4.7 Article

Spatiotemporal Evolution of Wetland Eco-Hydrological Connectivity in the Poyang Lake Area Based on Long Time-Series Remote Sensing Images

Journal

REMOTE SENSING
Volume 13, Issue 23, Pages -

Publisher

MDPI
DOI: 10.3390/rs13234812

Keywords

wetland; morphological spatial pattern analysis (MSPA); hydrological connectivity composite index; spatial and temporal evolution; Poyang Lake area

Funding

  1. National Natural Science Foundation of China [U1811464]
  2. Major Project of Art Science of the National Social Science Foundation of China [19ZD27]
  3. Cultural Arts and Tourism Research Project [xxhfzzx201907]
  4. Key Projects of the Key R&D plan in Jiangxi Province [20192ACB70014]

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This study used Landsat remote sensing images and land use data to assess wetland hydrological connectivity in the Poyang Lake area using a morphological spatial pattern analysis model. The results showed dramatic changes in wetland landscape area, with the core wetland playing a dominant role in hydrological connectivity. The hydrological connectivity of wetlands in the area has been increasing since 2005, driven by precipitation and large-scale water conservation projects.
Hydrological connectivity is important for maintaining the stability and function of wetland ecosystems. Small-scale hydrological connectivity restricts large-scale hydrological cycle processes. However, long-term evolutionary studies and quantitative evaluation of the hydrological connectivity of wetlands in the Poyang Lake area have not been sufficiently conducted. In this study, we collected 21 Landsat remote sensing images and extracted land use data from 1989 to 2020, introducing a morphological spatial pattern analysis model to assess the wetland hydrological connectivity. A comprehensive method for evaluating the hydrological connectivity of wetlands was established and applied to the Poyang Lake area. The results showed that, over the course of 31 years, the wetland landscape in the Poyang Lake area changed dramatically, and the wetland area has generally shown a decreasing and then increasing trend, among which the core wetland plays a dominant role in the hydrological connectivity of the Poyang Lake area. In addition, the hydrological connectivity decreases as the core wetland area decreases. From 1989 to 2005, the landscape in the Poyang Lake area focused mainly on the transition from wetland to non-wetland. From 2005 to 2020, the conversion of wetland landscape types shows a clear reversal compared to the previous period, showing a predominant shift from non-wetland to wetland landscapes. The eco-hydrological connectivity of the wetlands in the Poyang Lake area from 1989 to 2020 first decreased, and then increased after 2005. In the early stage of the study (1989-2005), we found that the connectivity of 0.3444 in 2005 was the lowest value in the study period. A resolution of 30 m and an edge effect width of 60 m were optimal for studying the hydrological connectivity of wetlands in the Poyang Lake area. The main drivers of the changes in hydrological connectivity were precipitation and the construction of large-scale water conservation projects, as well as changes in land use. This study provides a good basis for assessing hydrological connectivity in a meaningful way, and is expected to provide new insights for maintaining and restoring biodiversity and related ecosystem services in the Poyang Lake area.

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