Zobrazeno 1 - 10
of 47
pro vyhledávání: '"MIT General Circulation Model"'
Publikováno v:
Ocean Dynamics. 70:879-896
Vertical axes of mesoscale eddies with the coherent structure were observed to tilt southwestward significantly from the sea surface to bottom in the South China Sea. The dynamic mechanism for vertical tilting of eddies, however, is not well understo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2e03109eaaff26e7f8c5dfb918f685d4
https://doi.org/10.1007/s10236-020-01375-3
https://doi.org/10.1007/s10236-020-01375-3
Publikováno v:
Acta Oceanologica Sinica. 38:20-30
Numerical simulations based on a high-resolution three-dimensional MIT general circulation model (MITgcm) using realistic topography and tidal forcing are conducted to investigate the generation and propagation of the so-called type-a waves (large-am
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::01aefa17806b72fe9dc7c6c35b017a96
https://doi.org/10.1007/s13131-019-1495-2
https://doi.org/10.1007/s13131-019-1495-2
Publikováno v:
Coastal engineering journal. 61(4):520-534
Explosive cyclones formed in the northwest Pacific region can be categorized into three major types based on their evolution: Type-I cyclones develop over the Sea of Japan, Type-II are generated on the continent and move toward the Pacific Ocean, and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9b263ae785b3697edef3e9a1182eac68
http://hdl.handle.net/2115/80808
http://hdl.handle.net/2115/80808
Autor:
Bing Han, Carsten Eden
Publikováno v:
Ocean Dynamics. 69:1009-1022
Three-dimensional simulations of the M2 and K1 internal tides using the MIT General Circulation Model (MITgcm) configured for the Luzon Ridge are presented. The energetics of M2 and K1 internal tides are studied by analyzing the full barotropic and b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1942e6da2ac2247bcf778484acbea89e
https://doi.org/10.1007/s10236-019-01297-9
https://doi.org/10.1007/s10236-019-01297-9
Autor:
J. Thomas Farrar, Dimitris Menemenlis, Andrew F. Thompson, María del Mar Flexas, Patrice Klein, Hector S. Torres, Hong Zhang
Publikováno v:
Journal of Geophysical Research. Oceans
Journal Of Geophysical Research-oceans (2169-9275) (American Geophysical Union (AGU)), 2019-08, Vol. 124, N. 8, P. 5723-5746
Journal Of Geophysical Research-oceans (2169-9275) (American Geophysical Union (AGU)), 2019-08, Vol. 124, N. 8, P. 5723-5746
Estimates of the kinetic energy transfer from the wind to the ocean are often limited by the spatial and temporal resolution of surface currents and surface winds. Here we examine the wind work in a pair of global, very high‐resolution (1/48° and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::63f867b80e8c17666dba9dbdad664e83
https://doi.org/10.1029/2018jc014453
https://doi.org/10.1029/2018jc014453
Publikováno v:
Journal of Marine Systems. 194:66-80
Satellite observations reveal many mesoscale eddies in the West Pacific Ocean (WPO) that propagate westwards and eventually interact with the Kuroshio Current. Examination of global ocean and sea ice reanalysis data in years 2008–2015 suggests traj
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7a0d90a0dc08da5d5e645190e4c1b2b9
https://doi.org/10.1016/j.jmarsys.2019.02.009
https://doi.org/10.1016/j.jmarsys.2019.02.009
Publikováno v:
Journal of Marine Science and Engineering, Vol 9, Iss 703, p 703 (2021)
Journal of Marine Science and Engineering
Volume 9
Issue 7
Journal of Marine Science and Engineering
Volume 9
Issue 7
The impact of fortnightly stratification variability induced by tide–topography interaction on the generation of baroclinic tides in the Luzon Strait is numerically investigated using the MIT general circulation model. The simulation shows that adv
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2baa631ebe252b23ea068026404b7aff
https://www.mdpi.com/2077-1312/9/7/703
https://www.mdpi.com/2077-1312/9/7/703
Autor:
Mateus Carvalho, Shanon Reckinger, Thomas H. Gibson, Scott Reckinger, Fred Hohman, Theresa J. Morrison
Overflows in the ocean occur when dense water flows down a continental slope into less dense ambient water. It is important to study idealized and small-scale models, which allow for confidence and control of parameters. The work presented here is a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c6a750c8953d7c84b47bf6768ca845c4
Autor:
Maura Brunetti, Christian Vérard
Publikováno v:
Climate Dynamics, Vol. 50 (2018) pp. 4425-4436
Climate models are often affected by long-term drift that is revealed by the evolution of global variables such as the ocean temperature or the surface air temperature. This spurious trend reduces the fidelity to initial conditions and has a great in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5c1105694bfa8e049bee5443216c280f
https://doi.org/10.1007/s00382-017-3883-7
https://doi.org/10.1007/s00382-017-3883-7
Autor:
Chang Liu, Caixia Shao, Lianxin Zhang, Yuxin Zhao, Xiaoshuang Zhang, Xuefeng Zhang, Chaohui Sun
Publikováno v:
Advances in Meteorology, Vol 2017 (2017)
Observing System Simulation Experiments (OSSEs) have been conducted to evaluate the effect of Argo data assimilation on ocean reanalysis in the Pacific region. The “truth” is obtained from a 5-year model integration from 2003 to 2007 based on the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::dc497e183b8c9326f5fb106970e458df
https://doi.org/10.1155/2017/7314106
https://doi.org/10.1155/2017/7314106