Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Jean-Marc Verstraete"'
Autor:
Jean-Marc Verstraete
Publikováno v:
Progress in Oceanography. 29:1-60
Observational as well as numerical experiments show that Ekman divergence neither at the equator nor at the coast can explain a significant part of the annual upwelling in the Gulf of Guinea. The remote forcing theory is tested by analyzing both hist
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7896b1e3e24d85dfaecda8b64bd339ac
https://doi.org/10.1016/0079-6611(92)90002-h
https://doi.org/10.1016/0079-6611(92)90002-h
Publikováno v:
Progress in Oceanography
Progress in Oceanography, 1991, 27 (3-4), pp.273-340. ⟨10.1016/0079-6611(91)90027-J⟩
Progress in Oceanography, Elsevier, 1991, 27 (3-4), pp.273-340. ⟨10.1016/0079-6611(91)90027-J⟩
Progress in Oceanography, 1991, 27 (3-4), pp.273-340. ⟨10.1016/0079-6611(91)90027-J⟩
Progress in Oceanography, Elsevier, 1991, 27 (3-4), pp.273-340. ⟨10.1016/0079-6611(91)90027-J⟩
Isotherm vertical displacements within the thermocline and surface currents were investigated in the tropical Atlantic Ocean from 12°N to 12°S in 1982–1984, the period of the FOCAL-SEQUAL experiment. The study is based on a numerical simulation o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e235f59cd06ae36d727dee35e97f557e
https://doi.org/10.1016/0079-6611(91)90027-j
https://doi.org/10.1016/0079-6611(91)90027-j
Autor:
Jean-Marc Verstraete, John Vassie
Publikováno v:
Deep Sea Research Part A. Oceanographic Research Papers. 37:1-26
The vertical structures (relative to 500 dbar) of the equatorial pressure gradients, as well as the meridional pressure gradients at the equator in the Gulf of Guinea, were studied in response to the seasonal synoptic wind field from eight FOCAL (pro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::341c49ef3525c6c4a3823863e54b9141
https://doi.org/10.1016/0198-0149(90)90026-r
https://doi.org/10.1016/0198-0149(90)90026-r
Autor:
Julian P. McCreary, Jean-Marc Verstraete, Carl Wunsch, Dennis W. Moore, Joël Picaut, Jacques Merle, James J. O'Brien, Philippe Hisard
Publikováno v:
Geophysical Research Letters. 5:637-640
Observations suggest that the annual upwelling event in the Gulf of Guinea is not associated with changes in the local winds. A possible explanation is that a strong upwelling signal, generated by increased westward wind stress in the western Atlanti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::31d4b2fcbe06988f50b52e81bb9de7a1
https://doi.org/10.1029/gl005i008p00637
https://doi.org/10.1029/gl005i008p00637
Autor:
Jean Marc Verstraete, Joël Picaut
Publikováno v:
Journal of Physical Oceanography. 9:136-149
Long time series of sea level and sea surface temperatures measured at different coastal stations along the northern coast of the Gulf of Guinea are analyzed statistically. The results indicate that pronounced fortnightly oscillations in sea level ar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eeb4a3d7639dfb824b2dda06eaf82103
https://doi.org/10.1175/1520-0485(1979)009<0136:poadwa>2.0.co
https://doi.org/10.1175/1520-0485(1979)009<0136:poadwa>2.0.co
Publikováno v:
Nature. 322:245-247
For two years beginning in October 1982, oceanographic observations were made in the equatorial Atlantic to investigate the relationship between sea level, wind stress, sea surface slope (zonal pressure gradient, thermocline depth) and equatorial cur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::20424397cff2a68561a02d953e7a6c72
https://doi.org/10.1038/322245a0
https://doi.org/10.1038/322245a0
In order to investigate an extensive set of large-scale ocean-atmosphere events in the Guinea Gulf, we present the following time series: sea level, daily sea surface temperature at the coast, sea temperature at a thermistor chain mooring and atmosph
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::32f5d8387d10af04b3e359cdc8dbb09f
https://doi.org/10.1016/b978-1-4832-8366-1.50036-4
https://doi.org/10.1016/b978-1-4832-8366-1.50036-4
