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  • 11
    Online-Ressource
    Online-Ressource
    American Meteorological Society ; 2009
    In:  Journal of Climate Vol. 22, No. 2 ( 2009-01-15), p. 285-299
    In: Journal of Climate, American Meteorological Society, Vol. 22, No. 2 ( 2009-01-15), p. 285-299
    Kurzfassung: Measurements from three long-term moored buoys are used to investigate the impact of barrier layer thickness (BLT) on the seasonal cycle of sea surface temperature (SST) in the central tropical North Atlantic Ocean. It is found that seasonal variations of the BLT exert a considerable influence on SST through their modulation of the vertical heat flux at the base of the mixed layer, estimated as the residual in the mixed layer heat balance. Cooling associated with this term is strongest when the barrier layer is thin and the vertical temperature gradient at the base of the mixed layer is strong. Conversely, thick barrier layers are associated with a significant reduction in the vertical temperature gradient at the base of the mixed layer, which suppresses the upward transfer of cooler water into the mixed layer. Forced ocean and coupled ocean–atmosphere models that do not properly simulate the barrier layer may have difficulty reproducing the observed seasonal cycle of SST in the tropical North Atlantic.
    Materialart: Online-Ressource
    ISSN: 1520-0442 , 0894-8755
    RVK:
    Sprache: Englisch
    Verlag: American Meteorological Society
    Publikationsdatum: 2009
    ZDB Id: 246750-1
    ZDB Id: 2021723-7
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 12
    Online-Ressource
    Online-Ressource
    American Meteorological Society ; 2006
    In:  Journal of Climate Vol. 19, No. 23 ( 2006-12-01), p. 6122-6138
    In: Journal of Climate, American Meteorological Society, Vol. 19, No. 23 ( 2006-12-01), p. 6122-6138
    Kurzfassung: The role of horizontal oceanic heat advection in the generation of tropical North and South Atlantic sea surface temperature (SST) anomalies is investigated through an analysis of the oceanic mixed layer heat balance. It is found that SST anomalies poleward of 10° are driven primarily by a combination of wind-induced latent heat loss and shortwave radiation. Away from the eastern boundary, horizontal advection damps surface flux–forced SST anomalies due to a combination of mean meridional Ekman currents acting on anomalous meridional SST gradients, and anomalous meridional currents acting on the mean meridional SST gradient. Horizontal advection is likely to have the most significant effect on the interhemispheric SST gradient mode through its impact in the 10°–20° latitude bands of each hemisphere, where the variability in advection is strongest and its negative correlation with the surface heat flux is highest. In addition to the damping effect of horizontal advection in these latitude bands, evidence for coupled wind–SST feedbacks is found, with anomalous equatorward (poleward) SST gradients contributing to enhanced (reduced) westward surface winds and an equatorward propagation of SST anomalies.
    Materialart: Online-Ressource
    ISSN: 1520-0442 , 0894-8755
    RVK:
    Sprache: Englisch
    Verlag: American Meteorological Society
    Publikationsdatum: 2006
    ZDB Id: 246750-1
    ZDB Id: 2021723-7
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 13
    Online-Ressource
    Online-Ressource
    American Meteorological Society ; 2005
    In:  Journal of Climate Vol. 18, No. 20 ( 2005-10-15), p. 4168-4184
    In: Journal of Climate, American Meteorological Society, Vol. 18, No. 20 ( 2005-10-15), p. 4168-4184
    Kurzfassung: Recent observations have shown evidence of intraseasonal oscillations (with periods of approximately 1–2 months) in the northern and southern tropical Atlantic trade winds. In this paper, the oceanic response to the observed intraseasonal wind variability is addressed through an analysis of the surface mixed layer heat balance, focusing on three locations in the northwestern tropical Atlantic where in situ measurements from moored buoys are available (14.5°N, 51°W; 15°N, 38°W; and 18°N, 34°W). It is found that local heat storage at all three locations is balanced primarily by wind-induced latent heat loss, which is the same mechanism that is believed to play a dominant role on interannual and decadal time scales in the region. It is also found that the intraseasonal wind speed oscillations are linked to changes in surface wind convergence and convection over the western equatorial Atlantic warm pool. These atmospheric circulation anomalies and wind-induced SST anomalies potentially feed back on one another to affect longer time-scale variability in the region.
    Materialart: Online-Ressource
    ISSN: 1520-0442 , 0894-8755
    RVK:
    Sprache: Englisch
    Verlag: American Meteorological Society
    Publikationsdatum: 2005
    ZDB Id: 246750-1
    ZDB Id: 2021723-7
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 14
    Online-Ressource
    Online-Ressource
    American Meteorological Society ; 2013
    In:  Journal of Atmospheric and Oceanic Technology Vol. 30, No. 7 ( 2013-07-01), p. 1414-1432
    In: Journal of Atmospheric and Oceanic Technology, American Meteorological Society, Vol. 30, No. 7 ( 2013-07-01), p. 1414-1432
    Kurzfassung: Long-term and direct measurements of surface shortwave radiation (SWR) have been recorded by the Prediction and Research Moored Array in the Tropical Atlantic (PIRATA) since 1997. Previous studies have shown that African dust, transported westward from the Sahara and Sahel regions, can accumulate on mooring SWR sensors in the high-dust region of the North Atlantic (8°–25°N, 20°–50°W), potentially leading to significant negative SWR biases. Here dust-accumulation biases are quantified for each PIRATA mooring using direct measurements from the moorings, combined with satellite and reanalysis datasets and statistical models. The SWR records from five locations in the high-dust region (8°, 12°, and 15°N along 38°W; 12° and 21°N along 23°W) are found to contain monthly-mean accumulation biases as large as −200 W m−2 and record-length mean biases on the order of −10 W m−2. The other 12 moorings, located mainly between 10°S and 4°N, are in regions of lower atmospheric dust concentration and do not show statistically significant biases. Seasonal-to-interannual variability of the accumulation bias is found at all locations in the high-dust region. The moorings along 38°W also show decreasing trends in the bias magnitude since 1998 that are possibly related to a corresponding negative trend in atmospheric dust concentration. The dust-accumulation biases described here will be useful for interpreting SWR data from PIRATA moorings in the high-dust region. The biases are also potentially useful for quantifying dust deposition rates in the tropical North Atlantic, which at present are poorly constrained by satellite data and numerical models.
    Materialart: Online-Ressource
    ISSN: 0739-0572 , 1520-0426
    Sprache: Englisch
    Verlag: American Meteorological Society
    Publikationsdatum: 2013
    ZDB Id: 2021720-1
    ZDB Id: 48441-6
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 15
    Online-Ressource
    Online-Ressource
    American Geophysical Union (AGU) ; 2010
    In:  Geophysical Research Letters Vol. 37, No. 18 ( 2010-09), p. n/a-n/a
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 37, No. 18 ( 2010-09), p. n/a-n/a
    Materialart: Online-Ressource
    ISSN: 0094-8276
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 2010
    ZDB Id: 2021599-X
    ZDB Id: 7403-2
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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