局部海平面加速上升对湿地影响的遥感

R. Field, K. Philipp, V. Klemas, Jo Young
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引用次数: 0

摘要

预计未来50年海平面将大幅上升,风暴将更加频繁,这将影响沿海湿地、海滩侵蚀控制策略、河口和含水层盐度、沿海排水系统和沿海经济发展。沿海湿地,包括潮汐盐沼、潮汐淡水沼泽和红树林沼泽,一般在海平面不到一米的范围内,可能会消失,特别是如果相对海平面上升的影响被沿海风暴放大的话。为了规划湿地保护和合理的沿海发展,科学家和管理者需要监测沿海湿地随着海平面持续上升而发生的变化。本研究的主要目的是分析由于运河决口而面临海平面加速上升的特拉华湾潮汐湿地的变化,并展示如何使用遥感和相关技术来研究相对海平面上升(RSLR)和人类活动对沿海湿地的影响。第二个目标是通过尝试预测该测试点的未来变化来评估几个RSLR模型。初步结果表明,米尔福德颈部保护区试验场的植被、水文、泥沙增积和侵蚀正在发生快速变化,卫星和飞机遥感在合理数量的实地考察的支持下,非常适合对这些变化进行制图和研究。对该地点发生的过程的更好理解将有助于湿地管理者决定是否通过河道改造来干预水力制度,以加速或延迟沼泽在特定方向的发展。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Remote sensing of the impact of accelerated local sea level rise on wetlands
The substantial relative sea level rise and more frequent storms predicted for the next 50 years, will impact coastal wetlands, beach erosion control strategies, salinity of estuaries and aquifers, coastal drainage systems, and coastal economic development. Coastal wetlands, including tidal salt marshes, tidal freshwater marshes and mangrove swamps, are generally within fractions of a meter of sea level, and could be lost, especially if the impact of relative sea level rise is amplified by coastal storms. To plan for wetland protection and sensible coastal development, scientists and managers need to monitor the changes in coastal wetlands as the sea level continues to rise. The primary objective of our study is to analyze changes at a unique Delaware Bay tidal wetland site, which faces an accelerated sea level rise due to a canal breach and to show how remote sensors and related techniques can be used for studying the impact of relative sea level rise (RSLR) and human activities on coastal wetlands. A secondary objective is to evaluate several RSLR models by trying to predict future changes at this test site. Preliminary results indicate that rapid changes of vegetation, hydrology, sediment accretion and erosion are taking place at the Milford Neck Conservation Area test site and that satellite and aircraft remote sensors, supported by a reasonable number of site visits, are highly suitable for mapping and studying these changes. The improved understanding of the processes occurring at this site will help wetland managers decide whether to intervene in the hydraulic regime by channel modification in order to accelerate or delay marsh development in a particular direction.
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