Analysis of the influence of climate change on wetland evolution and its driving process from an integrated perspective of landscape connectivity and fragmentation.

IF 8 2区 环境科学与生态学 Q1 ENVIRONMENTAL SCIENCES
Journal of Environmental Management Pub Date : 2025-08-01 Epub Date: 2025-06-12 DOI:10.1016/j.jenvman.2025.126155
Can Li, Weiqun Lei, Yu Huang, Wenmin Hu
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Abstract

The evolution of wetland ecosystems from the perspectives of landscape connectivity and fragmentation is a critical interdisciplinary topic in contemporary wetland science and landscape ecology. In the context of global warming, the mechanisms by which wetland patches respond to climate change through changes in landscape connectivity and fragmentation require further elucidation. This study introduces an SEMD-XGboost-SHAP ecological modeling framework that systematically examines the evolution of wetland landscape patches and their responses under multiple climate scenarios. The findings indicate: (1) From 2000 to 2022, Permanent water, Marsh, and Flooded flat were the primary drivers of wetland evolution in Dongting Lake. Rapid warming led to a significant reduction in wetlands area, whereas slow warming resulted in a notable increase. (2) At the patch scale, aggregation was the predominant form of wetland evolution, while dissection characterized degradation. Under rapid warming and cooling scenarios, patches underwent significant evolution with connectivity increasing by 9.2 % and 48.63 %, respectively. Conversely, under slow warming and cooling scenarios, patches experienced significant degradation, with fragmentation increasing by 9.75 % and 40.62 %. (3) Annual average maximum temperature was a common factor influencing land type conversion across climate scenarios. In terms of patch evolution, annual average temperature, annual average maximum temperature, minimum temperature, and annual average evapotranspiration were key drivers. Moreover, the interaction between temperature and precipitation played a crucial role in maintaining the stability of wetland patterns. This study provides a foundation for understanding the critical responses of wetland patterns to climate change and offers insights into nature-based solutions for wetland conservation.

景观连通性与破碎化综合视角下气候变化对湿地演化的影响及驱动过程分析
景观连通性与破碎化视角下的湿地生态系统演化是当代湿地科学与景观生态学交叉研究的重要课题。在全球变暖背景下,湿地斑块通过景观连通性和破碎化变化对气候变化的响应机制有待进一步阐明。本研究引入了SEMD-XGboost-SHAP生态模型框架,系统考察了多种气候情景下湿地景观斑块的演变及其响应。结果表明:①2000 - 2022年,洞庭湖湿地演变的主要驱动力为常水、沼泽和泛洪滩;快速变暖导致湿地面积显著减少,而缓慢变暖导致湿地面积显著增加。(2)在斑块尺度上,聚集是湿地演化的主要形式,解剖是退化的主要形式。在快速增温和快速降温情景下,斑块发生显著变化,连通性分别增加9.2%和48.63%。相反,在缓慢增温和变冷情景下,斑块退化明显,破碎度分别增加了9.75%和40.62%。(3)年平均最高气温是各气候情景下影响土地类型转换的共同因子。在斑块演化方面,年平均气温、年平均最高气温、年平均最低气温和年平均蒸散量是主要驱动因子。此外,温度与降水的相互作用对维持湿地格局的稳定性起着至关重要的作用。该研究为理解湿地模式对气候变化的关键响应提供了基础,并为湿地保护提供了基于自然的解决方案。
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
Journal of Environmental Management
Journal of Environmental Management 环境科学-环境科学
CiteScore
13.70
自引率
5.70%
发文量
2477
审稿时长
84 days
期刊介绍: The Journal of Environmental Management is a journal for the publication of peer reviewed, original research for all aspects of management and the managed use of the environment, both natural and man-made.Critical review articles are also welcome; submission of these is strongly encouraged.
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