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美国太平洋沿海湿地对海平面上升的弹性和脆弱性。

U.S. Pacific coastal wetland resilience and vulnerability to sea-level rise.

机构信息

U.S. Geological Survey, Western Ecological Research Center, 505 Azuar Drive, Vallejo, CA 94592, USA.

Departments of Geography, Ecology and Evolutionary Biology, and Institute of the Environment and Sustainability, University of California, Los Angeles, Los Angeles, CA 90095-1524, USA.

出版信息

Sci Adv. 2018 Feb 21;4(2):eaao3270. doi: 10.1126/sciadv.aao3270. eCollection 2018 Feb.

DOI:10.1126/sciadv.aao3270
PMID:29507876
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC5834000/
Abstract

We used a first-of-its-kind comprehensive scenario approach to evaluate both the vertical and horizontal response of tidal wetlands to projected changes in the rate of sea-level rise (SLR) across 14 estuaries along the Pacific coast of the continental United States. Throughout the U.S. Pacific region, we found that tidal wetlands are highly vulnerable to end-of-century submergence, with resulting extensive loss of habitat. Using higher-range SLR scenarios, all high and middle marsh habitats were lost, with 83% of current tidal wetlands transitioning to unvegetated habitats by 2110. The wetland area lost was greater in California and Oregon (100%) but still severe in Washington, with 68% submerged by the end of the century. The only wetland habitat remaining at the end of the century was low marsh under higher-range SLR rates. Tidal wetland loss was also likely under more conservative SLR scenarios, including loss of 95% of high marsh and 60% of middle marsh habitats by the end of the century. Horizontal migration of most wetlands was constrained by coastal development or steep topography, with just two wetland sites having sufficient upland space for migration and the possibility for nearly 1:1 replacement, making SLR threats particularly high in this region and generally undocumented. With low vertical accretion rates and little upland migration space, Pacific coast tidal wetlands are at imminent risk of submergence with projected rates of rapid SLR.

摘要

我们采用了一种首创的综合情景方法,评估了美国太平洋沿岸 14 个河口的潮汐湿地对海平面上升(SLR)速度变化的垂直和水平响应。在美国太平洋地区,我们发现潮汐湿地极易受到本世纪末淹没的影响,导致栖息地大量丧失。在使用较高范围的海平面上升情景时,所有高和中沼泽生境都已丧失,到 2110 年,当前的潮汐湿地有 83%将转变为无植被生境。到本世纪末,加利福尼亚州和俄勒冈州的湿地损失更大(100%),但华盛顿州的情况仍然严重,有 68%的湿地被淹没。在较高范围的海平面上升率下,到本世纪末,仅低沼泽湿地将保留。即使在更保守的海平面上升情景下,潮汐湿地的损失也很可能发生,到本世纪末,高沼泽地的 95%和中沼泽地的 60%将丧失。大多数湿地的水平迁移受到沿海开发或陡峭地形的限制,只有两个湿地有足够的内陆空间进行迁移,并且有可能实现近 1:1 的替代,这使得该地区的海平面上升威胁特别高,而且通常没有记录。由于垂直堆积率低和内陆迁移空间小,太平洋沿岸的潮汐湿地面临着因预计的快速海平面上升而淹没的迫在眉睫的风险。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5bc9/5834000/6744fb708721/aao3270-F5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5bc9/5834000/6931127b4c27/aao3270-F1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5bc9/5834000/7d6e4ad37dff/aao3270-F2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5bc9/5834000/d2fe27663105/aao3270-F3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5bc9/5834000/1e2b91d53b65/aao3270-F4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5bc9/5834000/6744fb708721/aao3270-F5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5bc9/5834000/6931127b4c27/aao3270-F1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5bc9/5834000/7d6e4ad37dff/aao3270-F2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5bc9/5834000/d2fe27663105/aao3270-F3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5bc9/5834000/1e2b91d53b65/aao3270-F4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5bc9/5834000/6744fb708721/aao3270-F5.jpg

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