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Adding to the toolbox for tidal-inundation mapping in estuarine areas

机译:添加到eStuarine地区的TIDal-Inundation映射的工具箱

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In estuaries, land-surface and tidal elevation conspire to influence the amount of salt-water inundation in a specific location, ultimately affecting the distribution of estuary vegetation. Plants vary in their tolerances to salinity and inundation. Understanding even small changes in land-surface elevation at a site scale provides relevant information to managers seeking to design effective long-term restoration projects. Restoration of estuary habitats has been identified as a tool to mediate some anticipated effects of climate change, including flooding from sea-level rise, precipitation regimes, and storminess. Further, habitat restoration that is effective in the face of climate uncertainty is critical to the sustainable production of seafood and maintenance of ecosystem functions. We offer a simple method that links tidal elevations to upslope topography, allowing managers to determine where tidal inundation of upslope areas may occur. This method does not require complex modeling, rather we combine existing high-accuracy tide-gage information with LiDAR imagery. However, we found that if LiDAR is not flown at low tide, or at consistent tidal heights, it poses significant challenges in the interpretation of tidal elevations. Where LiDAR is consistently collected at low tide, this method of linking the tidal datum to upslope topography is not data-intensive, and does not require long-term data collection. Along with locally specific information, the types of map products that can be developed using this method should identify places that may be potentially vulnerable to salt-water inundation, along with places that may be effective migration corridors for marshes and other habitats.
机译:在河口,地表和潮汐高程共同影响特定位置的盐水淹没量,最终影响河口植被的分布。植物对盐分和洪水的耐受力各不相同。了解场地范围内地表高程的微小变化,可以为寻求设计有效长期修复项目的管理者提供相关信息。河口栖息地的恢复已被确定为调解气候变化的一些预期影响的工具,包括海平面上升引起的洪水、降水状况和暴风雨。此外,在气候不确定性面前有效的栖息地恢复对于海鲜的可持续生产和生态系统功能的维持至关重要。我们提供了一种将潮汐高程与上坡地形联系起来的简单方法,允许管理人员确定上坡区域可能发生潮汐淹没的位置。这种方法不需要复杂的建模,而是将现有的高精度验潮仪信息与激光雷达图像相结合。然而,我们发现,如果激光雷达不在低潮或一致的潮汐高度下飞行,则在解释潮汐高度时会带来重大挑战。在低潮时持续收集激光雷达的情况下,这种将潮汐基准面与上坡地形联系起来的方法不需要大量数据,也不需要长期收集数据。除了本地特定信息外,使用该方法可以开发的地图产品类型应确定可能容易受到盐水淹没的地方,以及可能成为沼泽和其他栖息地有效迁移走廊的地方。

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