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  • 11
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2003
    In:  Geophysical Research Letters Vol. 30, No. 10 ( 2003-05-15), p. n/a-n/a
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 30, No. 10 ( 2003-05-15), p. n/a-n/a
    Type of Medium: Online Resource
    ISSN: 0094-8276
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2003
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    SSG: 16,13
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  • 12
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2000
    In:  Journal of Geophysical Research: Oceans Vol. 105, No. C9 ( 2000-09-15), p. 21913-21925
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 105, No. C9 ( 2000-09-15), p. 21913-21925
    Abstract: All Agulhas rings that were spawned at the Agulhas retroflection between 1993 and 1996 (a total of 21 rings) have been monitored using TOPEX/Poseidon satellite altimetry and followed as they moved through the southeastern Atlantic Ocean, decayed, interacted with bottom topography and each other, or dissipated completely. Rings preferentially crossed the Walvis Ridge at its deepest parts. After having crossed this ridge they have lower translational speeds, and their decay rate decreases markedly. Half the decay of long‐lived rings takes place in the first 5 months of their lifetimes. In addition to the strong decay of rings in the Cape Basin, about one third of the observed rings do not seem to leave this region at all but totally disintegrate here. The interaction of rings with bottom topography, in particular with the Vema Seamount, is shown frequently to cause splitting of rings. This will enhance mixing of the rings' Indian Ocean water into that of the southern Atlantic. This localized mixing may well provide a considerable source of warm and salty Indian Ocean water into the Atlantic overturning circulation.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2000
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    SSG: 16,13
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  • 13
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2001
    In:  Geophysical Research Letters Vol. 28, No. 18 ( 2001-09-15), p. 3449-3452
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 28, No. 18 ( 2001-09-15), p. 3449-3452
    Abstract: Natal Pulses are intermittent, solitary meanders on the trajectory of the otherwise remarkably stable northern Agulhas Current. They play disparate roles in the process of inter‐ocean exchange. They have been thought to trigger the spawning of Agulhas Rings at the Agulhas Retroflection, but also to generate an upstream retroflection that prevents Agulhas water from reaching the inter‐ocean boundary. For the Natal Pulse to be such a control it has to extend to considerable depths. We present the first hard evidence that demonstrates that the Natal Pulse is indeed an inherent property of the Agulhas Current throughout its full depth. Our data comprise Eulerian current meter observations and Lagrangian float trajectories in combination with sea‐surface height and sea‐surface temperature data. The results reveal the trapping of water within the Natal Pulse, its southward advection at a phase speed of about 11–12 cm s −1 , and rotation periods of 6 days.
    Type of Medium: Online Resource
    ISSN: 0094-8276 , 1944-8007
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2001
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  • 14
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1999
    In:  Journal of Geophysical Research: Oceans Vol. 104, No. C9 ( 1999-09-15), p. 20987-21005
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 104, No. C9 ( 1999-09-15), p. 20987-21005
    Abstract: Hydrographic sections carried out in January‐March 1995 across the pathway of Agulhas rings in the Cape Basin are used for a brief description of the mesoscale thermohaline variability in this region and a detailed study of three rings that were identified in the data. The three eddies exhibited remarkably diverse dimensions, vertical structures, and water mass characteristics. One of them, R1, was located near the Agulhas retroflection, had a diameter of 200 km, a maximum azimuthal speed of 0.40 m s −1 , core oxygen values in excess of 260 μmol kg −1 and was characterized by a well‐developed thermostad of 11.6°C. A second ring, R2, at 31°30′S, 9°W, by contrast, had a diameter of about 500 km, a core temperature of 17.1°C, and azimuthal speeds of 0.50 m s −1 , suggesting a very different history. A third ring, R3, at 26°S, 9°W, although farthest north of the three, had characteristics similar to ring R1, but with a deeper thermostad. Satellite altimetric data allow one to infer the natural histories of these vortices. Ring Rl detached from the retroflection at the beginning of March 1994 and spent the whole of the subsequent winter south of 42°S. This could explain the estimated heat loss of 620 W m −2 . The two rings observed at 9°W were spawned as one feature in April 1993, but interaction with the Erica seamount split it into two eddies; R3 being stalled in the retroflection region for the winter, while R2 moved off rapidly into the South Atlantic, by contrast, retaining most of its heat. These histories account for the observed differences between the rings. They also demonstrate that the interaction of Agulhas rings with their environment, including ambient water masses, the overlying atmosphere, and the bottom topography, is critical to their eventual hydrographic characteristics and the manner in which they contribute to the transport of heat and salt from the Indian to the South Atlantic Ocean.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1999
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  • 15
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2008
    In:  Journal of Geophysical Research Vol. 113, No. C1 ( 2008-01-12)
    In: Journal of Geophysical Research, American Geophysical Union (AGU), Vol. 113, No. C1 ( 2008-01-12)
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2008
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    SSG: 16,13
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  • 16
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2008
    In:  Journal of Geophysical Research Vol. 113, No. C9 ( 2008-09-05)
    In: Journal of Geophysical Research, American Geophysical Union (AGU), Vol. 113, No. C9 ( 2008-09-05)
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2008
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    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
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    SSG: 16,13
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  • 17
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2006
    In:  Geophysical Research Letters Vol. 33, No. 24 ( 2006-12-21)
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 33, No. 24 ( 2006-12-21)
    Type of Medium: Online Resource
    ISSN: 0094-8276
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2006
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    SSG: 16,13
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  • 18
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2010
    In:  Journal of Geophysical Research Vol. 115, No. C3 ( 2010-03-02)
    In: Journal of Geophysical Research, American Geophysical Union (AGU), Vol. 115, No. C3 ( 2010-03-02)
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2010
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  • 19
    Online Resource
    Online Resource
    Informa UK Limited ; 1993
    In:  Transactions of the Royal Society of South Africa Vol. 48, No. 2 ( 1993-01), p. i-i
    In: Transactions of the Royal Society of South Africa, Informa UK Limited, Vol. 48, No. 2 ( 1993-01), p. i-i
    Type of Medium: Online Resource
    ISSN: 0035-919X , 2154-0098
    Language: English
    Publisher: Informa UK Limited
    Publication Date: 1993
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