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  • 1
    Online Resource
    Online Resource
    Elsevier BV ; 1990
    In:  Deep Sea Research Part A. Oceanographic Research Papers Vol. 37, No. 7 ( 1990-7), p. 1075-1084
    In: Deep Sea Research Part A. Oceanographic Research Papers, Elsevier BV, Vol. 37, No. 7 ( 1990-7), p. 1075-1084
    Type of Medium: Online Resource
    ISSN: 0198-0149
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1990
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  • 2
    Online Resource
    Online Resource
    American Meteorological Society ; 1990
    In:  Journal of Atmospheric and Oceanic Technology Vol. 7, No. 4 ( 1990-08), p. 568-575
    In: Journal of Atmospheric and Oceanic Technology, American Meteorological Society, Vol. 7, No. 4 ( 1990-08), p. 568-575
    Type of Medium: Online Resource
    ISSN: 0739-0572 , 1520-0426
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 1990
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  • 3
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1990
    In:  Journal of Geophysical Research: Oceans Vol. 95, No. C3 ( 1990-03-15), p. 3015-3024
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 95, No. C3 ( 1990-03-15), p. 3015-3024
    Abstract: The applicability of satellite altimeter data for estimating zonal current variability at the equator is assessed using the meridionally differenced form of the geostrophic balance. Estimates of geostrophic zonal flow anomalies in the equatorial Pacific have been deduced from 17‐day collinear altimeter data during the first year of the Geosat Exact Repeat Mission, November 1986 to November 1987. Altimeter‐derived geostrophic estimates agree well with in situ zonal current variability. Comparison of low‐frequency, near‐surface zonal current observed from equatorial moorings at 165°E;, 140°W, and 110°W yield correlations of 0.83, 0.85, and 0.51, respectively, with a mean rms difference of 23 cm s −1 . The geostrophic currents were calculated from all available ascending and descending Geosat tracks within ±4.5° of longitude from each mooring site. The inclusion of up to 11 ascending and descending Geosat tracks within the 9° band for every 17‐day repeat effectively reduced the temporal sampling interval to 1.5 days at 165°E and 140°W. However, only ascending tracks were available at 110°W. Alongtrack sea surface heights were first smoothed using a combination of linear and nonlinear filters. The 6.8 km alongtrack spacing of the altimeter measurements provides sufficient resolution for the effective filtering of small‐scale meridional noise, both instrumental and oceanic. High‐frequency temporal variability, such as noise and ageostrophic motions, was suppressed with a 31‐day Hanning filter. Sea level and zonal velocity solutions from a tropical Pacific numerical model were used as proxy data sets in order to estimate errors induced into the geostrophic calculation by the Geosat space‐time sampling.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1990
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    detail.hit.zdb_id: 3094268-8
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    detail.hit.zdb_id: 3094181-7
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    detail.hit.zdb_id: 3094167-2
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    SSG: 16,13
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  • 4
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1994
    In:  Journal of Geophysical Research: Oceans Vol. 99, No. C12 ( 1994-12-15), p. 24725-24738
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 99, No. C12 ( 1994-12-15), p. 24725-24738
    Abstract: As part of the verification phase of the TOPEX/POSEIDON mission, 10‐day gridded fields of altimeter data derived from TOPEX geophysical data records are compared with 10‐day gridded fields of dynamic height derived from more than 60 moorings of the Tropical Ocean and Global Atmosphere‐Tropical Atmosphere Ocean (TOGA‐TAO) array in the equatorial Pacific Ocean. Access to TAO data in real time permits the first 500 days of the TOPEX/POSEIDON mission to be placed in the context of complementary, in situ measurements of surface winds, sea surface temperatures, and upper ocean thermal structure, as well as the time history of these variables prior to launch. Analysis of the space‐time structure in the TOPEX and TAO surface topography data indicates sea level variability primarily due to equatorial Kelvin wave activity generated by intense wind bursts west of the date line in association with the 1991–1993 El Niño. Cross correlations between the two data sets are generally 〉 0.7, with RMS differences 〈 4 cm. However, for reasons not fully understood, correlations drop to 〈 0.5 in certain regions off the equator in the eastern Pacific, and RMS differences can be 〉 5 cm north of the equator in the central and eastern Pacific.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1994
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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
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    detail.hit.zdb_id: 3094197-0
    SSG: 16,13
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  • 5
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1990
    In:  Journal of Geophysical Research: Oceans Vol. 95, No. C12 ( 1990-12-15), p. 22089-22101
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 95, No. C12 ( 1990-12-15), p. 22089-22101
    Abstract: Anomalous heat transport and storage during the 1982–1983 El Niño are investigated using a linear, multimode model forced by observed winds. Heat transport is decomposed into symmetric (about the equator) and antisymmetric components. The former was dominated by anomalous northward Ekman transport which represented an enhancement of the usual seasonal cycle. The latter involved both Ekman and geostrophic transports. Near‐equatorial wind anomalies forced Kelvin and Rossby waves usually associated with El Niño; together these waves set up antisymmetric, geostrophic transport which tended to oppose direct Ekman transport. Because the opposition was imperfect, there was net heat convergence which caused variations in heat content in bands of latitude centered on the equator. Within a fairly narrow band (±5°) heat content was anomalously high preceding El Niño and was depleted following the event. Equatorial heat content anomalies were largely compensated by opposing anomalies in low latitudes of the extraequatorial ocean so that variability over broader bands of latitude about the equator was relatively small. A sampling study employing the model suggests that observational evidence for a heat content variations over the region ±15° is an artifact arising from inadequate spatial resolution offered by the sea level measurement network.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1990
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    detail.hit.zdb_id: 3094104-0
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    detail.hit.zdb_id: 2403298-0
    detail.hit.zdb_id: 2016800-7
    detail.hit.zdb_id: 161666-3
    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
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  • 6
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1994
    In:  Journal of Geophysical Research: Oceans Vol. 99, No. C1 ( 1994-01-15), p. 963-979
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 99, No. C1 ( 1994-01-15), p. 963-979
    Abstract: Mooring measurements at 0°, 165°E, for the period November 1988 to August 1991 indicate that surface layer structure was characterized by two distinct climatic regimes associated with dramatic differences in large‐scale atmospheric and oceanic conditions. La Niña conditions existed from November 1988 to November 1989, during which time the easterly trades were strong, Ekman divergence and upwelling were pronounced, surface velocity was strongly westward, and rainfall was low. The surface layer was cold, salty and well mixed down to 100‐m depth, with density variations controlled primarily by temperature. In contrast, from November 1989 to August 1991, the zonal winds were on average westerly and punctuated by frequent westerly wind bursts, the surface currents reversed and flowed eastward in the upper 50 m, and rainfall was high. Compared to the La Niña period, the surface layer was warmer and fresher, and the density mixed layer was shallower than the isothermal layer owing to the presence of a 30‐m‐thick mean halocline (or barrier layer) between 55‐ and 85‐m depth. Moreover, density variations in the mixed layer were determined primarily by salinity. During the November 1988 to November 1989 La Niña period, variability in sea surface temperature was influenced by local upwelling and zonal advection. However, during November 1989 to August 1991, the presence of the barrier layer effectively prevented the entrainment of cooler, saltier water from the thermocline into the surface layer. Local air‐sea heat fluxes were therefore more likely to be prominent in the surface layer temperature balance. The barrier layer thickness, which varied with a dominant time scale of 12–25 days, appears to have been affected by variations in zonal advection of low‐salinity water past the mooring.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1994
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    detail.hit.zdb_id: 710256-2
    detail.hit.zdb_id: 2016804-4
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    detail.hit.zdb_id: 3094219-6
    detail.hit.zdb_id: 3094167-2
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    SSG: 16,13
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  • 7
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1990
    In:  Journal of Geophysical Research: Oceans Vol. 95, No. C1 ( 1990-01-15), p. 805-806
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 95, No. C1 ( 1990-01-15), p. 805-806
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1990
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    detail.hit.zdb_id: 161667-5
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    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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  • 8
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1990
    In:  Journal of Geophysical Research: Oceans Vol. 95, No. C8 ( 1990-08-15), p. 13195-13208
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 95, No. C8 ( 1990-08-15), p. 13195-13208
    Abstract: We examine variability in the eastern equatorial Pacific during 1986–1988 using conductivity‐temperature‐depth data, velocity and temperature data from equatorial moorings between 110°W and 140°W, and wind data from a basin scale zonal array of islands and moorings between 110°W and 165°E. The period studied coincides with the El Niño/Southern Oscillation (ENSO) event of 1986–1987 and a subsequent cold event in 1988. Weak warm sea surface temperature anomalies first appeared in the eastern equatorial Pacific in mid‐1986 and increased to 〉 1°C in September–November 1986 in association with a 30 cm s −1 weakening of the South Equatorial Current and a 20‐ to 40‐m depression of the thermocline. These warm anomalies lasted until early 1988, after which a large‐scale shoaling of the thermocline led to sea surface temperatures more than 3°C colder than climatology. Year‐to‐year fluctuations in the eastern Pacific were related primarily to zonal wind variations in the central and western Pacific. Westerly wind stress anomalies of 0.02–0.05 N m −2 were observed between 140°W and 165°E from the latter half of 1986 until the end of 1987; these were replaced by easterly wind anomalies of similar magnitude between 157°W and 165°E in 1988. Energetic intraseasonal fluctuations with periods of 2–3 months were also prominent in zonal current, temperature, and dynamic height time series. These fluctuations propagate eastward at approximately first baroclinic mode Kelvin wave phase speeds and are forced west of the date line by episodes of westerly winds. Extrema in several oceanic variables occurred in association with these waves, though their precise dynamical link to the ENSO cycle is unclear from our data. Sea surface temperature and thermocline depth anomalies at 0°, 110°W were less pronounced during the 1986–87 ENSO than during the 1982–1983 ENSO; the Equatorial Undercurrent, though weaker than normal in early 1987, did not disappear as it did in early 1983.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1990
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    detail.hit.zdb_id: 2016813-5
    detail.hit.zdb_id: 2016810-X
    detail.hit.zdb_id: 2403298-0
    detail.hit.zdb_id: 2016800-7
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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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  • 9
    Online Resource
    Online Resource
    American Meteorological Society ; 1994
    In:  Journal of Atmospheric and Oceanic Technology Vol. 11, No. 5 ( 1994-10), p. 1334-1349
    In: Journal of Atmospheric and Oceanic Technology, American Meteorological Society, Vol. 11, No. 5 ( 1994-10), p. 1334-1349
    Type of Medium: Online Resource
    ISSN: 0739-0572 , 1520-0426
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 1994
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    detail.hit.zdb_id: 48441-6
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  • 10
    Online Resource
    Online Resource
    American Meteorological Society ; 1990
    In:  Journal of Climate Vol. 3, No. 5 ( 1990-05), p. 509-521
    In: Journal of Climate, American Meteorological Society, Vol. 3, No. 5 ( 1990-05), p. 509-521
    Type of Medium: Online Resource
    ISSN: 0894-8755 , 1520-0442
    RVK:
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 1990
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    detail.hit.zdb_id: 2021723-7
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