Abstract:There is a high demand for openly accessible hydroclimatic data for climate change adaptation. Different data sources are available, however, discrepancy between the data can confuse users and should be evaluated and explained. This study, investigates how climate impact indicators (CIIs) developed for global users in the Copernicus Climate Change Service (C3S) are comparable to other openly available global data for water and climate. We found that, for temperature, datasets are comparable and climate impacts… Show more
“…However, different number of GCMs used in different studies together with other assumptions, e.g., on reference period of bias-adjustment methods make the comparison of the impacts difficult. Merks et al (2020) found large differences between both current discharges and future changes projected with WW-HYPE using the full ensemble of 18 GCMs and those simulated with the variable infiltration capacity (VIC) model (Liang et al 1994;van Vliet et al 2015). The differences were partly attributed to propagation of change in areas with low annual precipitation and discharge, where it is difficult to predict runoff, and partly to differences between the models themselves (hydrological versus land-surface model), the evapotranspiration routines, and GCM ensembles.…”
Section: Present and Future Global Hydrological Conditionsmentioning
confidence: 99%
“…A variety of models can be strategically chosen to explore these key processes as well as a parameter space for the model calibration. Model performance also affects the agreement among the hydrological models (Merks et al 2020). A standardized evaluation, e.g., over smaller regions, would further help in these evaluations.…”
Section: Modeling a Change With A Large-scale Hydrological Modelmentioning
Continental and global dynamic hydrological models have emerged recently as tools for large-scale analyses. One such tool is a dynamic process-based rainfall-runoff and water quality model called Hydrological Predictions for Environment (HYPE). This study presents and compares historical simulations of runoff and sediment concentrations for three nested-model domains using global, continental (Europe), and national (Sweden) catchment-based HYPE applications. Future impacts on runoff, soil moisture, and aridity from changing climate were assessed using the global and continental HYPE applications with three coupled model intercomparison project phase 5 (CMIP5) global climate models (GCMs). Simulated sediment concentrations varied considerably among the nested models in spatial patterns due to different data sources, whereas runoff values were more similar. Regardless of the variation, the global model was able to provide information on climate change impacts comparable to those from the continental and national models for hydrological indicators. Global hydrological models are thus valuable tools for, e.g., first screenings of climate change effects and detection of spatial patterns. Comparison across nested domains demonstrates the significance of scale that needs to be considered when interpreting the impacts alongside with model performance.
“…However, different number of GCMs used in different studies together with other assumptions, e.g., on reference period of bias-adjustment methods make the comparison of the impacts difficult. Merks et al (2020) found large differences between both current discharges and future changes projected with WW-HYPE using the full ensemble of 18 GCMs and those simulated with the variable infiltration capacity (VIC) model (Liang et al 1994;van Vliet et al 2015). The differences were partly attributed to propagation of change in areas with low annual precipitation and discharge, where it is difficult to predict runoff, and partly to differences between the models themselves (hydrological versus land-surface model), the evapotranspiration routines, and GCM ensembles.…”
Section: Present and Future Global Hydrological Conditionsmentioning
confidence: 99%
“…A variety of models can be strategically chosen to explore these key processes as well as a parameter space for the model calibration. Model performance also affects the agreement among the hydrological models (Merks et al 2020). A standardized evaluation, e.g., over smaller regions, would further help in these evaluations.…”
Section: Modeling a Change With A Large-scale Hydrological Modelmentioning
Continental and global dynamic hydrological models have emerged recently as tools for large-scale analyses. One such tool is a dynamic process-based rainfall-runoff and water quality model called Hydrological Predictions for Environment (HYPE). This study presents and compares historical simulations of runoff and sediment concentrations for three nested-model domains using global, continental (Europe), and national (Sweden) catchment-based HYPE applications. Future impacts on runoff, soil moisture, and aridity from changing climate were assessed using the global and continental HYPE applications with three coupled model intercomparison project phase 5 (CMIP5) global climate models (GCMs). Simulated sediment concentrations varied considerably among the nested models in spatial patterns due to different data sources, whereas runoff values were more similar. Regardless of the variation, the global model was able to provide information on climate change impacts comparable to those from the continental and national models for hydrological indicators. Global hydrological models are thus valuable tools for, e.g., first screenings of climate change effects and detection of spatial patterns. Comparison across nested domains demonstrates the significance of scale that needs to be considered when interpreting the impacts alongside with model performance.
“…A quality assured production chain which is frequently used in climatic services (including hydro services; [17]) was implemented to produce Climate Indicators (CI) and Water Indicators (WI) from Essential Climate Variables (ECV) available in the Climate Information platform (Figure 1). The production follows a rigorous quality assurance protocol developed in previous projects and adjusted to fit the current needs.…”
Section: Data Productionmentioning
confidence: 99%
“…The ensemble of CMIP5 models previously used in a Copernicus Climate Change Service Sectoral Information System (C3S SIS, [17]) was also used to provide a complete global coverage. The ensemble was modified to fit the current requests (different reference period (1981-2010), which differs from C3S (1971-2000)); the ensemble is also available in Appendix A.…”
Section: Global and Regional Climate Modelsmentioning
confidence: 99%
“…The validity of spatial patterns in hydrological variables was assessed through visual inspection of mapped aggregates (averages, sums) of WW-HYPE output variables. Values of the model variables at selected spatial points, e.g., large river outlets, are semi-quantitatively assessed through comparison with expected ranges based on external data, e.g., observations or previous model results (runs with CMIP5, [17]), to make sure values are within a reasonable range.…”
Section: Global Hydrological Modelling and Water Indicatorsmentioning
The next generation of climate services needs not only tailoring to specific user needs but to provide, in addition, access to key information in a usable way that satisfies the needs of different users’ profiles; especially web-based services. Here, we present the outcomes from developing such a new interactive prototype. The service provides data for robust climate analysis to underpin decision-making when planning measures to compensate for climate impact. The goal is to facilitate the communication on climate information between climate modelling communities and adaptation or mitigation initiatives from vulnerable countries that are applying for funds from the Green Climate Fund (GCF). A participatory process was ensured during four workshops in four pilot countries, with an audience of national and international experts. During this process it was made clear that in all countries there is a strong need for knowledge in climate science, while in most countries there was also an increasing need of capacity in hydrological modelling and water management. The active interaction during the workshops was found necessary to facilitate the dialogue between service developers and users. Understanding the users, transparency on potentials and limitations of climate services together with capacity development in climate science and methods were required components in the development of the service.
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