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In this study, we explored the relationship between changes in surface runoff and changes in landscape pattern in the Keriya River basin, aiming to provide a technical reference for protecting the ecology of the basin. Based on land use/land cover(LULC) data for the study area in five periods(1980,1990, 2000, 2010, and 2020), we extracted landscape pattern index data at the levels of type and landscape. The effects of surface runoff on landscape pattern were then analyzed using ArcGIS and Fragstats 4.2 software, and multi-disciplinary methods including landscape index calculation, Pearson correlation analysis, and Meta analysis. Results show that:(1) From 1980 to 2020, changes in land use type in the basin were clear. Land use consisted primarily of unused land, grassland, and surface water. In 2020, the combined proportion of these three types accounted for 97.79% of the total area, with respective proportions of 75.17%, 20.58%, and 2.04%. The areas of cultivated land and unused land increased by 331.64 km2 and 3 838.09 km2. respectively, while the areas of surface water and grassland decreased respectively, by 1 147.64 km2 and 2 955.13 km2.(2) The areas of three land use types(cultivated land, surface water, and unused land) correlated positively with basin runoff, while areas of the three other land use types(forest land, grassland, and construction land) were negatively correlated with basin runoff. At the landscape level, total edge length(TE), edge density(ED), and landscape shape index(LSI) were positively correlated with basin runoff. Moreover, landscape fragmentation and landscape edge length trended upward during the study period.(3) Meta analysis further verified that basin surface runoff significantly impacted the landscape pattern at both the type level and landscape level.
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Basic Information:
DOI：10.15928/j.1674-3075.202403030059
China Classification Code:P333.1;P901
Citation Information:
[1]Nadira Akbar,Jumeniyaz Seydehmet,Mansur Shabiti.Correlation Analysis of Surface Runoff and Landscape Pattern in the Keriya River Basin[J].Journal of Hydroecology,2026,47(02):1-14.DOI:10.15928/j.1674-3075.202403030059.
Fund Information:
国家自然科学基金（32160319）; 新疆师范大学博士科研启动基金（XJNUBS2017）