Quadratic Response and Adaption of Vegetation Growth to Hydrological Drought in Heterogeneous Lake Floodplain Wetlands
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| Title: | Quadratic Response and Adaption of Vegetation Growth to Hydrological Drought in Heterogeneous Lake Floodplain Wetlands |
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| Authors: | Xuchun Ye, Enxin Yue, Yi Liu, Xianghu Li, Ligang Xu, Chong‐Yu Xu, Chuanzhe Li |
| Source: | Water Resources Research, Vol 61, Iss 11, Pp n/a-n/a (2025) |
| Publisher Information: | Wiley, 2025. |
| Publication Year: | 2025 |
| Collection: | LCC:Environmental sciences |
| Subject Terms: | standardized inundation area index, hydrological drought, quadratic fitting, time‐lag and cumulative effects, heterogeneous lake floodplains, Environmental sciences, GE1-350 |
| Description: | Abstract The growth state and distribution pattern of wetland vegetation are prominently affected by hydrological conditions, but the response and adaption of vegetation growth to hydrological drought in heterogeneous floodplain wetlands remain poorly understood. Given the critical role of eco‐hydrological conditions in lake functions, this study applied multi‐source remote sensing data and image fusion technology to construct continuous high‐spatiotemporal resolution Normalized Difference Water Index (NDWI) (8 days, 30 m) and Enhanced Vegetation Index (EVI) (16 days, 30 m) for the Poyang Lake (China's largest lake floodplain system) from 2000 to 2023. A novel Standardized Inundation Area Index (SIAI) was proposed, and then the responses of wetland vegetation growth to hydrological drought in the lake were quantitatively analyzed. Results revealed that EVI of the Poyang Lake floodplain wetlands exhibited a bimodal pattern throughout the year, with peaks in April and September. SIAI trends indicated a long‐term worsening condition of hydrological drought in the lake. Evident quadratic relationships were identified between EVI and SIAI at both monthly and annual time scales, with a concave fitted curve showing maximum annual EVI at SIAI = −1.46. The impact of hydrological drought on vegetation growth showed a 1–4 months time‐lag effect and a 2–11 months cumulative effect from March to June, though these were potentially interrupted by the summer flooding process. Autumn vegetation growth relied primarily on contemporary lake water conditions. The highlighted quadratic response of vegetation growth to hydrological drought deepens the understanding of floodplain eco‐hydrological adaptability under extreme water regimes. |
| Document Type: | article |
| File Description: | electronic resource |
| Language: | English |
| ISSN: | 1944-7973 0043-1397 |
| Relation: | https://doaj.org/toc/0043-1397; https://doaj.org/toc/1944-7973 |
| DOI: | 10.1029/2025WR040172 |
| Access URL: | https://doaj.org/article/f2aa8093f3704dfc895d5bfa1001e9bd |
| Accession Number: | edsdoj.f2aa8093f3704dfc895d5bfa1001e9bd |
| Database: | Directory of Open Access Journals |
| Abstract: | Abstract The growth state and distribution pattern of wetland vegetation are prominently affected by hydrological conditions, but the response and adaption of vegetation growth to hydrological drought in heterogeneous floodplain wetlands remain poorly understood. Given the critical role of eco‐hydrological conditions in lake functions, this study applied multi‐source remote sensing data and image fusion technology to construct continuous high‐spatiotemporal resolution Normalized Difference Water Index (NDWI) (8 days, 30 m) and Enhanced Vegetation Index (EVI) (16 days, 30 m) for the Poyang Lake (China's largest lake floodplain system) from 2000 to 2023. A novel Standardized Inundation Area Index (SIAI) was proposed, and then the responses of wetland vegetation growth to hydrological drought in the lake were quantitatively analyzed. Results revealed that EVI of the Poyang Lake floodplain wetlands exhibited a bimodal pattern throughout the year, with peaks in April and September. SIAI trends indicated a long‐term worsening condition of hydrological drought in the lake. Evident quadratic relationships were identified between EVI and SIAI at both monthly and annual time scales, with a concave fitted curve showing maximum annual EVI at SIAI = −1.46. The impact of hydrological drought on vegetation growth showed a 1–4 months time‐lag effect and a 2–11 months cumulative effect from March to June, though these were potentially interrupted by the summer flooding process. Autumn vegetation growth relied primarily on contemporary lake water conditions. The highlighted quadratic response of vegetation growth to hydrological drought deepens the understanding of floodplain eco‐hydrological adaptability under extreme water regimes. |
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| ISSN: | 19447973 00431397 |
| DOI: | 10.1029/2025WR040172 |
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