Quantifying intra- and inter-annual dynamics of river-floodplain connectivity and wetland inundation with remote sensing and wavelet analysis

被引:0
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作者
Zheng, Hanwu [1 ,2 ,6 ]
Tetzlaff, Doerthe [1 ,2 ,3 ]
Freymueller, Jonas [1 ]
Chmieleski, Jana [4 ]
Okujeni, Akpona [2 ,5 ]
Soulsby, Chris [3 ]
机构
[1] Leibniz Inst Freshwater Ecol & Inland Fisheries, Ecohydrol & Biogeochem, Berlin, Germany
[2] Humboldt Univ, Dept Geog, Berlin, Germany
[3] Univ Aberdeen, Northern Rivers Inst, Sch Geosci, Aberdeen, Scotland
[4] Natl Pk Lower Oder Valley, Schwedt, Germany
[5] Humboldt Univ, Integrat Res Inst Transformat Human Environm Syst, Berlin, Germany
[6] Leibniz Inst Freshwater Ecol & Inland Fisheries, Berlin, Germany
关键词
floodplain; Oder river; remote sensing; river-floodplain connectivity; wavelet analysis; wetlands; CLIMATE-CHANGE; CLOUD SHADOW; LAND-USE; WATER; RESTORATION; VEGETATION; TRANSFORM; ALGORITHM; IMPACTS; LEVEL;
D O I
10.1002/hyp.15137
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
We used imagery from remote sensing (FORCE Time Series Analysis submodule (combining Landsat and Sentinel-2 imagery) to derive spatially distributed times series (8 years) of NDWI data to infer patterns of floodplain inundation and river-floodplain connectivity in two contrasting polders in the Lower Oder Valley National Park. The upstream Polder A (14.4 km2) was extensively flooded for prolonged periods most winters. Wavelet analysis showed that this strong seasonality was primarily driven by winter water levels in the river Oder that could enter and leave the polder through two opened floodgates. Subsequent drainage was slow and aided by a pumping station. Inundation of the downstream Polder 10 (17.7km2) was lower and had less marked seasonality. This reflected the impact of flood attenuation by storage in Polder A upstream, but also the greater connectivity (via 10 floodgates) to the Oder and a functional network of channels, which facilitated rapid drainage after flood peaks. In Polder A, secondary periods of transient inundation could also occur in response to local intense summer rainfall. Wavelet analysis also showed that groundwater recharge in and around Polder A is primarily induced by floodwater, whilst Polder 10 also reflects the influence of local rainfall-driven recharge. The flood regimes of the two polders showed marked inter-annual variation, largely dependent on flows from the upper Oder catchment. Understanding these patterns and processes of inundation is important for both managing flows and sustaining valuable wetland habitats within the National Park. Given projected climate change in eastern Europe and possible management alterations to the flow regime of the Oder, the potential implications for these habitats needs urgent attention. Remote sensing products could be reliably used to derive spatially distributed time series of NDWI to map intra and interannual patterns of inundation of the floodplain of the River Oder. Wavelet analysis showed that inundation was strongly seasonal and primarily driven by the winter flood regime of the River Oder, though modulated by the contrasting management strategies of individual polders. Understanding controls on floodplain inundation provides an evidence base for management strategies for wetland conservation in the Lower Oder Valley National Park in the face of threats from climate change and river regulation. image
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页数:16
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