Titlebook: Knowledge Engineering, Machine Learning and Lattice Computing with Applications; 16th International C Manuel Graña,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,Paweł 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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habile

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

diathermy

Nikola Stanković,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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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

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