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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Geomorphic knowledge for mangrove restoration: a pan-tropical categorization
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Geomorphic knowledge for mangrove restoration: a pan-tropical categorization

机译:红树林恢复的地貌知识:泛热带分类

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Extreme events such as storm surges and tsunamis in combination with subsidence of densely populated coastal areas pose an increasing threat to millions of people in the tropics. Intertidal mangrove forests may form a natural protection against some extreme events, but have also widely been destroyed by coastal development. The establishment of mangroves and the maintenance of their stability over the short- to long-term requires an understanding of sedimentary processes and landforms in the coastal zone, making geomorphology a crucial, but sometimes neglected discipline when attempting restoration for disaster risk reduction. Mangrove geomorphic setting varies markedly across the tropics, depending on abiotic parameters such as suspended sediment supply and tidal range, with different restoration strategies suitable for each. In this study we provide a global categorization of mangrove geomorphic settings, based on the literature and global remote sensing data. The world's mangroves can be broadly defined as: (1) minerogenic and high tidal range; (2) minerogenic and low tidal range; and (3) organogenic and low tidal range. We further discuss restoration and management approaches most suitable for each geomorphic setting. Overall, this study can be used to inform managers about the relevance of geomorphic knowledge for successful mangrove restoration, how an understanding of geomorphology can influence site selection and restoration success, and how to match specific restoration methods to the prevailing geomorphic context. The stronger incorporation of geomorphic knowledge into site planning and design will improve the success rates of restoration for this important and globally threatened ecosystem. Copyright (c) 2015 John Wiley & Sons, Ltd.
机译:风暴潮和海啸等极端事件,再加上人口稠密的沿海地区的沉陷,对热带地区的数百万人构成了越来越大的威胁。潮间带的红树林可能构成抵御某些极端事件的自然保护,但也被沿海开发广泛破坏。建立红树林及其在短期至长期内的稳定性需要了解沿海地区的沉积过程和地貌,这使得地貌学成为至关重要的,但在尝试进行恢复以减少灾害风险时有时会被忽视。红树林的地貌环境在整个热带地区显着不同,这取决于非生物参数,例如悬浮的泥沙供应和潮汐范围,并且每种生态系统都有不同的恢复策略。在这项研究中,我们根据文献和全球遥感数据对红树林地貌环境进行了全球分类。世界上的红树林可大致定义为:(1)致矿作用和高潮差; (2)成矿作用和低潮差; (3)器官形成和低潮汐范围。我们将进一步讨论最适合每种地貌环境的恢复和管理方法。总体而言,该研究可用于告知管理人员有关地貌知识与成功的红树林恢复的相关性,对地貌的理解如何影响选址和恢复成功以及如何将特定的恢复方法与当前的地貌环境相匹配。将地貌知识更强地整合到场地规划和设计中,将提高这一重要且受到全球威胁的生态系统恢复的成功率。版权所有(c)2015 John Wiley&Sons,Ltd.

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