GoL, NW Mediterranean) is one of the most productive areas in the Mediterranean Sea. A 3D coupled hydrodynamic–biogeochemical model is used to study the mechanisms that drive the particulate organic carbon (POC) dynamics ove
Externí odkaz:
https://doaj.org/article/f36a49d51759473e98825bc6389c47c5
Publikováno v:
Biogeosciences, Vol 18, Pp 937-960 (2021)
The north-western Mediterranean deep convection plays a crucial role in the general circulation and biogeochemical cycles of the Mediterranean Sea. The DEWEX (DEnse Water EXperiment) project aimed to better understand this role through an intensive o
Externí odkaz:
https://doaj.org/article/15f9c784f6b1492f991c0a7551329d20
Publikováno v:
Geoscientific Model Development, Vol 13, Pp 1583-1607 (2020)
Consequences of tidal dynamics on hydro-sedimentary processes are a recurrent issue in estuarine and coastal processes studies, and accurate tidal solutions are a prerequisite for modeling sediment transport, especially in macro-tidal regions. The mo
Externí odkaz:
https://doaj.org/article/2eb204fabca64192bad33044eb68ecad
Publikováno v:
Ocean Science, Vol 15, Pp 179-198 (2019)
The North Balearic Front forms the southern branch of the cyclonic gyre in the northwestern Mediterranean Sea. Its dynamics exhibit significant seasonal variability. During autumn, the front spreads northward during the calm wind periods and rapidly
Externí odkaz:
https://doaj.org/article/07a457734c31465f94db6ac284cee99c