Titlebook: River Ice Processes and Ice Flood Forecasting; A Guide for Practiti Karl-Erich Lindenschmidt Textbook 20201st edition Springer Nature Switz

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Freeze-Up,ice-cover progression and lastly enters the breakup period. In an ice-jam flood forecasting context, it is important to understand the processes of ice-cover formation and the types of ice that form during freeze-up, since different kinds of ice have different characteristics, particularly their str

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Ice-Cover Breakup and Ice Jamming,d in order to be better prepared for ice-jam flood forecasting. Being able to predict ice-cover breakup provides an indication when ice-jam flood forecasting should commence. This chapter explains ice-cover breakup processes that can lead to ice jamming and ice-jam flooding. Spreadsheet exercises ar

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Remote Sensing,face using means that do not require direct contact with the surface. The information is attained by detecting energy emitted or reflected from the surface; this information is then processed and analysed further to determine particular characteristics of the surface features. These features can be,

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Numerical Modelling of River-Ice Processes (Model Description), if values for the models’ boundary conditions can be projected into the future. This applies to both operational flood forecasting and making predictions on ice-jam flood behaviour in a changed climate in the future. A river-ice model constitutes the core of the stochastic modelling framework used

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Numerical Modelling of River-Ice Processes (Application),tigate a measure to mitigate ice-jam flooding. A modelling exercise is provided at the end of the chapter to expose the reader to setting up RIVICE in a framework that automates multiple runs of the model. The framework is a requirement for Monte Carlo simulations for the stochastic modelling of ice

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Remote Sensing,breakup and helps in the predictions of ice-jam locations and timing. Remote sensing can provide estimates of the volumes of ice that can accumulate in ice jams by detecting the extents of ice covers upstream of potential ice-jam sites.