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Separating decadal global water cycle variability from sea level rise
B D Hamlington1, J T Reager2, M-H Lo3
1Center for Coastal Physical Oceanography, Old Dominion University, Norfolk, USA. bhamling@odu.edu.
Climate change amplifies the water cycle, affecting terrestrial water storage (TWS). TWS variability can mask sea level rise trends, but this study quantifies its impact on decadal sea level changes.
Area of Science:
- Climate Science
- Oceanography
- Hydrology
Background:
- Global warming alters precipitation and the water cycle, impacting terrestrial water storage (TWS).
- Changes in TWS influence global sea level variations.
- Natural TWS variability can obscure long-term sea level rise trends and complicate detection and attribution.
Purpose of the Study:
- To quantify and map the contribution of TWS variability to decadal sea level variability.
- To improve the detection and attribution of anthropogenic sea level rise.
- To understand TWS impacts on future flooding and drought.
Main Methods:
- Utilized a suite of observational data.
- Quantified TWS variability's contribution to sea level variability on decadal timescales.
- Mapped the spatial relationship between TWS and sea level changes.
Main Results:
- Decadal sea level variability, particularly in the Pacific Ocean, is strongly linked to low-frequency TWS variability globally.
- Identified key global regions where TWS variability significantly influences sea level.
- Established a method to separate TWS-induced sea level variability from other trends.
Conclusions:
- Separating TWS variability is crucial for accurately detecting and attributing anthropogenic sea level rise.
- Understanding TWS-driven sea level fluctuations is essential for predicting future climate change impacts.
- This research provides a pathway to better understand climate-driven sea level changes and their consequences.
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