Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Sean C. Kennan"'
Autor:
Sean C. Kennan, Pearn P. Niiler
Publikováno v:
Journal of Physical Oceanography. 33:2643-2656
Simultaneous moored temperature, salinity, velocity, and wind measurements from the equator at 157.5°E, during 10 May–21 December 1992, are combined with a no-stress-level boundary condition in the Equatorial Undercurrent core to estimate the tota
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4ee9a6830dae0ccc74cb8e8f21e2e075
https://doi.org/10.1175/1520-0485(2003)033<2643:teowfa>2.0.co
https://doi.org/10.1175/1520-0485(2003)033<2643:teowfa>2.0.co
Autor:
Pearn P. Niiler, Sean C. Kennan
Publikováno v:
Journal of Physical Oceanography. 33:2627-2642
A new method for diagnosing the zonal gradient of sea level on the equator from in situ data is proposed and validated using satellite altimetry. A no-turbulent-stress-level boundary condition in the Pacific Equatorial Undercurrent core constrains th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a81ab0f6cfca820bb136a0cf42e70a27
https://doi.org/10.1175/1520-0485(2003)033<2627:eslsot>2.0.co
https://doi.org/10.1175/1520-0485(2003)033<2627:eslsot>2.0.co
Autor:
Pierre Flament, Sean C. Kennan
Publikováno v:
Journal of Physical Oceanography. 30:2277-2301
An upper-ocean vortex associated with tropical instabilities was observed during fall 1990 at 140°W in the shear region between the Pacific South Equatorial Current and the North Equatorial Counter current. The velocity and thermohaline structures o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8f50f41e0d8d89f74ad26a38bd28bc00
https://doi.org/10.1175/1520-0485(2000)030<2277:ooativ>2.0.co
https://doi.org/10.1175/1520-0485(2000)030<2277:ooativ>2.0.co
Publikováno v:
Nature. 383:610-613
IN the equatorial Pacific Ocean, easterly trade winds and the Earth's rotation combine to drive surface currents away from the Equator, thereby causing cold nutrient-rich subsurface water to upwell. The front1 that forms between this upwelled water a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d125326460476a2a3149565e1c27d361
https://doi.org/10.1038/383610a0
https://doi.org/10.1038/383610a0
Autor:
Sean C. Kennan, Roger Lukas
Publikováno v:
Deep Sea Research Part II: Topical Studies in Oceanography. 43:215-241
The Hawaii Ocean Time-series (HOT) hydrographic observations at station ALOHA (22°45′N, 158°W) reveal that the region is sometimes the site of intrusive interleaving of different water types near the salinity minimum of the North Pacific Intermed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9ca46565401118d9328bb9bb44d9cfaf
https://doi.org/10.1016/0967-0645(95)00094-1
https://doi.org/10.1016/0967-0645(95)00094-1
Publikováno v:
Ocean Modelling
Ocean Modelling, 2011, 39 (1-2), pp.31-46. ⟨10.1016/j.ocemod.2011.04.011⟩
Ocean Modelling, Elsevier, 2011, 39 (1-2), pp.31-46. ⟨10.1016/j.ocemod.2011.04.011⟩
Ocean Modelling, 2011, 39 (1-2), pp.31-46. ⟨10.1016/j.ocemod.2011.04.011⟩
Ocean Modelling, Elsevier, 2011, 39 (1-2), pp.31-46. ⟨10.1016/j.ocemod.2011.04.011⟩
International audience; Submesoscale dynamics in tropical instability waves (TIWs) of the Pacific ocean are analyzed from nested numerical simulations of increasing resolution (36 km, 12 km, and 4 km). It is shown that numerical convergence, as deter
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1793ecf33b9aa258d87a9d07d2f5a11d
http://www.documentation.ird.fr/hor/fdi:010053741
http://www.documentation.ird.fr/hor/fdi:010053741
Autor:
Gurvan V. Madec, Christophe E. Menkès, Jérôme Vialard, Jean-Philippe Boulanger, Sean C. Kennan
Publikováno v:
Journal of Physical Oceanography
Journal of Physical Oceanography, American Meteorological Society, 2006, 36 (5), pp.847-865. ⟨10.1175/JPO2904.1⟩
Journal of Physical Oceanography, 2006, 36 (5), pp.847-865. ⟨10.1175/JPO2904.1⟩
Journal of Physical Oceanography, American Meteorological Society, 2006, 36 (5), pp.847-865. ⟨10.1175/JPO2904.1⟩
Journal of Physical Oceanography, 2006, 36 (5), pp.847-865. ⟨10.1175/JPO2904.1⟩
A numerical simulation is used to investigate the mixed layer heat balance of the tropical Pacific Ocean including the equatorial cold tongue and the region of vortices associated with tropical instability waves (TIWs). The study is motivated by a ne
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cb75da7f7c4473ca80dbfbe921c9b767
https://hal.archives-ouvertes.fr/hal-00124781
https://hal.archives-ouvertes.fr/hal-00124781
Autor:
Alain Morlière, Yves Montel, Emile Marchal, Benjamin Biessy, Yves Dandonneau, Sébastien Masson, Jacques Grelet, Gérard Eldin, Gisèle Champalbert, Alain Herbland, Pierre Flament, Cyril Moulin, Christophe E. Menkès, Anne Lebourges-Dhaussy, Sean C. Kennan
Publikováno v:
Geophysical Research Letters
Geophysical Research Letters, 2002, 29, pp.48-1-48-4. ⟨10.1029/2001GL014576⟩
Geophysical Research Letters, American Geophysical Union, 2002, 29, pp.48-1-48-4. ⟨10.1029/2001GL014576⟩
Geophysical Research Letters (0094-8276) (Amer Geophysical Union), 2002-06, Vol. 29, N. 11, P.
Geophysical Research Letters, 2002, 29, pp.48-1-48-4. ⟨10.1029/2001GL014576⟩
Geophysical Research Letters, American Geophysical Union, 2002, 29, pp.48-1-48-4. ⟨10.1029/2001GL014576⟩
Geophysical Research Letters (0094-8276) (Amer Geophysical Union), 2002-06, Vol. 29, N. 11, P.
International audience; The equatorial Pacific and Atlantic oceans exhibit remarkable meridional undulations in temperature and chlorophyll fronts visible from space over thousands of kilometers and often referred to as tropical instability waves. He
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b31cc177c31e3e32fe837dc2c7d8e98e
https://hal.science/hal-00770818
https://hal.science/hal-00770818
Autor:
Jerome Rothstein, Sean C. Kennan
Publikováno v:
Physics Today. 45:141-142
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a89ed06483c08914b21a30f696166f1d
https://doi.org/10.1063/1.2809856
https://doi.org/10.1063/1.2809856