首页> 外文会议>Coastal sediments'03: crossing disciplinary boundaries >WAVE TRANSFORMATIONS OVER MUDFLAT AND SALTMARSH SURFACES ONTHE UK EAST COAST - IMPLICATIONS FOR MARSH EVOLUTION
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WAVE TRANSFORMATIONS OVER MUDFLAT AND SALTMARSH SURFACES ONTHE UK EAST COAST - IMPLICATIONS FOR MARSH EVOLUTION

机译:英国东海岸泥浆和盐沼表面上的波变换-对沼泽演化的影响

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An extensive dataset of wave spectra was collected for marsh surface inundationrnevents (Sept 2000 - Jan 2002) at two sites on the Dengie saltmarshes, eastern England (southernrnNorth Sea), using a network of 21 bottom-mounted pressure sensors, covering both intertidalrnmudflat and saltmarsh surfaces. This paper focuses on an in-depth analysis of changes in wavernspectra over a range of distances across mudflat and saltmarsh surfaces and at a cliffed marshrnedge during 15 selected inundation events. Directional wave spectra were obtained on thernunvegetated intertidal flat and, together with information on meteorological conditions, are usedrnto explain the temporal and spatial variations in wave spectral characteristics. In particular, thernobserved patterns / re-distribution of spectral energy and peak wave period shifts over thernmudflat and the marsh surface are discussed for contrasting root-mean-square wave heightrn(Hrms) to water depth (h) ratios. Similarities and differences in the spectral transformationsrnobserved at both sites are discussed with reference to the contrasting mudflat and marsh edgerntopographies of the two field sites. From this comparison, the paper concludes that siterncharacteristics, including substrate type, micro-topography, and marsh surface vegetation cover,rnrather than meteorological conditions, are crucial in explaining the wave spectra transformations.rnSpectral transformations at the gradually sloping mudflat-saltmarsh transition generally confirmrnexpected patterns of energy redistribution derived from wave theory and observed in laboratoryrnmodels. At the more complex, cliffed transition, however, spectral changes vary significantlyrnbetween events with contrasting ('high' vs. 'low') Hrms/h ratios. Improved models are nowrnrequired to (a) evaluate marsh surface responses to changes in environmental forcing consequentrnupon global climate change, and (b) assist in the formulation of 'design rules' for the restorationrnand re-creation of degrading marsh systems.
机译:利用21个底部安装的压力传感器网络,收集了英格兰东部登格盐沼(北海南部)两个地点的沼泽地表淹没事件的大量波谱数据(2000年9月至2002年1月),覆盖了潮间带滩涂和盐沼表面。本文着重深入分析了在15个选定的淹没事件期间,在泥滩和盐沼表面以及悬崖沼泽边缘的一定距离范围内,波谱的变化。在无植被的潮间带上获得定向波谱,并与气象条件信息一起用于解释波谱特征的时空变化。尤其是,讨论了在平坦地带和沼泽地上的热能观测模式/频谱能量的重新分布和峰值波周期的偏移,以比较均方根波高rn(Hrms)与水深(h)的比率。参照两个现场的对比泥滩和沼泽边缘地形学,讨论了在两个现场观测到的光谱变换的异同。通过这种比较,本文得出结论,包括底物类型,微观地形和沼泽地表植被覆盖等地物特征,而不是气象条件,对于解释波谱转换至关重要。在逐渐倾斜的泥滩-盐沼转变处的光谱转换通常证实了预期的特征。波动理论推导的能量重新分布模式,并在实验室模型中观察到。然而,在更为复杂的陡峭过渡处,事件之间的光谱变化具有明显的Hrms / h比(“高”与“低”)比。现在需要改进的模型来(a)评估沼泽地表对环境强迫变化的响应,从而导致全球气候变化,以及(b)协助制定“设计规则”以恢复和重新创建退化的沼泽系统。

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