4.6 Article

Global Attribution of Runoff Variance Across Multiple Timescales

Journal

JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
Volume 124, Issue 24, Pages 13962-13974

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2019JD030539

Keywords

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Funding

  1. China National Key RD Program [2019YFA0606900]
  2. National Science Foundation for Distinguished Young Scholars of China [51425903]
  3. China Postdoctoral Science Foundation [BX20190301]
  4. Nature Science Foundation of Hubei Province [2019CFB221]
  5. Fund for Creative Research Groups of National Natural Science Foundation of China [41621061]
  6. National Science Foundation of China [41771536, 41901041]
  7. National Natural Science Foundation of China [41871029]
  8. Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) [162301182729]
  9. open funding of the State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS [SKLLQG1849]

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Previous findings on the relative importance of driving factors to runoff have been controversial, and the relative contribution of driving factors behind the temporal variance of runoff (Rv) still remains unquantified at a global scale. Here, we present a new framework to quantify the driving factors behind Rv globally by decomposing Rv into the temporal variance of precipitation (P), potential evapotranspiration (E-0), total water storage change ( increment S), and other factors (represented by n in Budyko equation), such as climate seasonality, land cover, and human impact, at intra-annual, interannual, and multiannual timescales. The results reveal that P controls Rv at different timescales in most parts of the globe. P has distinctly larger impacts on Rv in humid basins at the multiannual scale, while other factors have larger impacts in arid basins. We highlight the different impacts of driving factors on Rv at multiple timescales, which contradicts previous global assessments that assess the relative importance by sensitivity.

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