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  • 1
    Online Resource
    Online Resource
    American Meteorological Society ; 2013
    In:  Journal of Atmospheric and Oceanic Technology Vol. 30, No. 4 ( 2013-04-01), p. 810-824
    In: Journal of Atmospheric and Oceanic Technology, American Meteorological Society, Vol. 30, No. 4 ( 2013-04-01), p. 810-824
    Abstract: Biases in the depth estimation of expendable bathythermograph (XBT) measurements cause considerable errors in oceanic estimates of climate variables. Efforts are currently underway to improve XBT probes by including pressure switches. Information from these pressure measurements can be used to minimize errors in the XBT depth estimation. This paper presents a simple method to correct the XBT depth biases using a number of discrete pressure measurements. A blend of controlled simulations of XBT measurements and collocated XBT/CTD data is used along with statistical methods to estimate error parameters, and to optimize the use of pressure switches in terms of number of switches, optimal depth detection, and errors in the pressure switch measurements to most efficiently correct XBT profiles. The results show that given the typical XBT depth biases, using just two pressure switches is a reliable strategy for reducing depth errors, as it uses the least number of switches for an improved accuracy and reduces the variance of the resulting correction. Using only one pressure switch efficiently corrects XBT depth errors when the surface depth offset is small, its optimal location is at middepth (around or below 300 m), and the pressure switch measurement errors are insignificant. If two pressure switches are used, then results indicate that the measurements should be taken in the lower thermocline and deeper in the profile, at approximately 80 and 600 m, respectively, with an RMSE of approximately 1.6 m for pressure errors of 1 m.
    Type of Medium: Online Resource
    ISSN: 0739-0572 , 1520-0426
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 2013
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    Location Call Number Limitation Availability
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  • 2
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2014
    In:  Journal of Geophysical Research: Oceans Vol. 119, No. 9 ( 2014-09), p. 5654-5675
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 119, No. 9 ( 2014-09), p. 5654-5675
    Abstract: A significant increase in the salinity minimum starts in the 1990s Salinity increase linked to advective mechanisms and increased Agulhas leakage Drivers of changes are the Southern Annular Mode and CO 2 increase
    Type of Medium: Online Resource
    ISSN: 2169-9275 , 2169-9291
    URL: Issue
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2014
    detail.hit.zdb_id: 2016804-4
    detail.hit.zdb_id: 161667-5
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    SSG: 16,13
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  • 3
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2012
    In:  Journal of Geophysical Research: Atmospheres Vol. 117, No. D4 ( 2012-02-27), p. n/a-n/a
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 117, No. D4 ( 2012-02-27), p. n/a-n/a
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2012
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    detail.hit.zdb_id: 2016813-5
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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
    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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  • 4
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2013
    In:  Journal of Geophysical Research: Oceans Vol. 118, No. 6 ( 2013-06), p. 3026-3045
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 118, No. 6 ( 2013-06), p. 3026-3045
    Abstract: Synthetic method is efficiently applied to monitor currents The NECC and NEUC variability are linked to the meridional mode The NECC overlaps with the NEUC during winter/spring
    Type of Medium: Online Resource
    ISSN: 2169-9275 , 2169-9291
    URL: Issue
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2013
    detail.hit.zdb_id: 2016804-4
    detail.hit.zdb_id: 161667-5
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  • 5
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 2011
    In:  Climatic Change Vol. 109, No. 3-4 ( 2011-12), p. 719-744
    In: Climatic Change, Springer Science and Business Media LLC, Vol. 109, No. 3-4 ( 2011-12), p. 719-744
    Type of Medium: Online Resource
    ISSN: 0165-0009 , 1573-1480
    RVK:
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2011
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    SSG: 14
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  • 6
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 115, No. C12 ( 2010-12)
    Abstract: Current projections of the oceanic response to anthropogenic climate forcings are uncertain. Two key sources of these uncertainties are (1) structural errors in current Earth system models and (2) imperfect knowledge of model parameters. Ocean tracer observations have the potential to reduce these uncertainties. Previous studies typically consider each tracer separately, neglect potentially important statistical properties of the system, or use methods that impose rather daunting computational demands. Here we extend and improve upon a recently developed approach using horizontally averaged vertical profiles of chlorofluorocarbon (CFC‐11), radiocarbon (Δ 14 C), and temperature (T) observations to reduce model parametric and structural uncertainties. Our method estimates a joint probability density function, which considers cross‐tracer correlations and spatial autocorrelations of the errors. We illustrate this method by estimating two model parameters related to the vertical diffusivity, the background vertical diffusivity, and the upper Southern Ocean mixing. We show that enhancing the upper Southern Ocean mixing in the model improves the representations of ocean tracers and improves the hindcasts of the Atlantic Meridional Overturning Circulation (AMOC). The most probable value of the background vertical diffusivity in the pelagic pycnocline is between 0.1 and 0.2 cm 2 s −1 . According to the statistical method, observations of Δ 14 C reduce the uncertainty about the background vertical diffusivity mostly followed by CFC‐11 and T. Using all three tracers jointly reduces the model uncertainty by 40%, more than each tracer individually. Given several important caveats, we illustrate how the reduced model parametric uncertainty improves probabilistic projections of the AMOC.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2010
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    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
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    SSG: 16,13
    Location Call Number Limitation Availability
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  • 7
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2010
    In:  Journal of Geophysical Research: Oceans Vol. 115, No. C10 ( 2010-10)
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 115, No. C10 ( 2010-10)
    Abstract: We introduce a parameterization of ocean mixing by tropical cyclones (TCs) into an Earth system model of intermediate complexity. The parameterization is based on previously published global budgets of TC‐induced mixing derived from high‐resolution satellite measurements of anomalous sea surface temperatures along storm tracks. Recognizing the caveats introduced, for example, by the simplified model structure, we find that the representation of realistic TC‐induced mixing substantially alters the equilibrium conditions of (1) the thermal structure of the upper ocean, (2) the surface energy budget, and (3) the circulation in the equatorial to subtropical Pacific Ocean. These changes result in warmer upwelling regions in the eastern equatorial Pacific and an overall increase in ocean heat content consistent with the recent TC heat pump hypothesis. Spatial variability in the mixing appears to be a key factor in the modeled response. We find no substantial influence of the considered TC‐induced mixing on poleward ocean heat transport in the analyzed model. Our results suggest that climate‐sensitive mixing feedbacks are plausible; however, the large‐scale effect is mainly confined to the subtropical Indo‐Pacific region for present‐day TC climatology.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2010
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    detail.hit.zdb_id: 2016804-4
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    SSG: 16,13
    Location Call Number Limitation Availability
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