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Published on: June 30, 2020
Hydro-climatic extremes shift the hydrologic sensitivity regime in a cold basin
Shilei Peng1, Xianli Xu2, Renjun Liao3
1Huanjiang Observation and Research Station for Karst Ecosystem, Guangxi Key Laboratory of Karst Ecological Processes and Services, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha 410125, China; Research Faculty of Agriculture, Hokkaido University, Sapporo 0608589, Japan.
Climate extremes significantly alter water and sediment yields in cold regions. Hot-dry conditions decrease yields, while cold extremes may increase sediment, necessitating adaptive water management.
Area of Science:
- Hydrology
- Climate Science
- Environmental Science
Background:
- Climate extreme events increasingly disrupt hydrological processes, impacting water availability and sediment dynamics.
- The relationship between hydrological variability and climatic extremes is under-researched, especially in cold regions facing climate change.
- Cold regions are critical for agriculture and urban development, making their hydrological systems vulnerable.
Purpose of the Study:
- To investigate the impact of shifting climatic extreme patterns on hydrological regimes in the Ishikari River Basin (IRB).
- To develop a yield-based dichotomy framework for analyzing climate extreme impacts on water and sediment yields.
- To project future hydrological changes under different Shared Socioeconomic Pathways (SSPs) scenarios.
Main Methods:
- Utilized a modified Soil and Water Assessment Tool (SWAT).
- Integrated downscaled Coupled Model Intercomparison Project Phase 6 (CMIP6) General Circulation Model (GCM) climate projections.
- Employed Shared Socioeconomic Pathways (SSPs) scenarios for future climate projections.
Main Results:
- Identified significant annual variability in water and sediment yields linked to extreme climate events.
- Hot-dry conditions correlated with lower water and sediment yields.
- Increased cold extremes were associated with higher sediment yields in the IRB.
- Hotter and drier patterns may establish new hydrologic regimes and shift yield classification thresholds.
- SSP585 projections indicate intensified water availability and sediment transport, increasing flood and sedimentation risks.
Conclusions:
- Climate extremes significantly influence hydrological regimes, with distinct impacts from hot-dry versus cold conditions.
- Future climate change, particularly under SSP585, poses substantial risks to water availability and sediment transport in the IRB.
- Adaptive water management strategies are crucial to mitigate the impacts of altered hydrological regimes due to global climate change.
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