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  • 1
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Industrial and engineering chemistry 2 (1963), S. 61-66 
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2021-05-19
    Description: Global change is defined here for this review as changes caused by increasing greenhouse gas emissions resulting in a high CO2 world and the direct and indirect changes that ensue. Increasing green house gas emissions are causing three major impacts on the ocean: warming sea surface temperature (SST), ocean acidification and deoxygenation (Turley et al 2011). The latter two are poorly understood at present, particularly in Eastern Africa. Secondary impacts include sea level rise due to melting polar ice caps. Coral bleaching and death caused by SST rise has been extensively studied and measured (HoeghGuldberg 1999; Hughes et al. 2003), including in the WIO (Obura 2005, McClanahan 2009), with likely ecosystem phase shifts as coral reefs become dominated by macroalgae (brown algae such as Turbinaria, Sargassum spp.) (Bellwood et al. 2004; Hughes et al. 2005). Ocean acidification is likely to have enormous impacts on marine resources and hence fisheries (Turley et al. 2011), as ocean chemistry is changed and thus any marine organisms that rely on Ph sensitive chemical reactions will be affected. This field is still relatively new and early reports predict trophic level shifts as organisms with calcium carbonate skeletons, e.g molluscs, corals, are compromised. Deoxygenation is caused by ocean warming (oxygen becomes less soluble) which will result in less growth of most marine organisms and a shift to low oxygen tolerant organisms, often microorganisms. Coastal environments and people are also undergoing changes that are directly related to human pressures caused by development and other activities. These include increasing population, mechanisation (eg in fisheries), industrialisation (eg ports and coastal cities), pollution, and extraction of oil and gas.
    Description: Published
    Keywords: Global warming ; Sea level changes ; Greenhouse effect ; Mangroves ; Surface temperature
    Repository Name: AquaDocs
    Type: Report , Not Known
    Format: 50pp.
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  • 3
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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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  • 4
    Publication Date: 2021-05-19
    Description: Coral reefs in the Kiunga Marine National Reserve (KMNR) (40o 07’ E, 2o 00’ S) are located in a transition ecotone between the warmer East African coral reef bioregion to the south, and colder waters of the Somali Current to the north. The reefs have been monitored annually from 1998 to the present, documenting a range of ecosystem changes from large and small scale threats. Reefs in the area suffered ˜60% loss of coral cover due to mass bleaching in the 1998 El Niño event, and 25-40% loss of coral species at individual site levels. Recovery of coral community structure has been variable, with some reefs showing strong recovery, while others have declined further. A harmful algal bloom and coral disease in early 2002 further impacted these reefs, causing mass mortalities of fish and coral, and failure of coral recruitment in that year. Fishing impacts to the reserve are high, with a strong south-north decline in fish density due to easier access to the migrant and large fishing communities to the south of the reserve. Responsibility for management of the KMNR falls under multiple institutions, including the Kenya Wildlife Service, Fisheries and Forestry Departments, and the local council. Overlapping mandates, unclear relationships, limited information and understanding, and lack of resources have hampered effective management. The monitoring programme reported here is one aspect of new collaborative appro aches to coral reef and fisheries management, and has focused on improving the information and understanding of the biological and resource systems of the area. The ecosystem trends induced by larger scale threats and the south-north fish resource gradient caused by local use patterns will be analyzed in an attempt to develop sustainable management practices for the reserve.
    Description: Published
    Keywords: Fisheries management ; Overfishing ; Coral reefs ; Ecosystems ; Mass mortality
    Repository Name: AquaDocs
    Type: Book Section , Refereed
    Format: pp.1381-1390
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  • 5
    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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  • 6
    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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