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Assessing the Steady‐State Assumption in Water Balance Calculation Across Global Catchments
Author(s) -
Han Juntai,
Yang Yuting,
Roderick Michael L.,
McVicar Tim R.,
Yang Dawen,
Zhang Shulei,
Beck Hylke E.
Publication year - 2020
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1029/2020wr027392
Subject(s) - evapotranspiration , water balance , environmental science , streamflow , steady state (chemistry) , drainage basin , hydrology (agriculture) , precipitation , arid , aridity index , climatology , atmospheric sciences , meteorology , geology , geography , ecology , paleontology , chemistry , geotechnical engineering , cartography , biology
It has long been assumed that over a sufficiently long period of time, changes in catchment water storage (Δ S ) are a relatively minor term compared to other fluxes and can be neglected in the catchment water balance equation. However, the validity of this fundamental assumption has rarely been tested, and the associated uncertainties in water balance calculations remain unknown. Here, we use long‐term (1982–2011) observations of monthly streamflow ( Q ) and precipitation ( P ) for 1,057 global unimpaired catchments, combined with four independent evapotranspiration ( E ) estimates to infer Δ S and to provide a global assessment of the steady‐state assumption in catchment water balance calculations. Results show that when the threshold for steady state is set to 5% of the mean monthly P , ~70% of the catchments attain steady state within 10 years while ~6% of the catchments fail to reach a steady state even after 30 years. The time needed for a catchment to reach steady state ( τ s ) shows a close relationship with climatic aridity and vegetation coverage, with arid/semiarid and sparsely vegetated catchments generally having a longer τ s . Additionally, increasing snowfall fraction also increases τ s . The imbalance ( e wb ) caused by ignoring Δ S decreases as averaging period for water balance calculations increases as expected. For a typical 10‐year averaging period, e wb accounts for ~7% of P in arid, but that decreases to ~3% of P in humid catchments. These results suggest that catchment properties should be considered when applying the steady‐state assumption and call for caution when ignoring Δ S in arid/semiarid regions.