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Local control on precipitation in a fully coupled climate-hydrology model
Morten A D Larsen1, Jens H Christensen2, Martin Drews1
1Technical University of Denmark, Produktionstorvet, building 426, 2800 Kgs. Lyngby, Denmark.
Scientific Reports
|March 11, 2016
Summary
Coupling regional climate models with hydrological models improves precipitation simulation accuracy. This advancement enhances climate change adaptation by providing more reliable future projections and reducing the need for bias correction.
Area of Science:
- Climate Science
- Hydrology
- Environmental Modeling
Background:
- Accurate regional precipitation simulation is crucial for climate change adaptation.
- Climate models often struggle with precipitation biases due to complex, unresolved processes.
- Existing models face challenges in representing hydrological feedbacks influencing precipitation.
Purpose of the Study:
- To demonstrate how a coupled regional climate-hydrological model improves local precipitation simulation.
- To assess the impact of integrated water and energy fluxes on precipitation dynamics.
- To evaluate the potential of coupled models for enhancing climate projections and reducing bias correction needs.
Main Methods:
- Coupling a regional climate model (RCM) with a distributed hydrological catchment model.
- Fully integrating water and energy fluxes across subsurface, land surface, plant cover, and atmosphere.
- Conducting a six-year simulation period to analyze precipitation dynamics.
Main Results:
- The coupled model achieved a more realistic representation of local precipitation.
- Substantial improvements in simulated precipitation dynamics were observed on seasonal and longer timescales.
- Hydrological sub-surface processes, including groundwater and moisture feedback, were key to these improvements.
Conclusions:
- Coupled climate-hydrology models offer a pathway to more accurate climate projections.
- The local influence of hydrological processes on the atmosphere is significant.
- These models may reduce the necessity for bias correction in climate-hydrology impact studies.
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