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Non-linear quickflow response as indicators of runoff generation mechanisms

Publication ,  Journal Article
Scaife, CI; Singh, NK; Emanuel, RE; Miniat, CF; Band, LE
Published in: Hydrological Processes
June 30, 2020

Linking quickflow response to subsurface state can improve our understanding of runoff processes that drive emergent catchment behaviour. We investigated the formation of non-linear quickflows in three forested headwater catchments and also explored unsaturated and saturated storage dynamics, and likely runoff generation mechanisms that contributed to threshold formation. Our analyses focused on two reference watersheds at the Coweeta Hydrologic Laboratory (CHL) in western North Carolina, USA, and one reference watershed at the Susquehanna Shale Hills Critical Zone Observatory (SHW) in Central Pennsylvania, USA, with available hourly soil moisture, groundwater, streamflow, and precipitation time series over several years. Our study objectives were to characterise (a) non-linear runoff response as a function of storm characteristics and antecedent conditions, (b) the critical levels of shallow unsaturated and saturated storage that lead to hourly flow response, and (c) runoff mechanisms contributing to rapidly increasing quickflow using measurements of soil moisture and groundwater. We found that maximum hourly rainfall did not significantly contribute to quickflow production in our sites, in contrast to prior studies, due to highly conductive forest soils. Soil moisture and groundwater dynamics measured in hydrologically representative areas of the hillslope showed that variable subsurface states could contribute to non-linear runoff behaviour. Quickflow generation in watersheds at CHL were dominated by both saturated and unsaturated pathways, but the relative contributions of each pathway varied between catchments. In contrast, quickflow was almost entirely related to groundwater fluctuations at SHW. We showed that co-located measurements of soil moisture and groundwater supplement threshold analyses providing stronger prediction and understanding of quickflow generation and indicate dominant runoff processes.

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Published In

Hydrological Processes

DOI

EISSN

1099-1085

ISSN

0885-6087

Publication Date

June 30, 2020

Volume

34

Issue

13

Start / End Page

2949 / 2964

Related Subject Headings

  • Environmental Engineering
  • 4005 Civil engineering
  • 3709 Physical geography and environmental geoscience
  • 3707 Hydrology
  • 0907 Environmental Engineering
  • 0905 Civil Engineering
  • 0406 Physical Geography and Environmental Geoscience
 

Citation

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Scaife, C. I., Singh, N. K., Emanuel, R. E., Miniat, C. F., & Band, L. E. (2020). Non-linear quickflow response as indicators of runoff generation mechanisms. Hydrological Processes, 34(13), 2949–2964. https://doi.org/10.1002/hyp.13780
Scaife, C. I., N. K. Singh, R. E. Emanuel, C. F. Miniat, and L. E. Band. “Non-linear quickflow response as indicators of runoff generation mechanisms.” Hydrological Processes 34, no. 13 (June 30, 2020): 2949–64. https://doi.org/10.1002/hyp.13780.
Scaife CI, Singh NK, Emanuel RE, Miniat CF, Band LE. Non-linear quickflow response as indicators of runoff generation mechanisms. Hydrological Processes. 2020 Jun 30;34(13):2949–64.
Scaife, C. I., et al. “Non-linear quickflow response as indicators of runoff generation mechanisms.” Hydrological Processes, vol. 34, no. 13, June 2020, pp. 2949–64. Scopus, doi:10.1002/hyp.13780.
Scaife CI, Singh NK, Emanuel RE, Miniat CF, Band LE. Non-linear quickflow response as indicators of runoff generation mechanisms. Hydrological Processes. 2020 Jun 30;34(13):2949–2964.
Journal cover image

Published In

Hydrological Processes

DOI

EISSN

1099-1085

ISSN

0885-6087

Publication Date

June 30, 2020

Volume

34

Issue

13

Start / End Page

2949 / 2964

Related Subject Headings

  • Environmental Engineering
  • 4005 Civil engineering
  • 3709 Physical geography and environmental geoscience
  • 3707 Hydrology
  • 0907 Environmental Engineering
  • 0905 Civil Engineering
  • 0406 Physical Geography and Environmental Geoscience