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  • 1
    Online Resource
    Online Resource
    A comparison of coincidental time series of the ocean surface height by satellite altimeter, mooring, and inverted echo sounder
    American Geophysical Union (AGU) ; 1995
    In:  Journal of Geophysical Research: Oceans Vol. 100, No. C12 ( 1995-12-15), p. 25101-25108
    Details
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 100, No. C12 ( 1995-12-15), p. 25101-25108
    Abstract: Altimetric measurements of sea surface height at two locations in the western tropical Pacific Ocean are compared to estimates of the dynamic sea surface height computed from cotemporal surface‐to‐bottom temperature/salinity measurements on moorings and acoustic travel time measured by bottom‐moored inverted echo sounders. The results show statistically high correlation between the in situ measurements at periods greater than 5 days and between the altimeter and in situ measurements at periods greater than 20 days. The rms difference between any two modes of observation is consistently between 2 and 3 cm.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    URL: Article
    DOI: 10.1029/95JC01959
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1995
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    detail.hit.zdb_id: 2969341-X
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    detail.hit.zdb_id: 3094268-8
    detail.hit.zdb_id: 710256-2
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    detail.hit.zdb_id: 3094181-7
    detail.hit.zdb_id: 3094219-6
    detail.hit.zdb_id: 3094167-2
    detail.hit.zdb_id: 2220777-6
    detail.hit.zdb_id: 3094197-0
    SSG: 16,13
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  • 2
    Online Resource
    Online Resource
    A depth controlled tow system for hydrographic and current measurements with applications
    Elsevier BV ; 1979
    In:  Deep Sea Research Part A. Oceanographic Research Papers Vol. 26, No. 5 ( 1979-5), p. 579-596
    Details
    In: Deep Sea Research Part A. Oceanographic Research Papers, Elsevier BV, Vol. 26, No. 5 ( 1979-5), p. 579-596
    Type of Medium: Online Resource
    ISSN: 0198-0149
    URL: Article
    DOI: 10.1016/0198-0149(79)90098-0
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1979
    detail.hit.zdb_id: 2280519-9
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  • 3
    Online Resource
    Online Resource
    Further study of a front in the Sargasso Sea
    Stockholm University Press ; 1969
    In:  Tellus Vol. 21, No. 2 ( 1969-04), p. 259-269
    Details
    In: Tellus, Stockholm University Press, Vol. 21, No. 2 ( 1969-04), p. 259-269
    Type of Medium: Online Resource
    ISSN: 0040-2826 , 2153-3490
    URL: Issue
    URL: Article
    DOI: 10.1111/tus.1969.21.issue-2
    DOI: 10.1111/j.2153-3490.1969.tb00437.x
    Language: English
    Publisher: Stockholm University Press
    Publication Date: 1969
    detail.hit.zdb_id: 2576759-8
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  • 4
    Online Resource
    Online Resource
    Basin wide thermocline displacements along the equator of the Atlantic in 1983
    American Geophysical Union (AGU) ; 1984
    In:  Geophysical Research Letters Vol. 11, No. 8 ( 1984-08), p. 729-732
    Details
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 11, No. 8 ( 1984-08), p. 729-732
    Abstract: Observations from five inverted echo sounders deployed between 10°W and 38°30′W along the equator during the spring and summer of 1983 are presented. The annual development of the eastward acting zonal pressure gradient is described and related to the observed zonal wind stress. The minimum and maximum basin wide gradients are observed in mid‐April and in the latter part of July, respectively. The upwelling season in the Gulf of Guinea is identified at the easternmost sounder during May, June, and July. Pulses in thermocline displacement (first deepening, then shallowing) propagate eastward across the basin at speeds of 2.8 and 2.1 m s −1 . They arrive at 10°W at the onset and just after the cessation of the seasonal upwelling at that location. Their initialization is related to relaxation periods in the zonal wind. For four of the last five years, the time of the pulse preceding the upwelling is tentatively identified.
    Type of Medium: Online Resource
    ISSN: 0094-8276 , 1944-8007
    URL: Article
    DOI: 10.1029/GL011i008p00729
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1984
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    SSG: 16,13
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  • 5
    Online Resource
    Online Resource
    winds at St. Peter and St. Paul Rocks during the first sequal year
    American Geophysical Union (AGU) ; 1984
    In:  Geophysical Research Letters Vol. 11, No. 8 ( 1984-08), p. 715-718
    Details
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 11, No. 8 ( 1984-08), p. 715-718
    Abstract: Wind observations were obtained during the first nine months of the SEQUAL field program from a station maintained at St. Peter and St. Paul (SPP) rocks. Winds are very steady from May to November and very unsteady during April when the Intertropical Convergence Zone (ITCZ) crosses the site. Wind stress components are computed and comparison with 1979 data shows that the onset of the winds occurred one month earlier in 1983 but is of similar amplitude. The spectral analysis of the wind shows a significant increase in the variance for periods between 3‐5 days and 10‐15 days.
    Type of Medium: Online Resource
    ISSN: 0094-8276 , 1944-8007
    URL: Article
    DOI: 10.1029/GL011i008p00715
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1984
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    detail.hit.zdb_id: 7403-2
    SSG: 16,13
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  • 6
    Online Resource
    Online Resource
    Diffusion of the core of Mediterranean Water above the Mid-Atlantic Ridge crest
    Elsevier BV ; 1970
    In:  Deep Sea Research and Oceanographic Abstracts Vol. 17, No. 3 ( 1970-6), p. 611-625
    Details
    In: Deep Sea Research and Oceanographic Abstracts, Elsevier BV, Vol. 17, No. 3 ( 1970-6), p. 611-625
    Type of Medium: Online Resource
    ISSN: 0011-7471
    URL: Article
    DOI: 10.1016/0011-7471(70)90071-9
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1970
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    detail.hit.zdb_id: 426538-5
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  • 7
    Online Resource
    Online Resource
    Editorial
    American Meteorological Society ; 1993
    In:  Journal of Physical Oceanography Vol. 23, No. 1 ( 1993-01), p. 3-3
    Details
    In: Journal of Physical Oceanography, American Meteorological Society, Vol. 23, No. 1 ( 1993-01), p. 3-3
    Type of Medium: Online Resource
    ISSN: 0022-3670 , 1520-0485
    URL: Article
    DOI: 10.1175/1520-0485(1993)023〈0003:〉2.0.CO;2
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 1993
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    detail.hit.zdb_id: 184162-2
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  • 8
    Online Resource
    Online Resource
    Tow spectra from MODE
    American Geophysical Union (AGU) ; 1975
    In:  Journal of Geophysical Research Vol. 80, No. 9 ( 1975-03-20), p. 1163-1167
    Details
    In: Journal of Geophysical Research, American Geophysical Union (AGU), Vol. 80, No. 9 ( 1975-03-20), p. 1163-1167
    Type of Medium: Online Resource
    ISSN: 0148-0227
    URL: Article
    DOI: 10.1029/JC080i009p01163
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1975
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    detail.hit.zdb_id: 3094268-8
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    detail.hit.zdb_id: 2220777-6
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    SSG: 16,13
    Location Call Number Limitation Availability
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  • 9
    Online Resource
    Online Resource
    Equatorial Kelvin waves in the Atlantic
    American Geophysical Union (AGU) ; 1987
    In:  Journal of Geophysical Research: Oceans Vol. 92, No. C2 ( 1987-02-15), p. 1894-1898
    Details
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 92, No. C2 ( 1987-02-15), p. 1894-1898
    Abstract: Long‐term inverted echo sounder records along and north of the equator in the Atlantic are analyzed to show the dominance of equatorially trapped and eastward propagating disturbances with first baroclinic mode Kelvin wave characteristics in the frequency band of 10 −1 to 40 −1 (cycles day −1 ). Propagation speed is estimated as 2.35 ± 0.22 m s −1 along the equator from 34°W to 1°W. Coherence is present to 3°N but absent at 6°N (from mooring data) and 9°N. Coherence is shown with the zonal wind stress observed in midbasin, and it is suggested that the origin of the disturbance is not far from 40°W.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    URL: Article
    DOI: 10.1029/JC092iC02p01894
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1987
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    detail.hit.zdb_id: 161667-5
    detail.hit.zdb_id: 2969341-X
    detail.hit.zdb_id: 161665-1
    detail.hit.zdb_id: 3094268-8
    detail.hit.zdb_id: 710256-2
    detail.hit.zdb_id: 2016804-4
    detail.hit.zdb_id: 3094181-7
    detail.hit.zdb_id: 3094219-6
    detail.hit.zdb_id: 3094167-2
    detail.hit.zdb_id: 2220777-6
    detail.hit.zdb_id: 3094197-0
    SSG: 16,13
    Location Call Number Limitation Availability
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  • 10
    Online Resource
    Online Resource
    Effect of the Propagation of Internal Water Waves on Underwater Sound Transmission
    Acoustical Society of America (ASA) ; 1967
    In:  The Journal of the Acoustical Society of America Vol. 42, No. 1 ( 1967-07-01), p. 83-87
    Details
    In: The Journal of the Acoustical Society of America, Acoustical Society of America (ASA), Vol. 42, No. 1 ( 1967-07-01), p. 83-87
    Abstract: A numerical method of computing ray paths by geometric optics in a cylindrically homogeneous medium is outlined, and then applied in extending Lee's investigation of the disturbance to a high frequency sound field by an internal wave field [J. Acoust. Soc. Am. 33, 677–681 (1961)]. In particular, the changes in the ray paths as the wave field propagates between the source and the receiver are displayed on a cathode-ray tube. The resulting fluctuation in the sound intensity field due to the translation of the medium is computed in order to illustrate the signal variance caused by the phenomenon.
    Type of Medium: Online Resource
    ISSN: 0001-4966 , 1520-8524
    URL: Article
    DOI: 10.1121/1.1910579
    RVK:
    EQ 1000
    Language: English
    Publisher: Acoustical Society of America (ASA)
    Publication Date: 1967
    detail.hit.zdb_id: 1461063-2
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