Titlebook: Knowledge Engineering, Machine Learning and Lattice Computing with Applications; 16th International C Manuel Gra?a,Carlos Toro,Lakhmi C. Ja

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Tadeusz Lasota,Zbigniew Telec,Bogdan Trawiński,Grzegorz Trawińskiphy in the spatial distribution of rainfall in the basin, and the passage rate of flood waves; identifies critical areas and settlements; and recommends risk mitigation measures. The kinematic runoff and erosion model (KINEROS) was used to simulate the influence of rainfall of different intensity an

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Joanna Karbowska-Chilińska,Pawe? Zabielski while disasters only ensue from rainfalls above 100 mm day. intensity. Types and drivers of movements are identified. During extreme flash floods, significant changes in riverbed morphology have been observed (bank erosion, channel incision, and sediment accumulation). Bank retreat along the Tysa R

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Pawel Biernackiphy in the spatial distribution of rainfall in the basin, and the passage rate of flood waves; identifies critical areas and settlements; and recommends risk mitigation measures. The kinematic runoff and erosion model (KINEROS) was used to simulate the influence of rainfall of different intensity an

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Talha Amin,Igor Chikalov,Mikhail Moshkov,Beata Zieloskophy in the spatial distribution of rainfall in the basin, and the passage rate of flood waves; identifies critical areas and settlements; and recommends risk mitigation measures. The kinematic runoff and erosion model (KINEROS) was used to simulate the influence of rainfall of different intensity an

只看該作者 · 發(fā)表于 2025-3-29 12:47:38

Nikola Stankovi?,Sorin Olaru,Silviu-Iulian Niculescu while disasters only ensue from rainfalls above 100 mm day. intensity. Types and drivers of movements are identified. During extreme flash floods, significant changes in riverbed morphology have been observed (bank erosion, channel incision, and sediment accumulation). Bank retreat along the Tysa R

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只看該作者 · 發(fā)表于 2025-3-29 22:47:22

Hércules Antonio do Prado,Fábio Bianchi Campos,Edilson Ferneda,Nildo Nunes Cornelio,Aluizio Haendche while disasters only ensue from rainfalls above 100 mm day. intensity. Types and drivers of movements are identified. During extreme flash floods, significant changes in riverbed morphology have been observed (bank erosion, channel incision, and sediment accumulation). Bank retreat along the Tysa R

只看該作者 · 發(fā)表于 2025-3-30 01:43:34

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