Zobrazeno 1 - 10
of 22
pro vyhledávání: '"Michel Ollitrault"'
Publikováno v:
Journal of Geophysical Research: Oceans
Journal of Geophysical Research: Oceans, 2019, 124, pp.6270-6285. ⟨10.1029/2018JC014565⟩
Journal Of Geophysical Research-oceans (2169-9275) (Amer Geophysical Union), 2019-08, Vol. 124, N. 8, P. 6270-6285
Journal of Geophysical Research: Oceans, 2019, 124, pp.6270-6285. ⟨10.1029/2018JC014565⟩
Journal Of Geophysical Research-oceans (2169-9275) (Amer Geophysical Union), 2019-08, Vol. 124, N. 8, P. 6270-6285
A direct method is presented to obtain the meridional overturning and heat transport in oceanic basins from observations under the sole assumptions of geostrophy and hydrostatics. The method is made possible because of the rising Argo float displacem
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::acffa7378123b7ceb0810d878906cae5
https://hal-insu.archives-ouvertes.fr/insu-03683189
https://hal-insu.archives-ouvertes.fr/insu-03683189
Publikováno v:
Journal Of Physical Oceanography (0022-3670) (Amer Meteorological Soc), 2018-08, Vol. 48, N. 8, P. 1867-1883
Journal of Physical Oceanography
Journal of Physical Oceanography, American Meteorological Society, 2018, 48 (8), pp.1867-1883. ⟨10.1175/JPO-D-17-0272.1⟩
Journal of Physical Oceanography, 2018, 48 (8), pp.1867-1883. ⟨10.1175/JPO-D-17-0272.1⟩
Journal of Physical Oceanography
Journal of Physical Oceanography, American Meteorological Society, 2018, 48 (8), pp.1867-1883. ⟨10.1175/JPO-D-17-0272.1⟩
Journal of Physical Oceanography, 2018, 48 (8), pp.1867-1883. ⟨10.1175/JPO-D-17-0272.1⟩
The vertically integrated potential energy of an incompressible stratified fluid formulated in density coordinates can be simply written as a weighted vertical sum of the squares of the vertical displacements of density surfaces, a general expression
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::76ef407a73c3ee556adb8e21d1fa6e1f
https://archimer.ifremer.fr/doc/00464/57521/
https://archimer.ifremer.fr/doc/00464/57521/
Publikováno v:
Journal Of Physical Oceanography (0022-3670) (Amer Meteorological Soc), 2016-01, Vol. 46, N. 1, P. 255-273
The time-mean Argo float displacements and the World Ocean Atlas 2009 temperature–salinity climatology are used to obtain the total, top to bottom, mass transports. Outside of an equatorial band, the total transports are the sum of the vertical int
Publikováno v:
Journal of Physical Oceanography
Journal of Physical Oceanography, American Meteorological Society, 2017, 47 (7), pp.1569-1586. ⟨10.1175/JPO-D-16-0182.1⟩
Journal of Physical Oceanography, 2017, 47 (7), pp.1569-1586. ⟨10.1175/JPO-D-16-0182.1⟩
Journal Of Physical Oceanography (0022-3670) (Amer Meteorological Soc), 2017-07, Vol. 47, N. 7, P. 1569-1586
Journal of Physical Oceanography, American Meteorological Society, 2017, 47 (7), pp.1569-1586. ⟨10.1175/JPO-D-16-0182.1⟩
Journal of Physical Oceanography, 2017, 47 (7), pp.1569-1586. ⟨10.1175/JPO-D-16-0182.1⟩
Journal Of Physical Oceanography (0022-3670) (Amer Meteorological Soc), 2017-07, Vol. 47, N. 7, P. 1569-1586
The evolution and dispersion of intermediate water masses in the ocean interior is studied. To this purpose, an empirical statistical model of Lagrangian tracers at a constant depth level is developed. The model follows the transfer operator based on
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9a5cc3058921d83a3bf7df8d7d904c63
https://hal.archives-ouvertes.fr/hal-02355953
https://hal.archives-ouvertes.fr/hal-02355953
Autor:
David M. Fratantoni, Matthias Lankhorst, Philip L. Richardson, Uwe Send, Michel Ollitrault, Walter Zenk
Publikováno v:
Deep Sea Research Part I: Oceanographic Research Papers
Deep Sea Research Part I: Oceanographic Research Papers, Elsevier, 2009, 56 (10), pp.1615-1632. ⟨10.1016/j.dsr.2009.06.002⟩
Deep-Sea Research Part I-Oceanographic Research Papers, 56 . pp. 1615-1632.
Deep Sea Research Part I: Oceanographic Research Papers (0967-0637) (Elsevier), 2009-10, Vol. 56, N. 10, P. 1615-1632
Deep Sea Research Part I: Oceanographic Research Papers, Elsevier, 2009, 56 (10), pp.1615-1632. ⟨10.1016/j.dsr.2009.06.002⟩
Deep-Sea Research Part I-Oceanographic Research Papers, 56 . pp. 1615-1632.
Deep Sea Research Part I: Oceanographic Research Papers (0967-0637) (Elsevier), 2009-10, Vol. 56, N. 10, P. 1615-1632
A comprehensive analysis of velocity data from subsurface floats in the northwestern tropical Atlantic at two depth layers is presented: one representing the Antarctic Intermediate Water (AAIW, pressure range 600-1050dbar), the other the upper North
Publikováno v:
Journal of Physical Oceanography
Journal of Physical Oceanography, American Meteorological Society, 2002, 32 (7), pp.2020-2033. ⟨10.1175/1520-0485(2002)0322.0.CO;2⟩
Journal of Physical Oceanography, American Meteorological Society, 2002, 32 (7), pp.2020-2033. ⟨10.1175/1520-0485(2002)0322.0.CO;2⟩
International audience; Quasi-Lagrangian trajectories of 26 sound fixing and ranging (SOFAR) floats have been collected near a depth of 700 m in the Central North Atlantic between 1983 and 1989, aiming at studying the influence of the Mid-Atlantic ri
Autor:
Michel Ollitrault, Claudia Schmid, Philip L. Richardson, Walter Zenk, Olaf Boebel, Russ E. Davis, R. G. Peterson
Publikováno v:
Geophysical Research Letters, 26 . 21,3329-21,3332.
The subsurface oceanic circulation is an important part of the Earth climate system. Subsurface currents traditionally are inferred indirectly from distributions of temperature and dissolved substances, occasionally supplemented by current meter meas
Publikováno v:
Journal Of Physical Oceanography (0022-3670) (Amer Meteorological Soc), 2014-01, Vol. 44, N. 1, P. 384-409
Journal of Physical Oceanography
Journal of Physical Oceanography, American Meteorological Society, 2014, 44 (1), pp.384-409. ⟨10.1175/JPO-D-13-030.1⟩
Journal of Physical Oceanography
Journal of Physical Oceanography, American Meteorological Society, 2014, 44 (1), pp.384-409. ⟨10.1175/JPO-D-13-030.1⟩
The mean ocean circulation near 1000-m depth is estimated with 100-km resolution from the Argo float displacements collected before 1 January 2010. After a thorough validation, the 400 000 or so displacements found in the 950–1150 dbar layer and wi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bf2bceb2795ae668b763e656619c8b7f
https://archimer.ifremer.fr/doc/00174/28512/
https://archimer.ifremer.fr/doc/00174/28512/
Publikováno v:
Journal Of Atmospheric And Oceanic Technology (0739-0572) (Amer Meteorological Soc), 2013-04, Vol. 30, N. 4, P. 759-788
Journal of Atmospheric and Oceanic Technology
Journal of Atmospheric and Oceanic Technology, American Meteorological Society, 2013, 30, pp.759-788. ⟨10.1175/JTECH-D-12-00073.1⟩
Journal of Atmospheric and Oceanic Technology
Journal of Atmospheric and Oceanic Technology, American Meteorological Society, 2013, 30, pp.759-788. ⟨10.1175/JTECH-D-12-00073.1⟩
During the first decade of the twenty-first century, more than 6000 Argo floats have been launched over the World Ocean, gathering temperature and salinity data from the upper 2000 m, at a 10-day or so sampling period. Meanwhile their deep displaceme
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::37f27a9caab904dd59e96f912d573bf7
https://archimer.ifremer.fr/doc/00138/24901/
https://archimer.ifremer.fr/doc/00138/24901/
Publikováno v:
Deep Sea Research Part II: Topical Studies in Oceanography
Deep Sea Research Part II: Topical Studies in Oceanography, Elsevier, 2013, 85, pp.109-126. ⟨10.1016/j.dsr2.2012.07.028⟩
Deep-sea Research Part Ii-topical Studies In Oceanography (0967-0645) (Pergamon-elsevier Science Ltd), 2013-01, Vol. 85, P. 109-126
Deep Sea Research Part II: Topical Studies in Oceanography, Elsevier, 2013, 85, pp.109-126. ⟨10.1016/j.dsr2.2012.07.028⟩
Deep-sea Research Part Ii-topical Studies In Oceanography (0967-0645) (Pergamon-elsevier Science Ltd), 2013-01, Vol. 85, P. 109-126
Subsurface float measurements at 800 m depth carried out from 1994 to 2003 in the Brazil Basin are used to characterise the equatorward Intermediate Western Boundary Current (IWBC) and its connections to the ocean interior. Transversally, the boundar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::82aaa0ccb76cec678101fa84c911fa21
https://hal.archives-ouvertes.fr/hal-00852163
https://hal.archives-ouvertes.fr/hal-00852163