Changes in the Water Cycle
Providing global estimates of river runoff and freshwater availability to support climate adaptation measures.
In a nutshell
- Assessing water availability is key to adapt to water-related disasters and formulate mitigation policies.
- The use case aims to refine the current hydrology information system by providing more refined estimates of river runoff.
- Thanks to the developed application, it will be possible to obtain a greater understanding of the water availability and the measures needed for climate adaptation
Technical Overview
Challenge
Climate change is affecting the hydrological cycle and exacerbating water scarcity worldwide. Such water-related disasters as torrential rains, droughts and floods have been increasing both in frequency and intensity. With the raising hydro-hazard impacts, decision-makers require an improved scientific basis for preparation and response to the future extreme hydrological events.
DestinE Solution
With this use case the Climate DT will be able to provide global estimates of river runoff at a spatial scale of 5 km spatial scales and up to 1 hour, substantially more detailed than the current hydrology information systems. The HydroRiver application is based on the mesoscale Hydrologic Model (mHM), a well-established model used operationally by the German Drought Monitor, and the multiscale Routing Model (mRM), both developed by Germany’s Helmholtz Centre for Environmental Research (UFZ). The main users are DVGW (German Technical and scientific Association for Gas and Water) and EEA (European Environment Agency).
The mHM is used operationally by ECMWF in delivering the Copernicus Climate Change Service (C3S) to provide global seasonal hydrological forecasts and has also served for research, among others, about the impacts of climate change in flooding and droughts in Europe.
The application consists of a “wrapping” software built around the mHM model that makes the interface with the climate DT and adapts the model to the global scale with the spatial and temporal resolution required.
Global mean soil moisture (in red), and mean river discharge (in blue, zoomed in to show the high-resolution of the river networks) for the years February 2020-February 2022. The mHM model (using the results from the NextGEMS Cycle2) as a meteorological forcing, and provided output variables representing various freshwater components (e.g., discharge, soil-moisture). Credit: ufz.de
Impact
The “HydroRiver” application will provide data about a wide range of hydrological variables and indicators depicting global freshwater availability and providing insights on the requirements for climate adaptation from global to local level in areas of particular interest.
The enhanced global river discharge application processes enormous data rates resulting from the ever-evolving DT Climate simulations, as well as additional calculations for bias correction, which are critical on applications running at such spatial and temporal scales.
The system will also provide hydrology information tailored for the impact sector with expert users and stakeholders participating in the process.