Articles | Volume 23, issue 2
https://doi.org/10.5194/hess-23-989-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-23-989-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
19 Feb 2019
Research article |
| 19 Feb 2019
| 19 Feb 2019
A hybrid stochastic rainfall model that reproduces some important rainfall characteristics at hourly to yearly timescales
Jeongha Park
Department of Civil Engineering, Hongik University, Seoul, 04066,
Republic of Korea
Christian Onof
Department of Civil and Environmental
Engineering, Imperial College, London, SW7 2AZ, UK
Department of Civil Engineering, Hongik University, Seoul, 04066,
Republic of Korea
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Ivan Vorobevskii, Jeongha Park, Dongkyun Kim, Klemens Barfus, and Rico Kronenberg
Hydrol. Earth Syst. Sci., 28, 391–416, https://doi.org/10.5194/hess-28-391-2024, https://doi.org/10.5194/hess-28-391-2024, 2024
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High-resolution precipitation data are often a “must” as input for hydrological and hydraulic models (i.e. urban drainage modelling). However, station or climate projection data usually do not provide the required (e.g. sub-hourly) resolution. In the work, we present two new statistical models of different types to disaggregate precipitation from a daily to a 10 min scale. Both models were validated using radar data and then applied to climate models for 10 stations in Germany and South Korea.
Chi-Ling Wei, Pei-Chun Chen, Chien-Yu Tseng, Ting-Yu Dai, Yun-Ting Ho, Ching-Chun Chou, Christian Onof, and Li-Pen Wang
EGUsphere, https://doi.org/10.5194/egusphere-2024-1918, https://doi.org/10.5194/egusphere-2024-1918, 2024
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pyBL is an open-source package for generating realistic rainfall time series based on the Bartlett-Lewis (BL) model. It can preserve not only standard but also extreme rainfall statistics across various timescales. Notably, compared to traditional frequency analysis methods, the BL model requires only half the record length (or even shorter) to achieve similar consistency in estimating sub-hourly rainfall extremes. This makes it a valuable tool for modelling rainfall extremes with short records.
Chien-Yu Tseng, Li-Pen Wang, and Christian Onof
EGUsphere, https://doi.org/10.5194/egusphere-2024-1540, https://doi.org/10.5194/egusphere-2024-1540, 2024
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This study presents a new algorithm to better model convective storms. We used advanced tracking methods to analyse 165 storm events in Birmingham (UK) and to reconstruct storm cell lifecycles. We found that cell properties like intensity and size are interrelated and vary over time. The new algorithm, based on vine copulas, accurately simulates these properties and their evolution. It also integrates an exponential model for realistic rainfall patterns, enhancing its hydrological applicability.
Ivan Vorobevskii, Jeongha Park, Dongkyun Kim, Klemens Barfus, and Rico Kronenberg
Hydrol. Earth Syst. Sci., 28, 391–416, https://doi.org/10.5194/hess-28-391-2024, https://doi.org/10.5194/hess-28-391-2024, 2024
Short summary
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High-resolution precipitation data are often a “must” as input for hydrological and hydraulic models (i.e. urban drainage modelling). However, station or climate projection data usually do not provide the required (e.g. sub-hourly) resolution. In the work, we present two new statistical models of different types to disaggregate precipitation from a daily to a 10 min scale. Both models were validated using radar data and then applied to climate models for 10 stations in Germany and South Korea.
Abrar Habib, Athanasios Paschalis, Adrian P. Butler, Christian Onof, John P. Bloomfield, and James P. R. Sorensen
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2023-27, https://doi.org/10.5194/hess-2023-27, 2023
Preprint withdrawn
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Components of the hydrological cycle exhibit a “memory” in their behaviour which quantifies how long a variable would stay at high/low values. Being able to model and understand what affects it is vital for an accurate representation of the hydrological elements. In the current work, it is found that rainfall affects the fractal behaviour of groundwater levels, which implies that changes to rainfall due to climate change will change the periods of flood and drought in groundwater-fed catchments.
Judith Marie Pöschmann, Dongkyun Kim, Rico Kronenberg, and Christian Bernhofer
Nat. Hazards Earth Syst. Sci., 21, 1195–1207, https://doi.org/10.5194/nhess-21-1195-2021, https://doi.org/10.5194/nhess-21-1195-2021, 2021
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We examined maximum rainfall values for different durations from 16 years of radar-based rainfall records for whole Germany. Unlike existing observations based on rain gauge data no clear linear relationship could be identified. However, by classifying all time series, we could identify three similar groups determined by the temporal structure of rainfall extremes observed in the study period. The study highlights the importance of using long data records and a dense measurement network.
Christian Onof and Li-Pen Wang
Hydrol. Earth Syst. Sci., 24, 2791–2815, https://doi.org/10.5194/hess-24-2791-2020, https://doi.org/10.5194/hess-24-2791-2020, 2020
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The randomised Bartlett–Lewis (RBL) model is widely used to synthesise rainfall time series with realistic statistical features. However, it tended to underestimate rainfall extremes at sub-hourly and hourly timescales. In this paper, we revisit the derivation of equations that represent rainfall properties and compare statistical estimation methods that impact model calibration. These changes effectively improved the RBL model's capacity to reproduce sub-hourly and hourly rainfall extremes.
David Cross, Christian Onof, Hugo Winter, and Pietro Bernardara
Hydrol. Earth Syst. Sci., 22, 727–756, https://doi.org/10.5194/hess-22-727-2018, https://doi.org/10.5194/hess-22-727-2018, 2018
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Extreme rainfall is one of the most significant natural hazards. However, estimating very large events is highly uncertain. We present a new approach to construct intense rainfall using the structure of rainfall generation in clouds. The method is particularly effective at estimating short-duration extremes, which can be the most damaging. This is expected to have immediate impact for the estimation of very rare downpours, with the potential to improve climate resilience and hazard preparedness.
Waqas Ahmad, Minha Choi, Soohyun Kim, and Dongkyun Kim
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2017-234, https://doi.org/10.5194/nhess-2017-234, 2017
Revised manuscript not accepted
L.-P. Wang, S. Ochoa-Rodríguez, C. Onof, and P. Willems
Hydrol. Earth Syst. Sci., 19, 4001–4021, https://doi.org/10.5194/hess-19-4001-2015, https://doi.org/10.5194/hess-19-4001-2015, 2015
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A new methodology is proposed in this paper, focusing on improving the applicability of the operational weather radar data to urban hydrology with rain gauge data. The proposed methodology employed a simple yet effective technique to extract additional information (called local singularity structure) from radar data, which was generally ignored in related works. The associated improvement can be particularly seen in capturing storm peak magnitudes, which is critical for urban applications.
Z. Zulkafli, W. Buytaert, C. Onof, W. Lavado, and J. L. Guyot
Hydrol. Earth Syst. Sci., 17, 1113–1132, https://doi.org/10.5194/hess-17-1113-2013, https://doi.org/10.5194/hess-17-1113-2013, 2013
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Subject: Hydrometeorology | Techniques and Approaches: Stochastic approaches
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Assessing downscaling techniques for frequency analysis, total precipitation and rainy day estimation in CMIP6 simulations over hydrological years
Simulating sub-hourly rainfall data for current and future periods using two statistical disaggregation models: case studies from Germany and South Korea
Synoptic weather patterns conducive to compound extreme rainfall–wave events in the NW Mediterranean
Exploring the joint probability of precipitation and soil moisture over Europe using copulas
Water cycle changes in Czechia: a multi-source water budget perspective
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A storm-centered multivariate modeling of extreme precipitation frequency based on atmospheric water balance
Probabilistic subseasonal precipitation forecasts using preceding atmospheric intraseasonal signals in a Bayesian perspective
Stochastic daily rainfall generation on tropical islands with complex topography
Modeling seasonal variations of extreme rainfall on different timescales in Germany
Compound flood potential from storm surge and heavy precipitation in coastal China: dependence, drivers, and impacts
Influence of ENSO and tropical Atlantic climate variability on flood characteristics in the Amazon basin
Conditional simulation of spatial rainfall fields using random mixing: a study that implements full control over the stochastic process
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Francesco Serinaldi
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Most studies that aim to identify the impacts of climate change employ general circulation models. However, due to their low spatial resolution, it is necessary to apply downscaling techniques. This work assesses the performance of three methodologies in developing frequency analyses and estimating the number of rainy days and total precipitation per year. Quantile mapping and regression trees excelled in frequency analysis, and the delta method best estimated multiyear total precipitation.
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Hydrol. Earth Syst. Sci., 28, 283–302, https://doi.org/10.5194/hess-28-283-2024, https://doi.org/10.5194/hess-28-283-2024, 2024
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The work presents the first classification of weather types associated to compound events of extreme rainfall and coastal storms. These are found to be characterized by upper-level lows and troughs in conjunction with Mediterranean cyclones, resulting in severe to extreme coastal storms combined with convective systems. We used objective classification methods coupled with a Bayesian Network, testing different variables, domains and number of weather types.
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Hydrol. Earth Syst. Sci., 28, 103–115, https://doi.org/10.5194/hess-28-103-2024, https://doi.org/10.5194/hess-28-103-2024, 2024
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Precipitation and soil moisture have the potential to be jointly used for the modeling of drought conditions. In this research, we analysed how their statistical inter-relationship varies across Europe. We found some clear spatial patterns, especially in the so-called tail dependence (which measures the strength of the relationship for the extreme values). The results suggest that the tail dependence needs to be accounted for to correctly assess the value of joint modeling for drought.
Mijael Rodrigo Vargas Godoy, Yannis Markonis, Oldrich Rakovec, Michal Jenicek, Riya Dutta, Rajani Kumar Pradhan, Zuzana Bešťáková, Jan Kyselý, Roman Juras, Simon Michael Papalexiou, and Martin Hanel
Hydrol. Earth Syst. Sci., 28, 1–19, https://doi.org/10.5194/hess-28-1-2024, https://doi.org/10.5194/hess-28-1-2024, 2024
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The study introduces a novel benchmarking method based on the water cycle budget for hydroclimate data fusion. Using this method and multiple state-of-the-art datasets to assess the spatiotemporal patterns of water cycle changes in Czechia, we found that differences in water availability distribution are dominated by evapotranspiration. Furthermore, while the most significant temporal changes in Czechia occur during spring, the median spatial patterns stem from summer changes in the water cycle.
Yuan Li, Kangning Xü, Zhiyong Wu, Zhiwei Zhu, and Quan J. Wang
Hydrol. Earth Syst. Sci., 27, 4187–4203, https://doi.org/10.5194/hess-27-4187-2023, https://doi.org/10.5194/hess-27-4187-2023, 2023
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A spatial–temporal projection-based calibration, bridging, and merging (STP-CBaM) method is proposed. The calibration model is built by post-processing ECMWF raw forecasts, while the bridging models are built using atmospheric intraseasonal signals as predictors. The calibration model and bridging models are merged through a Bayesian modelling averaging (BMA) method. The results indicate that the newly developed method can generate skilful and reliable sub-seasonal precipitation forecasts.
Hetal P. Dabhi, Mathias W. Rotach, and Michael Oberguggenberger
Hydrol. Earth Syst. Sci., 27, 2123–2147, https://doi.org/10.5194/hess-27-2123-2023, https://doi.org/10.5194/hess-27-2123-2023, 2023
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Spatiotemporally consistent high-resolution precipitation data on climate are needed for climate change impact assessments, but obtaining these data is challenging for areas with complex topography. We present a model that generates synthetic gridded daily precipitation data at a 1 km spatial resolution using observed meteorological station data as input, thereby providing data where historical observations are unavailable. We evaluate this model for a mountainous region in the European Alps.
Yuxin Li, Sisi Chen, Jun Yin, and Xing Yuan
Hydrol. Earth Syst. Sci., 27, 1077–1087, https://doi.org/10.5194/hess-27-1077-2023, https://doi.org/10.5194/hess-27-1077-2023, 2023
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Flash drought is referred to the rapid development of drought events with a fast decline of soil moisture, which has serious impacts on agriculture, the ecosystem, human health, and society. While flash droughts have received much research attention, there is no consensus on its definition. Here we used a stochastic water balance framework to quantify the timing of soil moisture crossing different thresholds, providing an efficient tool for diagnosing and monitoring flash droughts.
Arun Ramanathan, Pierre-Antoine Versini, Daniel Schertzer, Remi Perrin, Lionel Sindt, and Ioulia Tchiguirinskaia
Hydrol. Earth Syst. Sci., 26, 6477–6491, https://doi.org/10.5194/hess-26-6477-2022, https://doi.org/10.5194/hess-26-6477-2022, 2022
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Reference rainfall scenarios are indispensable for hydrological applications such as designing storm-water management infrastructure, including green roofs. Therefore, a new method is suggested for simulating rainfall scenarios of specified intensity, duration, and frequency, with realistic intermittency. Furthermore, novel comparison metrics are proposed to quantify the effectiveness of the presented simulation procedure.
Judith Meyer, Malte Neuper, Luca Mathias, Erwin Zehe, and Laurent Pfister
Hydrol. Earth Syst. Sci., 26, 6163–6183, https://doi.org/10.5194/hess-26-6163-2022, https://doi.org/10.5194/hess-26-6163-2022, 2022
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We identified and analysed the major atmospheric components of rain-intense thunderstorms that can eventually lead to flash floods: high atmospheric moisture, sufficient latent instability, and weak thunderstorm cell motion. Between 1981 and 2020, atmospheric conditions became likelier to support strong thunderstorms. However, the occurrence of extreme rainfall events as well as their rainfall intensity remained mostly unchanged.
Yuan Liu and Daniel B. Wright
Hydrol. Earth Syst. Sci., 26, 5241–5267, https://doi.org/10.5194/hess-26-5241-2022, https://doi.org/10.5194/hess-26-5241-2022, 2022
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We present a new approach to estimate extreme rainfall probability and severity using the atmospheric water balance, where precipitation is the sum of water vapor components moving in and out of a storm. We apply our method to the Mississippi Basin and its five major subbasins. Our approach achieves a good fit to reference precipitation, indicating that the rainfall probability estimation can benefit from additional information from physical processes that control rainfall.
Yuan Li, Zhiyong Wu, Hai He, and Hao Yin
Hydrol. Earth Syst. Sci., 26, 4975–4994, https://doi.org/10.5194/hess-26-4975-2022, https://doi.org/10.5194/hess-26-4975-2022, 2022
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The relationship between atmospheric intraseasonal signals and precipitation is highly uncertain and depends on the region and lead time. In this study, we develop a spatiotemporal projection, based on a Bayesian hierarchical model (STP-BHM), to address the above challenge. The results suggest that the STP-BHM model is skillful and reliable for probabilistic subseasonal precipitation forecasts over China during the boreal summer monsoon season.
Lionel Benoit, Lydie Sichoix, Alison D. Nugent, Matthew P. Lucas, and Thomas W. Giambelluca
Hydrol. Earth Syst. Sci., 26, 2113–2129, https://doi.org/10.5194/hess-26-2113-2022, https://doi.org/10.5194/hess-26-2113-2022, 2022
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This study presents a probabilistic model able to reproduce the spatial patterns of rainfall on tropical islands with complex topography. It sheds new light on rainfall variability at the island scale, and explores the links between rainfall patterns and atmospheric circulation. The proposed model has been tested on two islands of the tropical Pacific, and demonstrates good skills in simulating both site-specific and island-scale rain behavior.
Jana Ulrich, Felix S. Fauer, and Henning W. Rust
Hydrol. Earth Syst. Sci., 25, 6133–6149, https://doi.org/10.5194/hess-25-6133-2021, https://doi.org/10.5194/hess-25-6133-2021, 2021
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The characteristics of extreme precipitation on different timescales as well as in different seasons are relevant information, e.g., for designing hydrological structures or managing water supplies. Therefore, our aim is to describe these characteristics simultaneously within one model. We find similar characteristics for short extreme precipitation at all considered stations in Germany but pronounced regional differences with respect to the seasonality of long-lasting extreme events.
Jiayi Fang, Thomas Wahl, Jian Fang, Xun Sun, Feng Kong, and Min Liu
Hydrol. Earth Syst. Sci., 25, 4403–4416, https://doi.org/10.5194/hess-25-4403-2021, https://doi.org/10.5194/hess-25-4403-2021, 2021
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A comprehensive assessment of compound flooding potential is missing for China. We investigate dependence, drivers, and impacts of storm surge and precipitation for coastal China. Strong dependence exists between driver combinations, with variations of seasons and thresholds. Sea level rise escalates compound flood potential. Meteorology patterns are pronounced for low and high compound flood potential. Joint impacts from surge and precipitation were much higher than from each individually.
Jamie Towner, Andrea Ficchí, Hannah L. Cloke, Juan Bazo, Erin Coughlan de Perez, and Elisabeth M. Stephens
Hydrol. Earth Syst. Sci., 25, 3875–3895, https://doi.org/10.5194/hess-25-3875-2021, https://doi.org/10.5194/hess-25-3875-2021, 2021
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We examine whether several climate indices alter the magnitude, timing and duration of floods in the Amazon. We find significant changes in both flood magnitude and duration, particularly in the north-eastern Amazon for negative SST years in the central Pacific Ocean. This response is not repeated when the negative anomaly is positioned further east. These results have important implications for both social and physical sectors working towards the improvement of flood early warning systems.
Jieru Yan, Fei Li, András Bárdossy, and Tao Tao
Hydrol. Earth Syst. Sci., 25, 3819–3835, https://doi.org/10.5194/hess-25-3819-2021, https://doi.org/10.5194/hess-25-3819-2021, 2021
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Accurate spatial precipitation estimates are important in various fields. An approach to simulate spatial rainfall fields conditioned on radar and rain gauge data is proposed. Unlike the commonly used Kriging methods, which provide a Kriged mean field, the output of the proposed approach is an ensemble of estimates that represents the estimation uncertainty. The approach is robust to nonlinear error in radar estimates and is shown to have some advantages, especially when estimating the extremes.
Hossein Tabari, Santiago Mendoza Paz, Daan Buekenhout, and Patrick Willems
Hydrol. Earth Syst. Sci., 25, 3493–3517, https://doi.org/10.5194/hess-25-3493-2021, https://doi.org/10.5194/hess-25-3493-2021, 2021
Sebastian Scher and Stefanie Peßenteiner
Hydrol. Earth Syst. Sci., 25, 3207–3225, https://doi.org/10.5194/hess-25-3207-2021, https://doi.org/10.5194/hess-25-3207-2021, 2021
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In hydrology, it is often necessary to infer from a daily sum of precipitation a possible distribution over the day – for example how much it rained in each hour. In principle, for a given daily sum, there are endless possibilities. However, some are more likely than others. We show that a method from artificial intelligence called generative adversarial networks (GANs) can
learnwhat a typical distribution over the day looks like.
Jun Li, Zhaoli Wang, Xushu Wu, Jakob Zscheischler, Shenglian Guo, and Xiaohong Chen
Hydrol. Earth Syst. Sci., 25, 1587–1601, https://doi.org/10.5194/hess-25-1587-2021, https://doi.org/10.5194/hess-25-1587-2021, 2021
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We introduce a daily-scale index, termed the standardized compound drought and heat index (SCDHI), to measure the key features of compound dry-hot conditions. SCDHI can not only monitor the long-term compound dry-hot events, but can also capture such events at sub-monthly scale and reflect the related vegetation activity impacts. The index can provide a new tool to quantify sub-monthly characteristics of compound dry-hot events, which are vital for releasing early and timely warning.
Damien Raynaud, Benoit Hingray, Guillaume Evin, Anne-Catherine Favre, and Jérémy Chardon
Hydrol. Earth Syst. Sci., 24, 4339–4352, https://doi.org/10.5194/hess-24-4339-2020, https://doi.org/10.5194/hess-24-4339-2020, 2020
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This research paper proposes a weather generator combining two sampling approaches. A first generator recombines large-scale atmospheric situations. A second generator is applied to these atmospheric trajectories in order to simulate long time series of daily regional precipitation and temperature. The method is applied to daily time series in Switzerland. It reproduces adequately the observed climatology and improves the reproduction of extreme precipitation values.
Marc Schleiss
Hydrol. Earth Syst. Sci., 24, 3699–3723, https://doi.org/10.5194/hess-24-3699-2020, https://doi.org/10.5194/hess-24-3699-2020, 2020
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A new way to downscale rainfall fields based on the notion of equal-volume areas (EVAs) is proposed. Experiments conducted on 100 rainfall events in the Netherlands show that the EVA method outperforms classical methods based on fixed grid cell sizes, producing fields with more realistic spatial structures. The main novelty of the method lies in its adaptive sampling strategy, which avoids many of the mathematical challenges associated with the presence of zero rainfall values.
Christian Onof and Li-Pen Wang
Hydrol. Earth Syst. Sci., 24, 2791–2815, https://doi.org/10.5194/hess-24-2791-2020, https://doi.org/10.5194/hess-24-2791-2020, 2020
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The randomised Bartlett–Lewis (RBL) model is widely used to synthesise rainfall time series with realistic statistical features. However, it tended to underestimate rainfall extremes at sub-hourly and hourly timescales. In this paper, we revisit the derivation of equations that represent rainfall properties and compare statistical estimation methods that impact model calibration. These changes effectively improved the RBL model's capacity to reproduce sub-hourly and hourly rainfall extremes.
Lionel Benoit, Mathieu Vrac, and Gregoire Mariethoz
Hydrol. Earth Syst. Sci., 24, 2841–2854, https://doi.org/10.5194/hess-24-2841-2020, https://doi.org/10.5194/hess-24-2841-2020, 2020
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At subdaily resolution, rain intensity exhibits a strong variability in space and time due to the diversity of processes that produce rain (e.g., frontal storms, mesoscale convective systems and local convection). In this paper we explore a new method to simulate rain type time series conditional to meteorological covariates. Afterwards, we apply stochastic rain type simulation to the downscaling of precipitation of a regional climate model.
Jieru Yan, András Bárdossy, Sebastian Hörning, and Tao Tao
Hydrol. Earth Syst. Sci., 24, 2287–2301, https://doi.org/10.5194/hess-24-2287-2020, https://doi.org/10.5194/hess-24-2287-2020, 2020
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For applications such as flood forecasting of urban- or town-scale distributed hydrological modeling, high-resolution quantitative precipitation estimation (QPE) with enough accuracy is the most important driving factor and thus the focus of this paper. Considering the fact that rain gauges are sparse but accurate and radar-based precipitation estimates are inaccurate but densely distributed, we are merging the two types of data intellectually to obtain accurate QPEs with high resolution.
Eva Steirou, Lars Gerlitz, Heiko Apel, Xun Sun, and Bruno Merz
Hydrol. Earth Syst. Sci., 23, 1305–1322, https://doi.org/10.5194/hess-23-1305-2019, https://doi.org/10.5194/hess-23-1305-2019, 2019
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We investigate whether flood probabilities in Europe vary for different large-scale atmospheric circulation conditions. Maximum seasonal river flows from 600 gauges in Europe and five synchronous atmospheric circulation indices are analyzed. We find that a high percentage of stations is influenced by at least one of the climate indices, especially during winter. These results can be useful for preparedness and damage planning by (re-)insurance companies.
Florian Ehmele and Michael Kunz
Hydrol. Earth Syst. Sci., 23, 1083–1102, https://doi.org/10.5194/hess-23-1083-2019, https://doi.org/10.5194/hess-23-1083-2019, 2019
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The risk estimation of precipitation events with high recurrence periods is difficult due to the limited timescale with meteorological observations and an inhomogeneous distribution of rain gauges, especially in mountainous terrains. In this study a spatially high resolved analytical model, designed for stochastic simulations of flood-related precipitation, is developed and applied to an investigation area in Germany but is transferable to other areas. High conformity with observations is found.
Juliette Blanchet, Emmanuel Paquet, Pradeebane Vaittinada Ayar, and David Penot
Hydrol. Earth Syst. Sci., 23, 829–849, https://doi.org/10.5194/hess-23-829-2019, https://doi.org/10.5194/hess-23-829-2019, 2019
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We propose an objective framework for estimating rainfall cumulative distribution functions in a region when data are only available at rain gauges. Our methodology allows us to assess goodness-of-fit of the full distribution, but with a particular focus on its tail. It is applied to daily rainfall in the Ardèche catchment in the south of France. Results show a preference for a mixture of Gamma distribution over seasons and weather patterns, with parameters interpolated with a thin plate spline.
Diana Lucatero, Henrik Madsen, Jens C. Refsgaard, Jacob Kidmose, and Karsten H. Jensen
Hydrol. Earth Syst. Sci., 22, 6591–6609, https://doi.org/10.5194/hess-22-6591-2018, https://doi.org/10.5194/hess-22-6591-2018, 2018
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The present study evaluates the skill of a seasonal forecasting system for hydrological relevant variables in Denmark. Linear scaling and quantile mapping were used to correct the forecasts. Uncorrected forecasts tend to be more skillful than climatology, in general, for the first month lead time only. Corrected forecasts show a reduced bias in the mean; are more consistent; and show a level of accuracy that is closer to, although no higher than, that of ensemble climatology, in general.
Kuganesan Sivasubramaniam, Ashish Sharma, and Knut Alfredsen
Hydrol. Earth Syst. Sci., 22, 6533–6546, https://doi.org/10.5194/hess-22-6533-2018, https://doi.org/10.5194/hess-22-6533-2018, 2018
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This study investigates the use of gauge precipitation and air temperature observations to ascertain radar precipitation in cold climates. The use of air temperature as an additional variable in a non-parametric model improved the estimation of radar precipitation significantly. Further, it was found that the temperature effects became insignificant when air temperature was above 10 °C. The findings from this study could be important for using radar precipitation for hydrological applications.
Lionel Benoit, Mathieu Vrac, and Gregoire Mariethoz
Hydrol. Earth Syst. Sci., 22, 5919–5933, https://doi.org/10.5194/hess-22-5919-2018, https://doi.org/10.5194/hess-22-5919-2018, 2018
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We propose a method for unsupervised classification of the space–time–intensity structure of weather radar images. The resulting classes are interpreted as rain types, i.e. pools of rain fields with homogeneous statistical properties. Rain types can in turn be used to define stationary periods for further stochastic rainfall modelling. The application of rain typing to real data indicates that non-stationarity can be significant within meteorological seasons, and even within a single storm.
Hannes Müller-Thomy, Markus Wallner, and Kristian Förster
Hydrol. Earth Syst. Sci., 22, 5259–5280, https://doi.org/10.5194/hess-22-5259-2018, https://doi.org/10.5194/hess-22-5259-2018, 2018
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Rainfall time series are disaggregated from daily to hourly values to be used for rainfall–runoff modeling of mesoscale catchments. Spatial rainfall consistency is implemented afterwards using simulated annealing. With the calibration process applied, observed runoff statistics (e.g., summer and winter peak flows) are represented well. However, rainfall datasets with under- or over-estimation of spatial consistency lead to similar results, so the need for a good representation can be questioned.
Xinjun Tu, Yiliang Du, Vijay P. Singh, Xiaohong Chen, Kairong Lin, and Haiou Wu
Hydrol. Earth Syst. Sci., 22, 5175–5189, https://doi.org/10.5194/hess-22-5175-2018, https://doi.org/10.5194/hess-22-5175-2018, 2018
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For given frequencies of precipitation of a large region, design water demands of irrigation of the entire region among three methods, i.e., equalized frequency, typical year and most-likely weight function, slightly differed, but their alterations in sub-regions were complicated. A design procedure using the most-likely weight function in association with a high-dimensional copula, which built a linkage between regional frequency and sub-regional frequency of precipitation, is recommended.
A. T. M. Sakiur Rahman, M. Shakil Ahmed, Hasnat Mohammad Adnan, Mohammad Kamruzzaman, M. Abdul Khalek, Quamrul Hasan Mazumder, and Chowdhury Sarwar Jahan
Hydrol. Earth Syst. Sci., 22, 4213–4228, https://doi.org/10.5194/hess-22-4213-2018, https://doi.org/10.5194/hess-22-4213-2018, 2018
Edmund P. Meredith, Henning W. Rust, and Uwe Ulbrich
Hydrol. Earth Syst. Sci., 22, 4183–4200, https://doi.org/10.5194/hess-22-4183-2018, https://doi.org/10.5194/hess-22-4183-2018, 2018
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Kilometre-scale climate-model data are of great benefit to both hydrologists and end users studying extreme precipitation, though often unavailable due to the computational expense associated with such high-resolution simulations. We develop a method which identifies days with enhanced risk of extreme rainfall over a catchment, so that high-resolution simulations can be performed only when such a risk exists, reducing computational expense by over 90 % while still well capturing the extremes.
Diana Lucatero, Henrik Madsen, Jens C. Refsgaard, Jacob Kidmose, and Karsten H. Jensen
Hydrol. Earth Syst. Sci., 22, 3601–3617, https://doi.org/10.5194/hess-22-3601-2018, https://doi.org/10.5194/hess-22-3601-2018, 2018
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The skill of an experimental streamflow forecast system in the Ahlergaarde catchment, Denmark, is analyzed. Inputs to generate the forecasts are taken from the ECMWF System 4 seasonal forecasting system and an ensemble of observations (ESP). Reduction of biases is achieved by processing the meteorological and/or streamflow forecasts. In general, this is not sufficient to ensure a higher level of accuracy than the ESP, indicating a modest added value of a seasonal meteorological system.
Sanjeev K. Jha, Durga L. Shrestha, Tricia A. Stadnyk, and Paulin Coulibaly
Hydrol. Earth Syst. Sci., 22, 1957–1969, https://doi.org/10.5194/hess-22-1957-2018, https://doi.org/10.5194/hess-22-1957-2018, 2018
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The output from numerical weather prediction (NWP) models is known to have errors. River forecast centers in Canada mostly use precipitation forecasts directly obtained from American and Canadian NWP models. In this study, we evaluate the forecast performance of ensembles generated by a Bayesian post-processing approach in cold climates. We demonstrate that the post-processing approach generates bias-free forecasts and provides a better picture of uncertainty in the case of an extreme event.
Md Abul Ehsan Bhuiyan, Efthymios I. Nikolopoulos, Emmanouil N. Anagnostou, Pere Quintana-Seguí, and Anaïs Barella-Ortiz
Hydrol. Earth Syst. Sci., 22, 1371–1389, https://doi.org/10.5194/hess-22-1371-2018, https://doi.org/10.5194/hess-22-1371-2018, 2018
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This study investigates the use of a nonparametric model for combining multiple global precipitation datasets and characterizing estimation uncertainty. Inputs to the model included three satellite precipitation products, an atmospheric reanalysis precipitation dataset, satellite-derived near-surface daily soil moisture data, and terrain elevation. We evaluated the technique based on high-resolution reference precipitation data and further used generated ensembles to force a hydrological model.
David Cross, Christian Onof, Hugo Winter, and Pietro Bernardara
Hydrol. Earth Syst. Sci., 22, 727–756, https://doi.org/10.5194/hess-22-727-2018, https://doi.org/10.5194/hess-22-727-2018, 2018
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Extreme rainfall is one of the most significant natural hazards. However, estimating very large events is highly uncertain. We present a new approach to construct intense rainfall using the structure of rainfall generation in clouds. The method is particularly effective at estimating short-duration extremes, which can be the most damaging. This is expected to have immediate impact for the estimation of very rare downpours, with the potential to improve climate resilience and hazard preparedness.
Jérémy Chardon, Benoit Hingray, and Anne-Catherine Favre
Hydrol. Earth Syst. Sci., 22, 265–286, https://doi.org/10.5194/hess-22-265-2018, https://doi.org/10.5194/hess-22-265-2018, 2018
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We present a two-stage statistical downscaling model for the probabilistic prediction of local precipitation, where the downscaling statistical link is estimated from atmospheric circulation analogs of the current prediction day.
The model allows for a day-to-day adaptive and tailored downscaling. It can reveal specific predictors for peculiar and non-frequent weather configurations. This approach noticeably improves the skill of the prediction for both precipitation occurrence and quantity.
Christoph Ritschel, Uwe Ulbrich, Peter Névir, and Henning W. Rust
Hydrol. Earth Syst. Sci., 21, 6501–6517, https://doi.org/10.5194/hess-21-6501-2017, https://doi.org/10.5194/hess-21-6501-2017, 2017
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A stochastic model for precipitation is used to simulate an observed precipitation series; it is compared to the original series in terms of intensity–duration frequency curves. Basis for the latter curves is a parametric model for the duration dependence of the underlying extreme value model allowing a consistent estimation of one single duration-dependent distribution using all duration series simultaneously. The stochastic model reproduces the curves except for very rare extreme events.
Poulomi Ganguli and Paulin Coulibaly
Hydrol. Earth Syst. Sci., 21, 6461–6483, https://doi.org/10.5194/hess-21-6461-2017, https://doi.org/10.5194/hess-21-6461-2017, 2017
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Using statistical models, we test whether nonstationary versus stationary models show any significant differences in terms of design storm intensity at different durations across Southern Ontario. We find that detectable nonstationarity in rainfall extremes does not necessarily lead to significant differences in design storm intensity, especially for shorter return periods. An update of 2–44 % is required in current design standards to mitigate the risk of storm-induced urban flooding.
Daniele Nerini, Nikola Besic, Ioannis Sideris, Urs Germann, and Loris Foresti
Hydrol. Earth Syst. Sci., 21, 2777–2797, https://doi.org/10.5194/hess-21-2777-2017, https://doi.org/10.5194/hess-21-2777-2017, 2017
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Stochastic generators are effective tools for the quantification of uncertainty in a number of applications with weather radar data, including quantitative precipitation estimation and very short-term forecasting. However, most of the current stochastic rainfall field generators cannot handle spatial non-stationarity. We propose an approach based on the short-space Fourier transform, which aims to reproduce the local spatial structure of the observed rainfall fields.
Tobias Mosthaf and András Bárdossy
Hydrol. Earth Syst. Sci., 21, 2463–2481, https://doi.org/10.5194/hess-21-2463-2017, https://doi.org/10.5194/hess-21-2463-2017, 2017
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Parametric distribution functions are commonly used to model precipitation amounts at gauged and ungauged locations. Nonparametric distributions offer a more flexible way to model precipitation amounts. However, the nonparametric models do not exhibit parameters that can be easily regionalized for application at ungauged locations. To overcome this deficiency, we present a new interpolation scheme for nonparametric models and evaluate the usage of daily gauges for sub-daily resolutions.
Claudia Volosciuk, Douglas Maraun, Mathieu Vrac, and Martin Widmann
Hydrol. Earth Syst. Sci., 21, 1693–1719, https://doi.org/10.5194/hess-21-1693-2017, https://doi.org/10.5194/hess-21-1693-2017, 2017
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For impact modeling, infrastructure design, or adaptation strategy planning, high-quality climate data on the point scale are often demanded. Due to the scale gap between gridbox and point scale and biases in climate models, we combine a statistical bias correction and a stochastic downscaling model and apply it to climate model-simulated precipitation. The method performs better in summer than in winter and in winter best for mild winter climate (Mediterranean) and worst for continental winter.
Aline Murawski, Gerd Bürger, Sergiy Vorogushyn, and Bruno Merz
Hydrol. Earth Syst. Sci., 20, 4283–4306, https://doi.org/10.5194/hess-20-4283-2016, https://doi.org/10.5194/hess-20-4283-2016, 2016
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To understand past flood changes in the Rhine catchment and the role of anthropogenic climate change in extreme flows, an attribution study relying on a proper GCM (general circulation model) downscaling is needed. A downscaling based on conditioning a stochastic weather generator on weather patterns is a promising approach. Here the link between patterns and local climate is tested, and the skill of GCMs in reproducing these patterns is evaluated.
Kue Bum Kim, Hyun-Han Kwon, and Dawei Han
Hydrol. Earth Syst. Sci., 20, 2019–2034, https://doi.org/10.5194/hess-20-2019-2016, https://doi.org/10.5194/hess-20-2019-2016, 2016
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A primary advantage of using model ensembles for climate change impact studies is to represent the uncertainties associated with models through the ensemble spread. Currently, most of the conventional bias correction methods adjust all the ensemble members to one reference observation. As a result, the ensemble spread is degraded during bias correction. However the proposed method is able to correct the bias and conform to the ensemble spread so that the ensemble information can be better used.
E. P. Maurer, D. L. Ficklin, and W. Wang
Hydrol. Earth Syst. Sci., 20, 685–696, https://doi.org/10.5194/hess-20-685-2016, https://doi.org/10.5194/hess-20-685-2016, 2016
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To translate climate model output from its native coarse scale to a finer scale more representative of that at which societal impacts are experienced, a common method applied is statistical downscaling. A component of many statistical downscaling techniques is quantile mapping (QM). QM can be applied at different spatial scales, and here we study how skill varies with spatial scale. We find the highest skill is generally obtained when applying QM at approximately a 50 km spatial scale.
S. Sadri, J. Kam, and J. Sheffield
Hydrol. Earth Syst. Sci., 20, 633–649, https://doi.org/10.5194/hess-20-633-2016, https://doi.org/10.5194/hess-20-633-2016, 2016
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Low flows are a critical part of the river flow regime but little is known about how they are changing in response to human influences and climate. We analyzed low flow records across the eastern US and identified sites that were minimally influenced by human activities. We found a general increasing trend in low flows across the northeast and decreasing trend across the southeast that are likely driven by changes in climate. The results have implications for how we manage our water resources.
Cited articles
Austin, P. M. and Houze Jr., R. A.: Analysis of the structure of
precipitation patterns in New England, J. Appl. Meteorol., 11, 926–935,
1972.
Benoit, L., Allard, D., and Mariethoz, G.: Stochastic Rainfall Modelling at
Sub-Kilometer Scale, Water Resour. Res., https://doi.org/10.1029/2018WR022817, 2018.
Bo, Z., Islam, S., and Eltahir, E.: Aggregation-disaggregation properties of
a stochastic rainfall model, Water Resour. Res., 30, 3423–3435, 1994.
Borgogno, F., D'Odorico, P., Laio, F., and Ridolfi, L.: Effect of rainfall
interannual variability on the stability and resilience of dryland plant
ecosystems, Water Resour. Res., 43, https://doi.org/10.1029/2006WR005314, 2007.
Burton, A., Kilsby, C., Fowler, H., Cowpertwait, P., and O'Connell, P.:
RainSim: A spatial–temporal stochastic rainfall modelling system, Environ.
Modell. Softw., 23, 1356–1369, 2008.
Burton, A., Fowler, H., Blenkinsop, S., and Kilsby, C.: Downscaling transient
climate change using a Neyman–Scott Rectangular Pulses stochastic rainfall
model, J. Hydrol., 381, 18–32, 2010.
Cameron, D., Beven, K., and Naden, P.: Flood frequency estimation by
continuous simulation under climate change (with uncertainty), Hydrol. Earth
Syst. Sci., 4, 393–405, https://doi.org/10.5194/hess-4-393-2000,
2000.
Cho, H., Kim, D., Olivera, F., and Guikema, S. D.: Enhanced speciation in
particle swarm optimization for multi-modal problems, Eur. J. Oper. Res.,
213, 15–23, 2011.
Cowpertwait, P. S.: Further developments of the Neyman-Scott clustered point
process for modeling rainfall, Water Resour. Res., 27, 1431–1438, 1991.
Cowpertwait, P. S.: A Poisson-cluster model of rainfall: some high-order
moments and extreme values, P. Roy. Soc. A-Math. Phy., https://doi.org/10.1098/rspa.1998.0191, 1998.
Cowpertwait, P., Isham, V., and Onof, C.: Point process models of rainfall:
developments for fine-scale structure, P. Roy. Soc. A-Math. Phy.,
https://doi.org/10.1098/rspa.2007.1889, 2007.
Cross, D., Onof, C., Winter, H., and Bernardara, P.: Censored rainfall
modelling for estimation of fine-scale extremes, Hydrol. Earth Syst. Sci.,
22, 727–756, https://doi.org/10.5194/hess-22-727-2018, 2018.
Delleur, J. W. and Kavvas, M. L.: Stochastic models for monthly rainfall
forecasting and synthetic generation, J. Appl. Meteorol., 17, 1528–1536,
1978.
Derzekos, C., Koutsoyiannis, D., and Onof, C.: A new randomised Poisson
cluster model for rainfall in time, Enrgy. Proced., https://doi.org/10.13140/RG.2.2.32544.38403, 2005.
Dimitriadis, P. and Koutsoyiannis, D.: Climacogram versus autocovariance and
power spectrum in stochastic modelling for Markovian and Hurst–Kolmogorov
processes, Stoch. Env. Res. Risk A., 29, 1649–1669, 2015.
Dimitriadis, P. and Koutsoyiannis, D.: Stochastic synthesis approximating any
process dependence and distribution, Stoch. Env. Res. Risk A., 32,
1493–1515, 2018.
Efstratiadis, A., Dialynas, Y. G., Kozanis, S., and Koutsoyiannis, D.: A
multivariate stochastic model for the generation of synthetic time series at
multiple time scales reproducing long-term persistence, Environ. Modell.
Softw., 62, 139–152, 2014.
Entekhabi, D., Rodriguez-Iturbe, I., and Eagleson, P. S.: Probabilistic
representation of the temporal rainfall process by a modified Neyman-Scott
Rectangular Pulses Model: Parameter estimation and validation, Water Resour.
Res., 25, 295–302, 1989.
Faramarzi, M., Abbaspour, K. C., Schulin, R., and Yang, H.: Modelling blue
and green water resources availability in Iran, Hydrol. Process., 23,
486–501, 2009.
Fatichi, S., Ivanov, V. Y., and Caporali, E.: Simulation of future climate
scenarios with a weather generator, Adv. Water Resour., 34, 448–467, 2011.
Fernandez-Illescas, C. P. and Rodriguez-Iturbe, I.: The impact of interannual
rainfall variability on the spatial and temporal patterns of vegetation in a
water-limited ecosystem, Adv. Water Resour., 27, 83–95, 2004.
Furrer, E. M. and Katz, R. W.: Improving the simulation of extreme
precipitation events by stochastic weather generators, Water Resour. Res.,
44, https://doi.org/10.1029/2008WR007316, 2008.
Glasbey, C., Cooper, G., and McGechan, M.: Disaggregation of daily rainfall
by conditional simulation from a point-process model, J. Hydrol., 165, 1–9,
1995.
Gyasi-Agyei, Y.: Identification of regional parameters of a stochastic model
for rainfall disaggregation, J. Hydrol., 223, 148–163, 1999.
Gyasi-Agyei, Y. and Willgoose, G. R.: A hybrid model for point rainfall
modeling, Water Resour. Res., 33, 1699–1706, 1997.
Iliopoulou, T., Papalexiou, S. M., Markonis, Y., and Koutsoyiannis, D.:
Revisiting long-range dependence in annual precipitation, J. Hydrol., https://doi.org/10.1016/j.jhydrol.2016.04.015, 2016.
Islam, S., Entekhabi, D., Bras, R., and Rodriguez-Iturbe, I.: Parameter
estimation and sensitivity analysis for the modified Bartlett-Lewis
rectangular pulses model of rainfall, J. Geophys. Res-Atmos., 95, 2093–2100,
1990.
Kaczmarska, J., Isham, V., and Onof, C.: Point process models for
fine-resolution rainfall, Hydrolog. Sci. J., 59, 1972–1991, 2014.
Kaczmarska, J. M., Isham, V. S., and Northrop, P.: Local generalised method
of moments: an application to point process-based rainfall models,
Environmetrics, 26, 312–325, 2015.
Katz, R. W. and Skaggs, R. H.: On the use of autoregressive-moving average
processes to model meteorological time series, Mon. Weather Rev., 109,
479–484, 1981.
Khaliq, M. and Cunnane, C.: Modelling point rainfall occurrences with the
modified Bartlett-Lewis rectangular pulses model, J. Hydrol., 180, 109–138,
1996.
Kilsby, C., Jones, P., Burton, A., Ford, A., Fowler, H., Harpham, C., James,
P., Smith, A., and Wilby, R.: A daily weather generator for use in climate
change studies, Environ. Modell. Softw., 22, 1705–1719, 2007.
Kim, D. and Olivera, F.: Relative importance of the different rainfall
statistics in the calibration of stochastic rainfall generation models, J.
Hydrol. Eng., 17, 368–376, 2011.
Kim, D., Olivera, F., and Cho, H.: Effect of the inter-annual variability of
rainfall statistics on stochastically generated rainfall time series: part 1.
Impact on peak and extreme rainfall values, Stoch. Env. Res. Risk A., 27,
1601–1610, 2013a.
Kim, D., Olivera, F., Cho, H., and Socolofsky, S. A.: Regionalization of the
Modified Bartlett-Lewis Rectangular Pulse Stochastic Rainfall Model, Terr.
Atmos. Ocean. Sci., 24, https://doi.org/10.3319/TAO.2012.11.12.01(Hy), 2013b.
Kim, D., Kim, J., and Cho, Y.: A poisson cluster stochastic rainfall
generator that accounts for the interannual variability of rainfall
statistics: validation at various geographic locations across the united
states, J. Appl. Math., 2014, https://doi.org/10.1155/2014/560390, 2014.
Kim, D., Kwon, H., Lee, S., and Kim, S.: Regionalization of the Modified
Bartlett–Lewis rectangular pulse stochastic rainfall model across the Korean
Peninsula, J. Hydro-Environ. Res., 11, 123–137, 2016.
Kim, D., Cho, H., Onof, C., and Choi, M.: Let-It-Rain: a web application for
stochastic point rainfall generation at ungaged basins and its applicability
in runoff and flood modeling, Stoch. Env. Res. Risk A., 31, 1023–1043,
2017a.
Kim, J., Kwon, H., and Kim, D.: A hierarchical Bayesian approach to the
modified Bartlett-Lewis rectangular pulse model for a joint estimation of
model parameters across stations, J. Hydrol., 544, 210–223, 2017b.
Köppen, W.: Versuch einer Klassifikation der Klimate, vorzugsweise nach
ihren Beziehungen zur Pflanzenwelt, Geogr. Z., 6, 593–611, 1900.
Kossieris, P., Efstratiadis, A., Tsoukalas, I., and Koutsoyiannis, D.:
Assessing the performance of Bartlett-Lewis model on the simulation of Athens
rainfall, Enrgy. Proced., https://doi.org/10.13140/RG.2.2.14371.25120, 2015.
Kossieris, P., Makropoulos, C., Onof, C., and Koutsoyiannis, D.: A rainfall
disaggregation scheme for sub-hourly time scales: Coupling a Bartlett-Lewis
based model with adjusting procedures, J. Hydrol., https://doi.org/10.1016/j.jhydrol.2016.07.015, 2016.
Kottek, M., Grieser, J., Beck, C., Rudolf, B., and Rubel, F.: World map of
the Köppen-Geiger climate classification updated, Meteorol. Z., 15,
259–263, 2006.
Koutsoyiannis, D.: Coupling stochastic models of different timescales, Water
Resour. Res., 37, 379–391, 2001.
Koutsoyiannis, D.: HESS Opinions “A random walk on water”, Hydrol. Earth
Syst. Sci., 14, 585–601, https://doi.org/10.5194/hess-14-585-2010, 2010.
Koutsoyiannis, D.: Generic and parsimonious stochastic modelling for
hydrology and beyond, Hydrolog. Sci. J., 61, 225–244, 2016.
Koutsoyiannis, D. and Onof, C.: Rainfall disaggregation using adjusting
procedures on a Poisson cluster model, J. Hydrol., 246, 109–122, 2001.
Koutsoyiannis, D., Onof, C., and Wheater, H. S.: Multivariate rainfall
disaggregation at a fine timescale, Water Resour. Res., 39,
https://doi.org/10.1029/2002WR001600, 2003.
Langousis, A. and Koutsoyiannis, D.: A stochastic methodology for generation
of seasonal time series reproducing overyear scaling behaviour, J. Hydrol.,
322, 138–154, 2006.
Lombardo, F., Volpi, E., and Koutsoyiannis, D.: Rainfall downscaling in time:
theoretical and empirical comparison between multifractal and
Hurst-Kolmogorov discrete random cascades, Hydrolog. Sci. J., 57, 1052–1066,
2012.
Lombardo, F., Volpi, E., Koutsoyiannis, D., and Serinaldi, F.: A
theoretically consistent stochastic cascade for temporal disaggregation of
intermittent rainfall, Water Resour. Res., 53, 4586–4605, 2017.
Marani, M.: On the correlation structure of continuous and discrete point
rainfall, Water Resour. Res., 39, https://doi.org/10.1029/2002WR001456, 2003.
Menabde, M. and Sivapalan, M.: Modeling of rainfall time series and extremes
using bounded random cascades and levy-stable distributions, Water Resour.
Res., 36, 3293–3300, 2000.
Mishra, A. and Desai, V.: Drought forecasting using stochastic models, Stoch.
Env. Res. Risk A., 19, 326–339, 2005.
Modarres, R. and Ouarda, T. B.: Modeling the relationship between climate
oscillations and drought by a multivariate GARCH model, Water Resour. Res.,
50, 601–618, 2014.
Molnar, P. and Burlando, P.: Preservation of rainfall properties in
stochastic disaggregation by a simple random cascade model, Atmos. Res., 77,
137–151, 2005.
Müller, H. and Haberlandt, U.: Temporal rainfall disaggregation with a
cascade model: from single-station disaggregation to spatial rainfall, J.
Hydrol. Eng., 20, 04015026, https://doi.org/10.1061/(ASCE)HE.1943-5584.0001195, 2015.
Müller, H. and Haberlandt, U.: Temporal rainfall disaggregation using a
multiplicative cascade model for spatial application in urban hydrology, J.
Hydrol., https://doi.org/10.1016/j.jhydrol.2016.01.031, 2016.
Ogston, A., Cacchione, D., Sternberg, R., and Kineke, G.: Observations of
storm and river flood-driven sediment transport on the northern California
continental shelf, Cont. Shelf Res., 20, 2141–2162, 2000.
Olsson, J. and Burlando, P.: Reproduction of temporal scaling by a
rectangular pulses rainfall model, Hydrol. Process., 16, 611–630, 2002.
Onof, C. and Wheater, H. S.: Modelling of British rainfall using a random
parameter Bartlett-Lewis rectangular pulse model, J. Hydrol., 149, 67–95,
1993.
Onof, C. and Wheater, H. S.: Improved fitting of the Bartlett-Lewis
Rectangular Pulse Model for hourly rainfall, Hydrolog. Sci. J., 39, 663–680,
1994a.
Onof, C. and Wheater, H. S.: Improvements to the modelling of British
rainfall using a modified random parameter Bartlett-Lewis rectangular pulse
model, J. Hydrol., 157, 177–195, 1994b.
Paschalis, A., Molnar, P., Fatichi, S., and Burlando, P.: A stochastic model
for high-resolution space-time precipitation simulation, Water Resour. Res.,
49, 8400–8417, 2013.
Paschalis, A., Molnar, P., Fatichi, S., and Burlando, P.: On temporal
stochastic modeling of precipitation, nesting models across scales, Adv.
Water Resour., 63, 152–166, 2014.
Patz, J. A., Campbell-Lendrum, D., Holloway, T., and Foley, J. A.: Impact of
regional climate change on human health, Nature, 438, 310, https://doi.org/10.1038/nature04188, 2005.
Peleg, N. and Morin, E.: Stochastic convective rain-field simulation using a
high-resolution synoptically conditioned weather generator (HiReS-WG), Water
Resour. Res., 50, 2124–2139, 2014.
Peleg, N., Fatichi, S., Paschalis, A., Molnar, P., and Burlando, P.: An
advanced stochastic weather generator for simulating 2-D high-resolution
climate variables, J. Adv. Model. Earth. Sy., 9, 1595–1627, 2017.
Peres, D. and Cancelliere, A.: Estimating return period of landslide
triggering by Monte Carlo simulation, J. Hydrol., 541, 256–271, 2016.
Peres, D. J. and Cancelliere, A.: Derivation and evaluation of
landslide-triggering thresholds by a Monte Carlo approach, Hydrol. Earth
Syst. Sci., 18, 4913–4931, https://doi.org/10.5194/hess-18-4913-2014, 2014.
Pohle, I., Niebisch, M., Müller, H., Schümberg, S., Zha, T., Maurer,
T., and Hinz, C.: Coupling Poisson rectangular pulse and multiplicative
microcanonical random cascade models to generate sub-daily precipitation
timeseries, J. Hydrol., https://doi.org/10.1016/j.jhydrol.2018.04.063, 2018.
Reed, S., Schaake, J., and Zhang, Z.: A distributed hydrologic model and
threshold frequency-based method for flash flood forecasting at ungauged
locations, J. Hydrol., 337, 402–420, 2007.
Ritschel, C., Ulbrich, U., Névir, P., and Rust, H. W.: Precipitation
extremes on multiple timescales – Bartlett-Lewis rectangular pulse model and
intensity-duration-frequency curves, Hydrol. Earth Syst. Sci., 21,
6501–6517, https://doi.org/10.5194/hess-21-6501-2017, 2017.
Rodriguez-Iturbe, I. and Isham, V.: Some models for rainfall based on
stochastic point processes, P. Roy. Soc. A-Math. Phy., 410, 269–288, 1987.
Rodriguez-Iturbe, I. and Isham, V.: A point process model for rainfall:
further developments, P. Roy. Soc. A-Math. Phy., 417, 283–298, 1988.
Shisanya, C., Recha, C., and Anyamba, A.: Rainfall variability and its impact
on normalized difference vegetation index in arid and semi-arid lands of
Kenya, International Journal of Geosciences, 2, 36, https://doi.org/10.4236/ijg.2011.21004, 2011.
Smithers, J., Pegram, G., and Schulze, R.: Design rainfall estimation in
South Africa using Bartlett–Lewis rectangular pulse rainfall models, J.
Hydrol., 258, 83–99, 2002.
Solo-Gabriele, H. M.: Generation of long-term record of contaminant
transport, J. Environ. Eng., 124, 619–627, 1998.
Sotiriadou, A., Petsiou, A., Feloni, E., Kastis, P., Iliopoulou, T.,
Markonis, Y., Tyralis, H., Dimitriadis, P., and Koutsoyiannis, D.: Stochastic
investigation of precipitation process for climatic variability
identification, in: EGU General Assembly Conference Abstracts 2017, 23–28 April 2017, Vienna,
Austria, 2016.
Thomas, M. A., Mirus, B. B., and Collins, B. D.: Identifying physics-based
thresholds for rainfall-induced landsliding, Geophys. Res. Lett., https://doi.org/10.1029/2018GL079662, 2018.
Tyralis, H., Dimitriadis, P., Koutsoyiannis, D., O'Connell, P. E., Tzouka,
K., and Iliopoulou, T.: On the long-range dependence properties of annual
precipitation using a global network of instrumental measurements, Adv. Water
Resour., 111, 301–318, 2018.
Ünal, N., Aksoy, H., and Akar, T.: Annual and monthly rainfall data
generation schemes, Stoch. Env. Res. Risk A., 18, 245–257, 2004.
Velghe, T., Troch, P. A., De Troch, F., and Van de Velde, J.: Evaluation of
cluster-based rectangular pulses point process models for rainfall, Water
Resour. Res., 30, 2847–2857, 1994.
Verhoest, N., Troch, P. A., and De Troch, F. P.: On the applicability of
Bartlett–Lewis rectangular pulses models in the modeling of design storms at
a point, J. Hydrol., 202, 108–120, 1997.
Verhoest, N. E., Vandenberghe, S., Cabus, P., Onof, C., Meca-Figueras, T.,
and Jameleddine, S.: Are stochastic point rainfall models able to preserve
extreme flood statistics?, Hydrol. Process., 24, 3439–3445, 2010.
Wagener, T., Sivapalan, M., Troch, P. A., McGlynn, B. L., Harman, C. J.,
Gupta, H. V., Kumar, P., Rao, P. S. C., Basu, N. B., and Wilson, J. S.: The
future of hydrology: An evolving science for a changing world, Water Resour.
Res., 46, https://doi.org/10.1029/2009WR008906, 2010.
Warner, K. and Afifi, T.: Where the rain falls: Evidence from 8 countries on
how vulnerable households use migration to manage the risk of rainfall
variability and food insecurity, Clim. Dev., 6, 1–17, 2014.
Wasko, C., Sharma, A., and Johnson, F.: Does storm duration modulate the
extreme precipitation-temperature scaling relationship?, Geophys. Res. Lett.,
42, 8783–8790, 2015.
Yoo, J., Kim, D., Kim, H., and Kim, T.: Application of copula functions to
construct confidence intervals of bivariate drought frequency curve, J.
Hydro-Environ. Res., 11, 113–122, 2016.
Yu, D. J., Sangwan, N., Sung, K., Chen, X., and Merwade, V.: Incorporating
institutions and collective action into a sociohydrological model of flood
resilience, Water Resour. Res., 53, 1336–1353, 2017.
Zonta, R., Collavini, F., Zaggia, L., and Zuliani, A.: The effect of floods
on the transport of suspended sediments and contaminants: a case study from
the estuary of the Dese River (Venice Lagoon, Italy), Environ. Int., 31,
948–958, 2005.
Zorzetto, E., Botter, G., and Marani, M.: On the emergence of rainfall
extremes from ordinary events, Geophys. Res. Lett., 43, 8076–8082, 2016.
Short summary
Rainfall data are often unavailable for the analysis of water-related problems such as floods and droughts. In such cases, researchers use rainfall generators to produce synthetic rainfall data. However, data from most rainfall generators can serve only one specific purpose; i.e. one rainfall generator cannot be applied to analyse both floods and droughts. To overcome this issue, we invented a multipurpose rainfall generator that can be applied to analyse most water-related problems.
Rainfall data are often unavailable for the analysis of water-related problems such as floods...
