Zobrazeno 1 - 10
of 1 283
pro vyhledávání: '"N. Peleg"'
Publikováno v:
Hydrology and Earth System Sciences, Vol 28, Pp 375-389 (2024)
Extreme sub-hourly precipitation, typically convective in nature, is capable of triggering natural disasters such as floods and debris flows. A key component of climate change adaptation and resilience is quantifying the likelihood that sub-hourly ex
Externí odkaz:
https://doaj.org/article/45a8b3aed82b4151bff14e43efe60172
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 23, Pp 1233-1240 (2023)
Floods in urban areas are one of the most common natural hazards. Due to climate change enhancing extreme rainfall and cities becoming larger and denser, the frequency, magnitude, and impact of these events are expected to increase. Pluvial floods ca
Externí odkaz:
https://doaj.org/article/b99e1daf24d6448e9bdf043da4e6f5f3
Publikováno v:
The Cryosphere, Vol 16, Pp 3469-3488 (2022)
Climate projection studies of future changes in snow conditions and resulting rain-on-snow (ROS) flood events are subject to large uncertainties. Typically, emission scenario uncertainties and climate model uncertainties are included. This is the fir
Externí odkaz:
https://doaj.org/article/01585ef20b204854b0dedcdb63d8418d
Autor:
A.M. Fischer, K.M. Strassmann, M. Croci-Maspoli, A.M. Hama, R. Knutti, S. Kotlarski, C. Schär, C. Schnadt Poberaj, N. Ban, M. Bavay, U. Beyerle, D.N. Bresch, S. Brönnimann, P. Burlando, A. Casanueva, S. Fatichi, I. Feigenwinter, E.M. Fischer, M. Hirschi, M.A. Liniger, C. Marty, I. Medhaug, N. Peleg, M. Pickl, C.C. Raible, J. Rajczak, O. Rössler, S.C. Scherrer, C. Schwierz, S.I. Seneviratne, M. Skelton, S.L. Sørland, C. Spirig, F. Tschurr, J. Zeder, E.M. Zubler
Publikováno v:
Climate Services, Vol 26, Iss , Pp 100288- (2022)
To make sound decisions in the face of climate change, government agencies, policymakers and private stakeholders require suitable climate information on local to regional scales. In Switzerland, the development of climate change scenarios is strongl
Externí odkaz:
https://doaj.org/article/76a9d85ecaff4b10bb2061a0b7994ec8
Publikováno v:
Earth Surface Dynamics, Vol 8, Pp 17-36 (2020)
Heavy rainfall is expected to intensify with increasing temperatures, which will likely affect rainfall spatial characteristics. The spatial variability of rainfall can affect streamflow and sediment transport volumes and peaks. Yet, the effect of cl
Externí odkaz:
https://doaj.org/article/d6f12997c9fd498f83bfd6e75815ce8c
Publikováno v:
Journal of Glaciology, Vol 63, Pp 803-822 (2017)
Previous estimates of melt and surface sublimation on glaciers of the subtropical semiarid Andes (29–34°S) have been obtained at few specific locations, but it is not clear how ablation components vary across the entire extent of a glacier in this
Externí odkaz:
https://doaj.org/article/4daa3545347640d6a5663c273a6766bf
Publikováno v:
Hydrology and Earth System Sciences, Vol 21, Pp 5165-5180 (2017)
Spatiotemporal patterns of rainfall are important characteristics that influence runoff generation and flash-flood magnitude and require high-resolution measurements to be adequately represented. This need is further emphasized in arid climates, w
Externí odkaz:
https://doaj.org/article/f99a6e67b61c4220ac2e20ae26383a2c
Publikováno v:
Hydrology and Earth System Sciences, Vol 21, Iss 5, Pp 2389-2404 (2017)
Intensity–duration–frequency (IDF) curves are widely used to quantify the probability of occurrence of rainfall extremes. The usual rain gauge-based approach provides accurate curves for a specific location, but uncertainties arise when ungauged
Externí odkaz:
https://doaj.org/article/1df35415f22b4b32a4b4c4bca5b3bd72
Publikováno v:
Hydrology and Earth System Sciences, Vol 21, Iss 3, Pp 1559-1572 (2017)
The performance of urban drainage systems is typically examined using hydrological and hydrodynamic models where rainfall input is uniformly distributed, i.e., derived from a single or very few rain gauges. When models are fed with a single uniformly
Externí odkaz:
https://doaj.org/article/a1ce76747fd048e68a0533bae21efcfc
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