11,637 research outputs found
Statistical post-processing of hydrological forecasts using Bayesian model averaging
Accurate and reliable probabilistic forecasts of hydrological quantities like
runoff or water level are beneficial to various areas of society. Probabilistic
state-of-the-art hydrological ensemble prediction models are usually driven
with meteorological ensemble forecasts. Hence, biases and dispersion errors of
the meteorological forecasts cascade down to the hydrological predictions and
add to the errors of the hydrological models. The systematic parts of these
errors can be reduced by applying statistical post-processing. For a sound
estimation of predictive uncertainty and an optimal correction of systematic
errors, statistical post-processing methods should be tailored to the
particular forecast variable at hand. Former studies have shown that it can
make sense to treat hydrological quantities as bounded variables. In this
paper, a doubly truncated Bayesian model averaging (BMA) method, which allows
for flexible post-processing of (multi-model) ensemble forecasts of water
level, is introduced. A case study based on water level for a gauge of river
Rhine, reveals a good predictive skill of doubly truncated BMA compared both to
the raw ensemble and the reference ensemble model output statistics approach.Comment: 19 pages, 6 figure
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ForChaos: Real Time Application DDoS detection using Forecasting and Chaos Theory in Smart Home IoT Network
Recently, D/DoS attacks have been launched by zombie IoT devices in smart home networks. They pose a great threat to to network systems with Application Layer DDoS attacks being especially hard to detect due to their stealth and seemingly legitimacy. In this paper, we propose we propose ForChaos, a lightweight detection algorithm for IoT devices, that is based on forecasting and chaos theory to identify flooding and DDoS attacks. For every time-series behaviour collected, a forecasting-technique prediction is generated, based on a number of features, and the error between the two values is calcualted. In order to assess the error of the forecasting from the actual value, the lyapunov exponent is used to detect potential malicious behaviour. In NS-3 we evaluate our detection algorithm through a series of experiments in Flooding and Slow-Rate DDoS attacks. The results are presented and discussed in detail and compared with related studies, demonstrating its effectiveness and robustness
Enhancing Students' Understanding of Risk and Geologic Hazards Using a Dartboard Model
This article describes the use of a model to express the magnitude-frequency relationships of natural hazards. The model consists of a dartboard whose rings can be drawn to represent magnitude, exceedence probability, average recurrence interval, or other statistical information. Students are engaged by "playing" the dart game through conducting a thought experiment, actually throwing at a physical dartboard, or simulating events based on a computer program. This type of model is applicable to any sequence of events that can be described by random sampling. It helps emphasize the random nature of such events, and provides a means for presenting hazard recurrence information in an easily visible form. In addition, it helps mitigate students' misconceptions about risk and average recurrence intervals, and provides a way to teach probability concepts without the use of sophisticated mathematics. Educational levels: Graduate or professional
Blue Nile Runoff Sensitivity to Climate Change
This study describes implementation of hydrological climate change impact assessment tool utilising a combination of statistical spatiotemporal downscaling and an operational hydrological model known as the Nile Forecasting System. A spatial rainfall generator was used to produce high-resolution (daily, 20km) gridded rainfall data required by the distributed hydrological model from monthly GCM outputs. The combined system was used to assess the sensitivity of upper Blue Nile flows at Diem flow gauging station to changes in future rainfall during the June-September rainy season based on output from three GCMs. The assessment also incorporated future evapotranspiration changes over the basin. The climate change scenarios derived in this study were broadly in line with other studies, with the majority of scenarios indicating wetter conditions in the future. Translating the impacts into runoff in the basin showed increased future mean flows, although these would be offset to some degree by rising evapotranspiration. Impacts on extreme runoff indicated the possibility of more severe floods in future. These are likely to be exacerbated by land-use changes including overgrazing, deforestation, and improper farming practices. Blue Nile basin flood managers therefore need to continue to prepare for the possibility of more frequent floods by adopting a range of measures to minimise loss of life and guard against other flood damage
Uncertainty Quantification of Future Design Rainfall Depths in Korea
One of the most common ways to investigate changes in future rainfall extremes is to use future rainfall data simulated by climate models with climate change scenarios. However, the projected future design rainfall intensity varies greatly depending on which climate model is applied. In this study, future rainfall Intensity???Duration???Frequency (IDF) curves are projected using various combinations of climate models. Future Ensemble Average (FEA) is calculated using a total of 16 design rainfall intensity ensembles, and uncertainty of FEA is quantified using the coefficient of variation of ensembles. The FEA and its uncertainty vary widely depending on how the climate model combination is constructed, and the uncertainty of the FEA depends heavily on the inclusion of specific climate model combinations at each site. In other words, we found that unconditionally using many ensemble members did not help to reduce the uncertainty of future IDF curves. Finally, a method for constructing ensemble members that reduces the uncertainty of future IDF curves is proposed, which will contribute to minimizing confusion among policy makers in developing climate change adaptation policies
Towards the improvement of machine learning peak runoff forecasting by exploiting ground- and satellite-based precipitation data: A feature engineering approach
La predicción de picos de caudal en sistemas montañosos complejos presenta desafíos en
hidrología debido a la falta de datos y las limitaciones de los modelos físicos. El aprendizaje
automático (ML) ofrece una solución al permitir la integración de técnicas y productos satelitales
de precipitación (SPPs). Sin embargo, se ha debatido sobre la efectividad del ML debido a su
naturaleza de "caja negra" que dificulta la mejora del rendimiento y la reproducibilidad de los
resultados. Para abordar estas preocupaciones, se han propuesto estrategias de ingeniería de
características (FE) para incorporar conocimiento físico en los modelos de ML, mejorando la
comprensión y precisión de las predicciones. Esta investigación doctoral tiene como objetivo
mejorar la predicción de picos de caudal mediante la integración de conceptos hidrológicos a
través de técnicas de FE y el uso de datos de precipitación in-situ y SPPs. Se exploran técnicas
y estrategias de ML para mejorar la precisión en sistemas hidrológicos macro y mesoescala.
Además, se propone una estrategia de FE para aprovechar la información de SPPs y superar la
escasez de datos espaciales y temporales. La integración de técnicas avanzadas de ML y FE
representa un avance en hidrología, especialmente para sistemas montañosos complejos con
limitada o nula red de monitoreo. Los hallazgos de este estudio serán valiosos para tomadores
de decisiones e hidrólogos, facilitando la mitigación de los impactos de los picos de caudal.
Además, las metodologías desarrolladas se pueden adaptar a otros sistemas de macro y
mesoescala, beneficiando a la comunidad científica en general.Peak runoff forecasting in complex mountain systems poses significant challenges in hydrology
due to limitations in traditional physically-based models and data scarcity. However, the
integration of machine learning (ML) techniques offers a promising solution by balancing
computational efficiency and enabling the incorporation of satellite precipitation products (SPPs).
However, debates have emerged regarding the effectiveness of ML in hydrology, as its black-box
nature lacks explicit representation of hydrological processes, hindering performance
improvement and result reproducibility. To address these concerns, recent studies emphasize the
inclusion of FE strategies to incorporate physical knowledge into ML models, enabling a better
understanding of the system and improved forecasting accuracy. This doctoral research aims to
enhance the effectiveness of ML in peak runoff forecasting by integrating hydrological concepts
through FE techniques, utilizing both ground-based and satellite-based precipitation data. For
this, we explore ML techniques and strategies to enhance accuracy in complex macro- and mesoscale
hydrological systems.
Additionally, we propose a FE strategy for a proper utilization of SPP information which is crucial for overcoming spatial and temporal data scarcity.
The integration of advanced ML techniques and FE represents a significant advancement in hydrology,
particularly for complex mountain systems with limited or inexistent monitoring networks.
The findings of this study will provide valuable insights for decision-makers and hydrologists, facilitating effective mitigation of the impacts of peak runoffs. Moreover, the developed methodologies can be adapted
to other macro- and meso-scale systems, with necessary adjustments based on available data
and system-specific characteristics, thus benefiting the broader scientific community.0000-0002-7683-37680000-0002-6206-075XDoctor (PhD) en Recursos HídricosCuenc
Ensemble evaluation of hydrological model hypotheses
It is demonstrated for the first time how model parameter, structural and data uncertainties can be accounted for explicitly and simultaneously within the Generalized Likelihood Uncertainty Estimation (GLUE) methodology. As an example application, 72 variants of a single soil moisture accounting store are tested as simplified hypotheses of runoff generation at six experimental grassland field-scale lysimeters through model rejection and a novel diagnostic scheme. The fields, designed as replicates, exhibit different hydrological behaviors which yield different model performances. For fields with low initial discharge levels at the beginning of events, the conceptual stores considered reach their limit of applicability. Conversely, one of the fields yielding more discharge than the others, but having larger data gaps, allows for greater flexibility in the choice of model structures. As a model learning exercise, the study points to a “leaking” of the fields not evident from previous field experiments. It is discussed how understanding observational uncertainties and incorporating these into model diagnostics can help appreciate the scale of model structural error
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