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MIKE 2026
Rainfall and Evaporation for Storage
Boundary conditions of type Network rainfall and Network evaporation can now be applied directly to storages, including large lakes and reservoirs. This enhancement enables accurate estimation of water balance by accounting for rainfall and evaporation effects without complex model setups. Users can efficiently apply these conditions to all, selected, or individual storages to streamline large-scale simulations.
Enhanced Cross Section Shapefile Export
Cross sections can now be exported to shapefiles with greater flexibility, allowing users to export only selected sections or the extents of active cross sections between markers 1 and 3. This improvement streamlines post-processing and presentation, enabling clearer visualisation of modelled cross sections in GIS or other mapping software.
MIKE 2025 Update 1
Simplify migrations with a new hydrological model type
- A new hydrological model type is now available in MIKE 1D, combining the New UK and Wallingford routing methods.
- Available for both collection system and river models, it helps you import setups that use similar approaches from other platforms. This is part of ongoing improvements to simplify model migration into MIKE+—allowing you to bring in network structures, catchments, loads, and boundaries with minimal adjustment.
Simplify migrations with a new hydrological model type
- A new hydrological model type is now available in MIKE 1D, combining the New UK and Wallingford routing methods.
- Available for both collection system and river models, it helps you import setups that use similar approaches from other platforms. This is part of ongoing improvements to simplify model migration into MIKE+—allowing you to bring in network structures, catchments, loads, and boundaries with minimal adjustment.
More easily manage rainfall events in simulations
- You can now tag boundary conditions with event names like "100-year" or "30-year", and select the relevant tag when running simulations.
- This means no more toggling individual boundaries on and off, or setting up full scenarios just to swap rainfall data.
- It’s a simpler way to manage multiple return periods, and makes re-running simulations much faster and less error-prone.
