Results 21 to 30 of about 52,299 (312)

Evaluating Simulated Microphysics of Stratiform and Convective Precipitation in a Squall Line Event Using Polarimetric Radar Observations

Remote Sensing, 2023
Recent upgrades to China’s radar network now allow for polarimetric measurements of convective systems in central China, providing an effective data set with which to evaluate the microphysics schemes employed in local squall line simulations.
Yuting Sun, Zhimin Zhou, Qingjiu Gao, Hongli Li, Minghuan Wang   +4 more
doaj   +1 more source

Prolonged heavy rainfall and land use drive catchment sediment source dynamics: appraisal using multiple biotracers [PDF]

, 2022
Excessive sediment loss degrades freshwater quality and is prone to further elevation and variable source contributions due to the combined effect of extreme rainfall and differing land uses.
Micale, M., Collins, A. L., Upadhayay, H. R., Zhang, Y., Granger, S. J.   +4 more
core   +1 more source

Probabilistic Envelope Curves for Extreme Rainfall Events - Curve Inviluppo Probabilistiche per Precipitazioni Estreme [PDF]

, 2005
A regional envelope curve (REC) of flood flows summarises the current bound on our experience of extreme floods in a region. RECs are available for most regions of the world.
Nicholas C. Matalas, Tagliaferri, Lorenza, Attilio Castellarin, Richard M. Vogel   +3 more
core   +1 more source

Spatial and temporal variability of rainfall erosivity factor for Switzerland [PDF]

, 2011
Rainfall erosivity, considering rainfall amount and intensity, is an important parameter for soil erosion risk assessment under future land use and climate change.
Steel, A., C. Alewell, Panagos, P., L. Montanarella, Montanarella, L., MONTANARELLA Luca, PANAGOS Panagiotis, Alewell, Christine, A. Steel, Meusburger, Katrin, STEEL Alan, K. Meusburger, P. Panagos, MEUSBURGER Katrin, ALEWELL Christine   +14 more
core   +1 more source

Persistent Meteorological Drought in the Yangtze River Basin during Summer–Autumn 2022: Relay Effects of Different Atmospheric Internal Variabilities

Atmosphere, 2023
During the summer–autumn (July–October, Jul–Oct) period of 2022, the Yangtze River Basin (YRB) of China experienced an extreme meteorological drought, with Jul–Oct containing the lowest precipitation in the YRB since 1979.
Ruili Wang, Xiao Li, Hedi Ma, Xing Li, Junchao Wang, Anwei Lai   +5 more
doaj   +1 more source

Heavy Rainfalls [PDF]

Nature, 1898
n ...
openaire   +2 more sources

Consequences to flood management of using different probability distributions to estimate extreme rainfall [PDF]

, 2013
The design of flood defences, such as pumping stations, takes into consideration the predicted return periods of extreme precipitation depths. Most commonly these are estimated by fitting the Generalised Extreme Value (GEV) or the Generalised Pareto (GP)
Esteves, L.S., Luciana S. Esteves
core   +1 more source

Post-Processing Ensemble Precipitation Forecasts and Their Applications in Summer Streamflow Prediction over a Mountain River Basin

Atmosphere, 2023
Ensemble precipitation forecasts (EPFs) can help to extend lead times and provide reliable probabilistic forecasts, which have been widely applied for streamflow predictions by driving hydrological models.
Yiheng Xiang, Yanghe Liu, Xiangxi Zou, Tao Peng, Zhiyuan Yin, Yufeng Ren   +5 more
doaj   +1 more source

philipp-hess/deep-learning-for-heavy-rainfall: v1.0.0

, 2022
No description ...
philipp-hess
core   +1 more source

Anatomy of extraordinary rainfall and flash flood in a Dutch lowland catchment [PDF]

, 2011
On 26 August 2010 the eastern part of The Netherlands and the bordering part of Germany were struck by a series of rainfall events lasting for more than a day.
van der Velde, Y., A. Overeem, Y. van der Velde, Teuling, R., Brauer, C.C., Warmerdam, P. M. M., P. Hazenberg, A. J. Teuling, Van Der Velde, Y.; id_orcid, Overeem, A., Hazenberg, P., C. C. Brauer, Uijlenhoet, R., Brauer, C. C., Warmerdam, P. M.M., Teuling, A. J., Velde, Y., van der, P. M. M. Warmerdam, Warmerdam, P.M.M., van der Velde, Y.,, R. Uijlenhoet   +20 more
core   +1 more source