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EUROFRIEND Workshop & training
เข้าร่วมเมื่อ 6 ก.ค. 2022
Monthly, EURO-FRIEND proposes a seminar/training on new datasets, methodologies, or results in the field. We hope this initiative encourages early-career scientists to join our FRIENDly community.
We are pleased to offer two more sessions this year:
Session 8: Current Challenges of Research Transfer from Hydrology to Operational Applications
Led by Stephan Dietrich (ICWRGC)
Date: November 20th
Time: 2 PM UTC
Registration: us06web.zoom.us/meeting/register/tZcud-GtrDkjH9SY48cehfqz6lzO8OJq-EfF#/registration
Session 9: Explainable AI in Machine Learning Hydrological Models: Bridging Physical Interpretation and Black-Box Paradigms
Led by Gerald Corzo-Perez (IHE Delft)
Date: December 6th
Time: 12 PM UTC
Registration: us06web.zoom.us/meeting/register/tZ0pcuivrzsuEtUkOrah-ezXGbf5WuTdv6M8#/registration
We are pleased to offer two more sessions this year:
Session 8: Current Challenges of Research Transfer from Hydrology to Operational Applications
Led by Stephan Dietrich (ICWRGC)
Date: November 20th
Time: 2 PM UTC
Registration: us06web.zoom.us/meeting/register/tZcud-GtrDkjH9SY48cehfqz6lzO8OJq-EfF#/registration
Session 9: Explainable AI in Machine Learning Hydrological Models: Bridging Physical Interpretation and Black-Box Paradigms
Led by Gerald Corzo-Perez (IHE Delft)
Date: December 6th
Time: 12 PM UTC
Registration: us06web.zoom.us/meeting/register/tZ0pcuivrzsuEtUkOrah-ezXGbf5WuTdv6M8#/registration
2024 Session 9: Explainable AI in Machine Learning Hydrological Models
In recent decades, the use of machine learning has significantly increased, raising concerns about its application and the uncertainties it introduces across various fields-including hydrology. Explainable Artificial Intelligence (XAI) offers a framework for understanding machine and deep learning models, enabling clear interpretation of models, their parameters, and specific behaviours under simulated conditions.
Machine learning approaches have gained substantial ground in the realm of hydrological modelling. Studies have demonstrated that incorporating multiple physical input parameters can enhance or diminish models' interpretability and increase or decrease their predictive performance. Therefore, it is crucial to determine what is physically plausible within the model, identify patterns that extend beyond established physics, and ascertain whether these patterns provide a foundation for future research or reveal key mistakes in the modelling process.
This work presents a series of examples of how hydrological machine learning models can provide basic interpretability, but also to discuss the model interpretability, utilizing methods ranging from feature engineering to model-agnostic techniques-including applications of SHAP (SHapley Additive exPlanations) and LIME (Local Interpretable Model-Agnostic Explanations). This presentation aims to demonstrate how explainability can serve as a basis for model improvement and also highlight instances where physical processes are underrepresented, leading to increased model uncertainty.
Speaker: Gerald Corzo Perez (IHE Delft, Netherlands)
Machine learning approaches have gained substantial ground in the realm of hydrological modelling. Studies have demonstrated that incorporating multiple physical input parameters can enhance or diminish models' interpretability and increase or decrease their predictive performance. Therefore, it is crucial to determine what is physically plausible within the model, identify patterns that extend beyond established physics, and ascertain whether these patterns provide a foundation for future research or reveal key mistakes in the modelling process.
This work presents a series of examples of how hydrological machine learning models can provide basic interpretability, but also to discuss the model interpretability, utilizing methods ranging from feature engineering to model-agnostic techniques-including applications of SHAP (SHapley Additive exPlanations) and LIME (Local Interpretable Model-Agnostic Explanations). This presentation aims to demonstrate how explainability can serve as a basis for model improvement and also highlight instances where physical processes are underrepresented, leading to increased model uncertainty.
Speaker: Gerald Corzo Perez (IHE Delft, Netherlands)
มุมมอง: 137
วีดีโอ
2024 Session 8: Current challenges of research transfer from hydrology for operational applications
มุมมอง 64หลายเดือนก่อน
With climate change, the need for high-quality, state-of-the-art monitoring and forecasting tools in the climate and freshwater sector is becoming increasingly important. This accounts for both, science-based policy support and operational technical solutions ranging from observations, IT and data management infrastructures to operational forecasting and warning systems. Although operational sy...
2024 Session 7: Quality Control of Hydrological Data [L. Strohmenger, W. Korres, S. Turner]
มุมมอง 1673 หลายเดือนก่อน
Part 1 [Visual detection of non-natural records in streamflow/ Laurent Strohmenger, IGB-Berlin]: Streamflow measurements can contain anomalies, e.g., erroneous values and human influences, affecting the understanding of hydrological processes. Identifying these anomalies is time-consuming, and no prior study explored their impact on hydrological indicators across large datasets. This study pres...
2024 Session 6: The Hydrological Modelling Framework HydPy: Introductory Workshop
มุมมอง 1504 หลายเดือนก่อน
HydPy is a Python-based open-source framework for developing and applying different types of hydrological models. In this workshop, we give an overview of its possibilities and show how to get started with HydPy in understandable steps.
2024 Session 5: Harnessing R and Cloud for Hydrology [A. Khouakhi]
มุมมอง 1066 หลายเดือนก่อน
The emergence of Earth Observation (EO) cloud computing technologies such as Google Earth Engine and Microsoft Planetary Computer, has facilitated open access to extensive computational resources and datasets. This course will showcase the synergies between R programming and EO cloud computing capabilities for hydrological research. This course will guide you on how to harness these platforms f...
2024 Session 4: Advances in Seasonal Hydrological Forecasting [K. Facer-Childs]
มุมมอง 1726 หลายเดือนก่อน
Seasonal hydrological forecasts are critical for water resources management all over the world. Highlighting the emergence of drought and flood-rich periods, and providing likelihoods of the cessation of such events, benefits a wide number of sectors from agriculture and environment, through water supply, to leisure. This presentation details the advances of the UK Hydrological Outlook seasonal...
2024 Session 3: Climate Change Projections, their Uncertainties and the Potential to Reduce Them
มุมมอง 4377 หลายเดือนก่อน
With climate change adaptation now being inevitable, demand for accurate climate projections is growing. However, uncertainty in future projections, especially at regional scales, remains sizable and originates from a mix of reducible and irreducible sources. We will review the main sources of projection uncertainty across scales and climate model generations, before discussing prospects of con...
2024 Session 2: Reconstructing and Re-Evaluating Historical Drought [Conor Murphy]
มุมมอง 758 หลายเดือนก่อน
Long meteorological records are fundamental for understanding historical droughts and the management of water resources, yet digitised observations typically span less than 100 years, and much less in most regions, with considerable uncertainties surrounding earlier records. Water managers are especially interested in the ‘worst drought on record’ and ‘long-droughts’ that persist for multiple s...
2024 Session 1: The IX-Phase of the Intergovernmental Hydrological Program & FRIEND-Water
มุมมอง 1039 หลายเดือนก่อน
The FRIEND-Water program (FWP) is the oldest and the most transverse Flagship Initiative within the Intergovernmental Hydrological Program (IHP) of UNESCO. FRIEND stands for “Flow Regimes from International and Experimental Network Data”. The FWP is dedicated to facilitating and fostering collaborations between large communities of hydrologists and associated disciplines on data sharing and res...
2023 Session 9: Anthropogenic intensification of life-threatening rainfall extremes [H. Fowler]
มุมมอง 117ปีที่แล้ว
Short-duration (1 to 3 hours) rainfall extremes can cause serious damage to infrastructure and ecosystems and can result in loss of life through rapidly developing (flash) flooding. Short-duration rainfall extremes are intensifying with warming at a rate consistent with atmospheric moisture increase (~7%/K) that also drives intensification of longer-duration extremes (1day ). Evidence from some...
2023 Session 8: Using GRACE for global hydrological modelling: benefits and limitations [P. Doell]
มุมมอง 215ปีที่แล้ว
To improve our understanding of the global freshwater system, global hydrological modeling needs to utilize not only the best available data regarding model input such as irrigated areas and attributes of surface water bodies but also observations of model output variables. While in-situ observations of streamflow have traditionally been employed for the calibration and validation of hydrologic...
2023 Session 7: ROBIN - a global Reference Hydrometric Network [J. Hannaford]
มุมมอง 128ปีที่แล้ว
Floods and droughts are expected to become more severe in a warming world, furthering the impacts they cause on lives and livelihoods, infrastructure, and economies. To adapt to future changes, we need to detect and attribute emerging trends in hydrological variables such as river flow, to better understand and constrain model-based projections. Unfortunately, the modification of river flows by...
2023 Session 6: Model-comparison frameworks: Introduction and examples of how to use them[W Knoben]
มุมมอง 211ปีที่แล้ว
Hydrologists may share a certain common understanding of how water moves through the landscape, but the way this understanding is encoded in models varies wildly. Models differ in their spatial organization, the temporal resolution of the simulations, the equations used to describe physical processes and the numerical techniques used to solve the model equations. It is well-known that different...
2023 Session 5: Exceptional flood events: insights from three simulation approaches [M. Brunner]
มุมมอง 199ปีที่แล้ว
Exceptional floods, i.e. flood events with magnitudes occurring only once or twice a century, are rare by definition. Therefore, it is challenging to estimate their frequency and magnitude. In this talk, I discuss three methods that enable us to study exceptional extreme events absent in observational records thanks to increasing sample size: stochastic simulation, reanalysis ensemble pooling, ...
2023 Session 4: A Range of Outcomes in Regional Climate Trends [C. Deser]
มุมมอง 140ปีที่แล้ว
A range of outcomes: Combined effects of internal variability and anthropogenic forcing on regional climate trends in Europe [C. Deser] Disentangling the effects of internal variability and anthropogenic forcing on regional climate trends remains a key challenge with far-reaching implications. Due to its largely unpredictable nature on timescales longer than a decade, internal climate variabili...
2023 Session 3: Shiny Workshop - Create Your Own Hydrological Data App [T. Recknagel]
มุมมอง 161ปีที่แล้ว
2023 Session 3: Shiny Workshop - Create Your Own Hydrological Data App [T. Recknagel]
2023 Session 2: 23 unsolved problems in hydrology (UPH) - a community perspective [G. Bloschl]
มุมมอง 239ปีที่แล้ว
2023 Session 2: 23 unsolved problems in hydrology (UPH) - a community perspective [G. Bloschl]
2023 Session 1: The UNESCO IHP FRIEND-Water program [Dietrich, Bharati, Dieppois, Hannaford]
มุมมอง 138ปีที่แล้ว
2023 Session 1: The UNESCO IHP FRIEND-Water program [Dietrich, Bharati, Dieppois, Hannaford]
2022 Session 8 "Long Short-Term Memory networks for rainfall-runoff modelling" [Frederik Kratzert]
มุมมอง 6492 ปีที่แล้ว
2022 Session 8 "Long Short-Term Memory networks for rainfall-runoff modelling" [Frederik Kratzert]
2022 Session 7 "Hydrological Modelling with R" [Dr G Thirel and O Delaigue; INRAE]
มุมมอง 2.2K2 ปีที่แล้ว
2022 Session 7 "Hydrological Modelling with R" [Dr G Thirel and O Delaigue; INRAE]
2022 Session 2 "Improving Reproducibility and Efficiency - Use of R in Hydrology"[T. Recknagel]
มุมมอง 2402 ปีที่แล้ว
2022 Session 2 "Improving Reproducibility and Efficiency - Use of R in Hydrology"[T. Recknagel]
2022 Session 6 "Large-sample hydrology: learning from hundreds to thousands of catchments"[N. Addor]
มุมมอง 2942 ปีที่แล้ว
2022 Session 6 "Large-sample hydrology: learning from hundreds to thousands of catchments"[N. Addor]
2022 Session 5 "A hydrologist's guide to open science" [N. Dogulu]
มุมมอง 1752 ปีที่แล้ว
2022 Session 5 "A hydrologist's guide to open science" [N. Dogulu]
2022 Session 4 "Constructing and Communicating Regional Climate Change Scenarios" [T. Shepherd]
มุมมอง 1212 ปีที่แล้ว
2022 Session 4 "Constructing and Communicating Regional Climate Change Scenarios" [T. Shepherd]
2022 Session 3 "Climate analysis in R" [R Benestad]
มุมมอง 2212 ปีที่แล้ว
2022 Session 3 "Climate analysis in R" [R Benestad]
2022 Session 1 "What is needed to bridge the data knowledge gap in hydrology?" [S. Dietrich]
มุมมอง 1372 ปีที่แล้ว
2022 Session 1 "What is needed to bridge the data knowledge gap in hydrology?" [S. Dietrich]
Thanks a lot for this. Very informative. I am however not able to run the airGRteaching GUI, i get a shiny app but every option seemx to be greyed out. Also the first command throws the following error: PREP <- PrepGR(ObsDF = BasinObs, HydroModel = "GR5J", CemaNeige = FALSE) Error in CreateInputsModel(FUN_MOD = FUN_MOD, DatesR = ObsDF$DatesR, Precip = ObsDF$Precip, : time series could not be trunced since missing values were detected at the last time-step
GR models are continuous hydrological model; no missing data in precipitation and PET times series are allowed. Please note thBasinObs column names respect the following order: DatesR: dates in the POSIXt format [NO MISSING TIME STEPS] P: average precipitation [mm/time step] [NO MISSING VALUES] T: catchment average air temperature [℃] [OPTIONAL] E: catchment average potential evapotranspiration [mm/time step] [NO MISSING VALUES] Qmm: outlet discharge [mm/time step]
Thanks a lot for this extremely nice overview of airGR. I have a question: Is it possible to have multiple hydrological response units (HRUs) as GR4Js in a catchment using your package? Do you have an example code? Thanks a lot in advance!
Usually, GR4J is used either in a lumped way, i.e. on a total catchment, or in a semi-distributed way, i.e. on sub-catchments, with GR4J models flowing on downstream GR4J models. For the second option, we usually use streamflow stations to mesh the total catchment and the measured data at this station to calibrate the model. Using GR4J on HRUs is theoretically possible, if the HRUs respect the flowing directions, even if we have never done it. The only issue is that to do so, a method to estimate the GR4J parameters on ungauged HRUs would be necessary. There is plenty of litterature on this, but we do not provide the regionalisation tool. Finally, please note that the airGRiwrm package, which is an extension of airGR, should be prefered as it automatizes the use of GR4J models in a semi-distributed way.
Very interesting talk!