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230811 ||| eng |
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|a books978-3-0365-4643-8
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|a 9783036546445
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|a 9783036546438
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1 |
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|a Shrestha, Rajesh R.
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| 245 |
0 |
0 |
|a Hydrological Extremes in a Warming Climate
|h Elektronische Ressource
|b Nonstationarity, Uncertainties and Impacts
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| 260 |
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|a Basel
|b MDPI - Multidisciplinary Digital Publishing Institute
|c 2022
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| 300 |
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|a 1 electronic resource (254 p.)
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| 653 |
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|a CMIP5
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| 653 |
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|a peak flows
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| 653 |
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|a region of influence
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| 653 |
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|a Canadian annual maximum flow
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| 653 |
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|a predictand
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|a most likely regional composition
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| 653 |
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|a uncertainties
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| 653 |
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|a CMIP6
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| 653 |
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|a extreme events
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| 653 |
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|a n/a
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| 653 |
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|a Yakima River basin
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| 653 |
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|a SWAT
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| 653 |
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|a compound flooding
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| 653 |
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|a spatiotemporal changes
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| 653 |
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|a climatic controls
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| 653 |
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|a permafrost region
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| 653 |
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|a multi-purpose reservoir
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| 653 |
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|a concurrent
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| 653 |
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|a transformation of flood discharges
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| 653 |
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|a uncertainty
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| 653 |
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|a heat wave
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| 653 |
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|a trends
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| 653 |
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|a snow water equivalent
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| 653 |
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|a dependence structure
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| 653 |
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|a drought
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| 653 |
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|a optimal storage volume
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| 653 |
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|a western Canada
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| 653 |
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|a design flood
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|a simulation model
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| 653 |
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|a Kelantan
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| 653 |
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|a IHA
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| 653 |
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|a Monte Carlo method
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| 653 |
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|a cascade reservoirs
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|a global warming
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| 653 |
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|a annual maximum flow
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| 653 |
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|a equivalent reliability
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| 653 |
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|a extreme precipitation
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| 653 |
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|a simulation-optimization model
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| 653 |
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|a multiple linear regression
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| 653 |
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|a design storm
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| 653 |
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|a LARS-WG
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|a Research & information: general / bicssc
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|a functional volume
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| 653 |
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|a glacier ablation
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| 653 |
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|a Malaysia
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| 653 |
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|a flood region revision process
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|a coastal flooding
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| 653 |
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|a nonstationary conditions
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| 653 |
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|a flood-related attribute
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| 653 |
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|a riverine flooding
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| 653 |
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|a retention volume
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| 653 |
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|a flooding
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|a salmon
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| 653 |
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|a streamflow extremes
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| 653 |
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|a flood
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| 653 |
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|a Colorado River basin
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|a snow
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| 653 |
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|a Stephenville Crossing
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| 653 |
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|a heatwaves
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| 653 |
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|a climate change
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| 653 |
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|a Geography / bicssc
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| 653 |
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|a extreme
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| 653 |
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|a predictor
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| 653 |
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|a trend analysis
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| 653 |
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|a North Cascade Range
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| 653 |
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|a glacier mass balance
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| 653 |
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|a variable importance analysis
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| 653 |
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|a regional flood frequency analysis
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| 653 |
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|a projected IDF curves
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| 653 |
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|a low flows
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| 653 |
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|a hydrology
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| 653 |
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|a hydrological extremes
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| 700 |
1 |
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|a Najafi, Mohammad Reza
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| 700 |
1 |
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|a Shrestha, Rajesh R.
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| 700 |
1 |
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|a Najafi, Mohammad Reza
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| 041 |
0 |
7 |
|a eng
|2 ISO 639-2
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| 989 |
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|b DOAB
|a Directory of Open Access Books
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| 500 |
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|a Creative Commons (cc), https://creativecommons.org/licenses/by/4.0/
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| 028 |
5 |
0 |
|a 10.3390/books978-3-0365-4643-8
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| 856 |
4 |
2 |
|u https://directory.doabooks.org/handle/20.500.12854/97406
|z DOAB: description of the publication
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| 856 |
4 |
0 |
|u https://www.mdpi.com/books/pdfview/book/5960
|7 0
|x Verlag
|3 Volltext
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| 082 |
0 |
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|a 551
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| 082 |
0 |
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|a 551.6
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0 |
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|a 000
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| 082 |
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|a 320
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| 520 |
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|a 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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