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Title: Functional approach to exploring climatic and landscape controls on runoff generation: 2 Timing of runoff storm response

Journal Article · · Water Resources Research
DOI:https://doi.org/10.1002/2014WR016308· OSTI ID:1837456
 [1];  [2]
  1. Hydrology Technical Group, Pacific Northwest National Laboratory Richland Washington USA
  2. Department of Civil and Environmental Engineering University of Illinois at Urbana‐Champaign, Hydrosystems Laboratory Urbana Illinois USA, Department of Geography and Geographic Information Science University of Illinois at Urbana‐Champaign Champaign Illinois USA

Abstract Hortonian overland flow, Dunne overland flow, and subsurface stormflow are the three most dominant mechanisms contributing to both the volume and timing of streamflow in headwater catchments. In this paper, guided by the Dunne diagram, we explore the impacts of climate, soil, and topography on estimated probability distributions of the travel times of each of these three runoff components. In each case, these are expressed in terms of the Connected Instantaneous Response Functions (CIRF) and account for the dynamics of their individual partial effective contributing areas that retain the connectivity to the outlet (instead of the whole catchment area). A spatially distributed hydrological model is used to derive the CIRFs numerically under multiple combinations of climate, soil, and topographic properties. The mean travel times and dimensionless forms of the CIRFs (i.e., scaled by their respective mean travel times) are used to examine both advective and dispersive aspects of catchment's runoff routing response. It is found that the CIRFs, upon nondimensionalization, collapsed to common characteristic shapes, which could be explained in terms of the relative contributions of hillslope and channel network flows, and the size of runoff contributing areas. The contributing areas, particularly for the Dunne overland flow, are themselves found to be governed by the competition between drainage of and recharge to the water table, and could be explained by a dimensionless drainage index which quantifies this competition. The study also reveals simple indicators based on landscape properties that can explain the magnitude of travel times in different catchments.

Sponsoring Organization:
USDOE
Grant/Contract Number:
AC06-76RLO1830; AC06-76RL01830
OSTI ID:
1837456
Journal Information:
Water Resources Research, Journal Name: Water Resources Research Vol. 50 Journal Issue: 12; ISSN 0043-1397
Publisher:
American Geophysical Union (AGU)Copyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 7 works
Citation information provided by
Web of Science

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