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Updated: Oct 29, 2025

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
Published on: June 8, 2015
Attribution of streamflow changes across the globe based on the Budyko framework
Jianyu Liu1, Yuanyuan You2, Qiang Zhang3
1Laboratory of Critical Zone Evolution, School of Geography and Information Engineering, China University of Geosciences, Wuhan 430074, China; State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, China; State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan 430074, China.
Global streamflow changes are driven by factors beyond precipitation and evaporation. Using observed data reveals that other influences, like vegetation and human impact, are dominant, challenging previous findings from reconstructed data.
Area of Science:
- Hydrology
- Environmental Science
- Climate Change Research
Background:
- Understanding streamflow change drivers is crucial for predicting hydrological responses to environmental shifts.
- Global assessments of streamflow change attribution are debated due to limited hydrological station data.
- Previous studies often rely on reconstructed streamflow data, potentially leading to biased conclusions.
Purpose of the Study:
- To attribute observed global streamflow changes using a comprehensive dataset from 1960-2014.
- To compare attribution results from observed versus reconstructed streamflow data.
- To clarify the dominant factors influencing global streamflow variability.
Main Methods:
- Utilized the most comprehensive dataset available for global streamflow attribution.
- Analyzed streamflow changes between 1960 and 2014.
- Compared attribution results derived from observed streamflow data against those from reconstructed datasets.
Main Results:
- Factors other than precipitation (P) and potential evaporation (E0) were found to be the dominant drivers of observed global streamflow changes (48.9-50.9% of stations).
- Reconstructed streamflow datasets indicated precipitation as the dominant factor (72.3-72.9% of stations), contrasting with results from observed data.
- Attribution using reconstructed data may overestimate precipitation's role and underestimate other factors like vegetation and human impacts.
Conclusions:
- Observed streamflow data is essential for accurate attribution of streamflow changes, avoiding biases inherent in reconstructed datasets.
- Non-precipitation/evaporation factors significantly influence streamflow, with notable regional variations.
- This study underscores the need for empirical data in hydrological research to prevent skewed scientific understanding.
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