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Hydrological Extremes in a Warming Climate: Nonstationarity, Uncertainties and Impacts
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This Special Issue comprises 11 papers that outline the advances in research on various aspects of climate change impacts on hydrologic extremes, including both drivers (temperature, precipitation, and snow) and effects (peak flow, low flow, and water temperature). These studies cover a broad range of topics on hydrological extremes, including hydro-climatic controls, trends, homogeneity, nonstationarity, compound events and associated uncertainties, for both historical and future climates.
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Keywords
- annual maximum flow
- Canadian annual maximum flow
- cascade reservoirs
- Climate Change
- climatic controls
- CMIP5
- CMIP6
- coastal flooding
- Colorado River Basin
- compound flooding
- concurrent
- dependence structure
- design flood
- Design Storm
- drought
- equivalent reliability
- Extreme
- extreme events
- extreme precipitation
- Flood
- flood region revision process
- flood-related attribute
- flooding
- functional volume
- Geography
- glacier ablation
- glacier mass balance
- Global warming
- heat wave
- heatwaves
- hydrological extremes
- hydrology
- IHA
- Kelantan
- LARS-WG
- low flows
- Malaysia
- Monte Carlo method
- most likely regional composition
- multi-purpose reservoir
- multiple linear regression
- n/a
- nonstationary conditions
- North Cascade Range
- optimal storage volume
- peak flows
- permafrost region
- predictand
- predictor
- projected IDF curves
- Reference, information & interdisciplinary subjects
- region of influence
- regional flood frequency analysis
- Research & information: general
- retention volume
- riverine flooding
- Salmon
- simulation model
- simulation-optimization model
- Snow
- snow water equivalent
- spatiotemporal changes
- Stephenville Crossing
- streamflow extremes
- SWAT
- transformation of flood discharges
- Trend Analysis
- Trends
- uncertainties
- uncertainty
- variable importance analysis
- Western Canada
- Yakima River basin
Links
DOI: 10.3390/books978-3-0365-4643-8Editions