2013
DOI: 10.1016/j.geomorph.2012.06.020
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Using VHR multispectral remote sensing and LIDAR data to determine the geomorphological effects of overbank flow on a floodplain (the Vistula River, Poland)

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Cited by 38 publications
(27 citation statements)
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“…Wierzbicki et al (2013) used post-flood A. Izumida et al: Application of UAV-SfM photogrammetry and aerial lidar to a disastrous flood aerial lidar data to capture a newly formed crevasse splay of the Vistula River, Poland, but they did not have any pre-flood data to use for topographic comparison. The UAV-based SfM photogrammetric method (UAV-SfM) has basically not been used to examine floodplain topography in the context of a natural disaster, although Tamminga et al (2015b) used it in a fluvial setting to characterize the morphology of a gravelbed river.…”
Section: Introductionmentioning
confidence: 99%
“…Wierzbicki et al (2013) used post-flood A. Izumida et al: Application of UAV-SfM photogrammetry and aerial lidar to a disastrous flood aerial lidar data to capture a newly formed crevasse splay of the Vistula River, Poland, but they did not have any pre-flood data to use for topographic comparison. The UAV-based SfM photogrammetric method (UAV-SfM) has basically not been used to examine floodplain topography in the context of a natural disaster, although Tamminga et al (2015b) used it in a fluvial setting to characterize the morphology of a gravelbed river.…”
Section: Introductionmentioning
confidence: 99%
“…SAR images have also been employed due to their strength that can acquire the data regardless of the weather condition [8][9][10]. In spite of the advantages of those sensors, exploiting very high-resolution (VHR) multi-temporal images is still attractive to detect flood extent for more detail analysis with precise performance [11].…”
Section: Introductionmentioning
confidence: 99%
“…As precipitation was also recorded at the beginning of May 2010, the water retention capacity of the soil was already very limited. Hence, these heavy rainfall events caused serious problems in many lowland areas due to flooding and increased sedimentation rates (Bissolli et al, 2011;Skolasi ska et al, 2014;Wierzbicki et al, 2013). In upland and mountain areas, the rainfall intensified soil erosion and initiated mass movements of soil, with consequent delivery of debris to streams and rivers and damage to infrastructure such as houses, roads and bridges.…”
Section: Extreme Weather Event: Intense Rainfall In May 2010mentioning
confidence: 99%