不同湿地景观的水文同步与功能冗余

IF 2.9 3区 地球科学 Q1 Environmental Science
Joshua M. Epstein, Matthew J. Cohen
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引用次数: 0

摘要

湿地淹没和水文连通性的时间、持续时间和同步性的变化影响了湿地景观(即嵌入高地的不同湿地复合体)的总体水文、生物地球化学和生境功能。为了量化和预测湿地之间水文功能的冗余性,我们测量了佛罗里达州三个湿地景观的水文同步性,并对比了形态和连通性模式。将每个湿地景观中多个湿地(n = 14-15)的高频阶段与激光雷达衍生的地形相结合,我们基于湿地阶段相关性和淹没(即湿与干)和表面连通性(即连通与不连通)模式的每日对齐来测量同步。我们评估了流道成员或位置、湿地大小、深度和距离如何影响同步模式。我们进一步评估了假设整个湿地景观的平面水位在空间上是均匀的,这意味着完美的水位同步,是否准确地代表了观测到的模式。在地形异质性最小的湿地中,观测到的同步几乎是完美的,在那里,地表连通性频繁且持续时间长,支持空间均匀地下水位的假设。湿地的大小、距离和深度预测了同步性,而湿地水文功能的变化可以忽略不计,完全归因于地形异质性。相反,在地形异质性最大的地区,水文同步性较低,地表水连通性罕见且短暂。在这里,流道成员是同步性的重要预测因子。不同湿地景观的湿地水文冗余度差异显著,当同步性高时,总体景观功能的退化与湿地面积的损失成正比,但在水文同步性和冗余度较低时,景观功能的退化速度要快于湿地面积的损失。随着国家和全球湿地的持续损失,同步评估为评估和预测湿地景观对湿地功能丧失的恢复力提供了信息,并为非冗余湿地的优先保护提供了信息,以确保维持湿地景观结构的完整连续性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Wetland Hydrologic Synchrony and Functional Redundancy Across Contrasting Wetlandscapes

Wetland Hydrologic Synchrony and Functional Redundancy Across Contrasting Wetlandscapes

Variation in the timing, duration, and synchrony of wetland inundation and hydrologic connectivity influences aggregate hydrologic, biogeochemical, and habitat functions of wetlandscapes (i.e., complexes of distinct wetlands embedded in uplands). To quantify and predict the redundancy of hydrological functions amongst wetlands, we measured hydrologic synchrony in three Florida wetlandscapes with contrasting morphology and connectivity patterns. Combining high frequency stage from multiple wetlands (n = 14–15) in each wetlandscape with LiDAR-derived topography, we measured synchrony based on wetland stage correlation and daily alignment of inundation (i.e., wet vs. dry) and surface connectivity (i.e., connected vs. disconnected) patterns. We evaluated how flowpath membership or position, wetland size, depth, and distance impacted synchrony patterns. We further evaluated whether assuming a spatially uniform planar water table across the wetlandscapes, implying perfect water level synchrony, accurately represented observed patterns. Observed synchrony was nearly perfect in the least topographically heterogeneous wetlandscape, where surface connectivity was frequent and prolonged, supporting the assumption of a spatially uniform water table. Wetland size, distance, and depth predicted synchrony, and variation in wetland hydrological function was negligible and fully attributed to topographic heterogeneity. In contrast, hydrological synchrony was lower where wetlandscape topographic heterogeneity was highest, and surface water connectivity was rare and brief. Here, flowpath membership was a significant predictor of synchrony. Hydrological redundancy of wetlands varies markedly across wetlandscapes, with aggregate landscape function degraded in proportion to wetland area loss when synchrony is high, but degraded more rapidly than the loss of area where hydrologic synchrony, and therefore redundancy, is low. With ongoing wetland losses nationally and globally, synchrony assessments inform efforts to evaluate and predict wetlandscape resilience to loss of wetland function and prioritise conservation of non-redundant wetlands to ensure the full continuum of wetlandscape structure is maintained.

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来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
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