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  • Wiley-Blackwell  (3)
  • Maputo, Mozambique  (1)
  • 2015-2019  (3)
  • 2010-2014  (1)
  • 1
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    SEACAM | Maputo, Mozambique
    Publication Date: 2021-05-19
    Description: The project focuses on safeguarding the biodiversity, natural resources and ecological processes in Kiunga Marine and Dodori national Reserves through the development and implementation of a consensus-based management plan, involving full participation of local communities.
    Description: Published
    Keywords: Marine resources ; Marine parks ; Protected areas ; Protected resources ; Biodiversity ; Resource conservation ; Resource management
    Repository Name: AquaDocs
    Type: Book Section , Not Known
    Format: pp.51-57
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  • 2
    Publication Date: 2013-08-20
    Description: [1]  The evolution of ocean temperature measurement systems is presented with a focus on the development and accuracy of two critical devices in use today (expendable bathythermographs and CTDs – conductivity-temperature-depth instruments used on Argo floats). A detailed discussion of the accuracy of these devices and a projection of the future of ocean temperature measurements are provided. The accuracy of ocean temperature measurements is discussed in detail in the context of ocean heat content, Earth's energy imbalance, and thermosteric sea level rise. Up-to-date estimates are provided for these three important quantities. The total energy imbalance at the top-of-atmosphere is best assessed by taking an inventory of changes in energy storage. The main storage is in the ocean; the latest values of which are presented. Furthermore, despite differences in measurement methods and analysis techniques, multiple studies show that there has been a multi-decadal increase in the heat content of both the upper and deep ocean regions, which reflect the impact of anthropogenic warming. With respect to sea-level rise, mutually reinforcing information from tide gauges and radar altimetry show that presently, sea-level is rising at approximately 3 mm yr -1 with contributions from both thermal expansion and mass accumulation from ice melt. The latest data for thermal expansion sea-level rise are included here and analyzed.
    Print ISSN: 8755-1209
    Topics: Geosciences
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  • 3
    Publication Date: 2017-10-26
    Description: Several existing statistical and dynamical reconstructions of past regional sea level variability and trends are compared with each other and with tide gauges over the 48-yr period 1960–2007, partially pre-dating the satellite altimetry era. Evaluated statistical reconstructions were built from tide gauge data (TGR), and dynamical reconstructions from ocean data assimilation (ODA) approaches. Although most of the TGRs yield global-mean time series of sea level with trends deviating within only ±0.1 mm yr −1 , the spatial anomalies of the trends deviate substantially between the reconstructions over the period predating altimetry. In contrast, TGRs match observed regional trend patterns fairly well during the satellite altimetry era. TGRs match tide gauge data better than ODA results; however, they exhibit less variability in the open ocean compared to altimetric data. Over the pre-altimetry period, all reconstructed regional sea level trend patterns deviate substantially from each other. In terms of detrended correlations in this earlier period, the reconstructions match tide gauges, and each other, much better in the Pacific than in the Atlantic. An ensemble of all TGR and ODA estimates provides some improvements in correlations and trends to both tide gauges and altimetry. Nevertheless, a lack of independent open-ocean sea surface height data predating altimetry makes impossible the validation of the ensemble for pre-altimetry open ocean sea level trends and variability. Estimating regional sea level changes prior to altimetry therefore remains an unsolved challenge.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
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  • 4
    Publication Date: 2016-12-28
    Description: We note the presence in the literature of two different concepts of the term ‘active layer’ in relation to fluvial sediment transport. It has been used to represent the current dynamically active streambed surface, or to represent the depth of event-scale scour and fill. These concepts involve distinct length and time scales. We propose that, when the distinction is important, the concepts be distinguished as either a ‘dynamical active layer' or an ‘event active layer'. This article is protected by copyright. All rights reserved.
    Print ISSN: 0043-1397
    Electronic ISSN: 1944-7973
    Topics: Architecture, Civil Engineering, Surveying , Geography
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