Streamflow generation in a large, alpine watershed in the southern Rocky Mountains of Colorado: Is streamflow generation simply the aggregation of hillslope runoff responses?

Water Resources Research

Volumn 47, Issue 6, 2011, Pages

  Frisbee, Marty D ^a,b   Phillips, Fred M ^b   Campbell, Andrew R ^b   Liu, Fengjing ^c   Sanchez, Steve A ^d  

^a AMEC FOSTER WHEELER   (United States)

^b NEW MEXICO INSTITUTE OF MINING AND TECHNOLOGY   (United States)

^c LINCOLN UNIVERSITY   (United States)

^d BLM/USFS   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ALPINE WATERSHED; CHEMICAL CONSTITUENTS; CONCEPTUAL MODEL; DRAINAGE AREA; END-MEMBER MIXING ANALYSIS; GENERATION PROCESS; HILLSLOPES; HYDRAULIC HEADS; ROCKY MOUNTAINS; RUNOFF RESPONSE; SHALLOW SUBSURFACE; SMALL CATCHMENT; SPATIAL SCALE; STREAM CHEMISTRY; STREAMBEDS; TEMPORAL TRENDS; WATERSHED SCALE;

AGGLOMERATION; CATCHMENTS; GROUNDWATER; GROUNDWATER FLOW; LANDFORMS; RUNOFF; THREE DIMENSIONAL; TWO DIMENSIONAL; WATERSHEDS;

STREAM FLOW;

ALPINE ENVIRONMENT; CATCHMENT; DRAINAGE; GEOACCUMULATION; GROUNDWATER FLOW; HILLSLOPE; HYDRAULIC CONDUCTIVITY; HYDROLOGICAL RESPONSE; MAGNITUDE; NUMERICAL MODEL; OBSERVATIONAL METHOD; RUNOFF; SPATIOTEMPORAL ANALYSIS; STREAMFLOW; THREE-DIMENSIONAL MODELING; TWO-DIMENSIONAL MODELING; WATERSHED;

ROCKY MOUNTAINS;

EID: 79959517596     PISSN: 00431397     EISSN: None     Source Type: Journal    
DOI: 10.1029/2010WR009391     Document Type: Article

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