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  • vegetation density  (2)
  • mangrove physics  (1)
  • 1
    Keywords: mangrove systems ; physical processes ; mangrove physics ; tidal flow ; mangrove vegetation ; mangrove swamps ; sea waves and tsunamis ; formation of water properties ; material exchange ; sediment transport ; groundwater flow ; formation of soil properties
    Description / Table of Contents: Part I: Outline of the physical processes within mangrove systems --- Chapter 1: Introduction --- Chapter 2: Present state of mangrove studies from a physical viewpoint --- Chapter 3: Physical factors that shape mangrove environments --- Chapter 4: Hydrodynamics and physics that support the mangrove environment --- Chapter 5: Feedback processes that maintain the mangrove environment --- Chapter 6: Research technology --- Chapter 7: Modeling of mangrove systems --- Chapter 8: Future studies in the context of the preservation and utilization of mangroves
    Pages: Online-Ressource (XX, 598 Seiten)
    Language: English
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Mangroves and salt marshes 3 (1999), S. 59-66 
    ISSN: 1572-977X
    Keywords: dispersion ; mangrove swamp ; secondary circulation ; tidal creek ; tidal trapping ; vegetation density
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The dependence of dispersion in a tidal creek on the vegetation density in a fringing mangrove swamp is discussed through a numerical model. A secondary circulation prevails everywhere in the tidal creek‐mangrove swamp system and is generated by the overflow into the swamp at every high tide. As a result, dissolved and suspended matter moving with the circulation is trapped in the swamp for a fraction of the tidal cycle; it flows out of the swamp at ebb tide and disperses in the creek. The relation between the dispersion coefficient and the mangrove vegetation density is shown to be non‐linear. Dispersion is large both for bare and high vegetation densities and minimum for intermediate vegetation density. The ecological and management applications may be profound as our study suggests that such systems may be unstable and cannot naturally recover from excessive anthropogenic disturbances.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Mangroves and salt marshes 1 (1997), S. 193-199 
    ISSN: 1572-977X
    Keywords: mangrove swamp ; drag coefficient ; flow resistance ; tidal flow ; vegetation density ; Reynolds number
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Field studies of tidal flows in largely pristine mangrove swamps suggestthat the momentum equation simplifies to a balance between the water surfaceslope and the drag force. The controlling parameter is the vegetation lengthscale LE, which is a function of the projected area ofmangrove vegetation and the volume of the vegetation. The value ofLE varies greatly with mangrove species and water depth. It isfound that the drag coefficient is related to the Reynolds number Re definedusing LE. The drag coefficient decreases with increasingvalues of Re from a maximum value of 10 at low value of Re (〈104), and converges towards 0.4 for Re 〈 5 ×104.
    Type of Medium: Electronic Resource
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