Wetland Gain and Loss in the Mississippi River Bird-Foot Delta

IF 7.3 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES
Earths Future Pub Date : 2025-06-19 DOI:10.1029/2024EF005003
Jiangjie Yang, Zhijun Dai, Xuefei Mei, Yaying Lou, Sergio Fagherazzi
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Abstract

The Mississippi River Bird-foot Delta (MRBD) has long been at risk of deterioration due to Relative Sea Level Rise (RSLR), yet information on historical spatial distribution in wetland gain and loss remains limited. Using a Random Forest algorithm in Google Earth Engine, we extract wetland area from multiple Landsat images spanning 1990–2022. Data are integrated with sediment load, wave dynamics, sea level, and surface elevation to analyze drivers of wetland gain and loss. Results indicate a minor net change of only 1.21 km2, with a total gain of 160.83 km2 and a total loss of 159.62 km2. Overall stability of wetland area masks significant regional variability, with notable wetland expansion in the interior and substantial losses along eastern and southeastern margins. Sediment diversion toward the interior of the delta lead to distributaries narrowing (Main Pass and Pass a Loutre) that further hindered sediment-laden water transport into deltaic margins. Wetland dynamics along the edges were closely linked to wave action, with large-scale retreat in northern (4.0 ± 9.9 m/yr), eastern (58.0 ± 48.2 m/yr), and southeastern (38.6 ± 15.8 m/yr) regions, while progradation in the southern (13.6 ± 10.1 m/yr) and western areas (7.4 ± 19.4 m/yr). Fluvial sediments significantly impact wetland growth with 1-year lag. Vertical accretion of wetlands exceeds RSLR, indicating equilibrium along vertical dimension but are affected by lateral dynamics driven by wave and fluvial sediment inputs. In conclusion, the MRBD is abandoning the distal parts to wave erosion, while focusing on building wetlands in the interior to create a more compact delta.

密西西比河鸟足三角洲湿地的得失
由于相对海平面上升(RSLR)的影响,密西西比河鸟脚三角洲(MRBD)长期处于退化的危险之中,但有关湿地增减的历史空间分布信息仍然有限。利用谷歌Earth Engine中的随机森林算法,从1990-2022年的多幅Landsat图像中提取湿地面积。数据与泥沙负荷、波浪动力学、海平面和地表高程相结合,分析湿地增减的驱动因素。结果表明,净变化较小,仅为1.21 km2,总增益为160.83 km2,总损失为159.62 km2。湿地面积的总体稳定性掩盖了显著的区域差异,内陆湿地扩张显著,东部和东南部边缘湿地损失显著。沉积物向三角洲内部转移导致支流变窄(主要通道和河口),进一步阻碍了含沙水向三角洲边缘的运输。边缘湿地动态与波浪作用密切相关,北部(4.0±9.9 m/yr)、东部(58.0±48.2 m/yr)和东南部(38.6±15.8 m/yr)区域出现大规模后退,南部(13.6±10.1 m/yr)和西部(7.4±19.4 m/yr)区域出现进积。河流沉积物对湿地生长的影响具有显著的1年滞后效应。湿地的垂直增积超过RSLR,表明湿地在垂直方向上处于平衡状态,但受到波浪和河流沉积物输入驱动的横向动力的影响。总之,MRBD正在放弃远端部分的波浪侵蚀,而专注于在内部建立湿地,以创造一个更紧凑的三角洲。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Earths Future
Earths Future ENVIRONMENTAL SCIENCESGEOSCIENCES, MULTIDI-GEOSCIENCES, MULTIDISCIPLINARY
CiteScore
11.00
自引率
7.30%
发文量
260
审稿时长
16 weeks
期刊介绍: Earth’s Future: A transdisciplinary open access journal, Earth’s Future focuses on the state of the Earth and the prediction of the planet’s future. By publishing peer-reviewed articles as well as editorials, essays, reviews, and commentaries, this journal will be the preeminent scholarly resource on the Anthropocene. It will also help assess the risks and opportunities associated with environmental changes and challenges.
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