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Channel and Perennial Flow Initiation in Headwater Streams: Management Implications of Variability in Source-Area Size

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Abstract

Despite increasing attention to management of headwater streams as sources of water, sediment, and wood to downstream rivers, the extent of headwater channels and perennial flow remain poorly known and inaccurately depicted on topographic maps and in digital hydrographic data. This study reports field mapping of channel head and perennial flow initiation locations in forested landscapes underlain by sandstone and basalt lithologies in Washington State, USA. Contributing source areas were delineated for each feature using a digital elevation model (DEM) as well as a Global Positioning System device in the field. Systematic source area–slope relationships described in other landscapes were not evident for channel heads in either lithology. In addition, substantial variability in DEM-derived source area sizes relative to field-delineated source areas indicates that in this area, identification of an area–slope relationship, should one even exist, would be difficult. However, channel heads and stream heads, here defined as the start of perennial flow, appear to be co-located within both of the lithologies, which together with lateral expansion and contraction of surface water around channel heads on a seasonal cycle in the basalt lithology, suggest a controlling influence of bedrock springs for that location. While management strategies for determining locations of channel heads and perennial flow initiation in comparable areas could assign standard source area sizes based on limited field data collection within that landscape, field-mapped source areas that support perennial flow are much smaller than recognized by current Washington State regulations.

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References

  • Abrahams AD (1980) Channel link density and ground slope. Ann Assoc Am Geogr 70:80–93

    Article  Google Scholar 

  • Anderson SP, Dietrich WE, Montgomery DR, Torres R, Conrad ME, Loague K (1997) Subsurface flow paths in a steep, unchanneled catchment. Water Resources Res 33:2637–2653

    Article  Google Scholar 

  • Asano Y, Uchida T, Ohte N (2002) Residence times and flow paths of water in steep unchannelled catchments, Tanakami, Japan. J Hydrol 261:173–192

    Article  Google Scholar 

  • Bischetti GB, Gandolfi C, Whelan MJ (1998) The definition of stream channel head location using digital elevation data. 1998. In Kovar K, Tappeiner U, Peters NE, Craig RG (eds.) Hydrology, water resources and ecology in headwaters. International Association of Hydrological Sciences publication no. 248, Pages 545–552

  • Climate Summaries Data (2003) Available at http://www.wrcc.dri.edu/summary/climsmwa.html. Accessed on September 15, 2003

  • Daly C, Neilson RP, Phillips DL (1994) A statistical-topographic model for mapping climatological precipitation over mountainous terrain. J Appl Meteorol 33:140–158; http://www.ocs.orst.edu/prism/prism_new.html

    Article  Google Scholar 

  • Dietrich WE, Dunne T (1993) The channel head. In Beven K, Kirkby MJ (eds.) Channel network hydrology. John Wiley & Sons Ltd, Pages 175–218

  • Dietrich WE, Reneau SL, Wilson CJ (1987) Overview: “zero-order basins” and problems of drainage density, sediment transport and hillslope morphology. In Beschta RL (ed.) Erosion and sedimentation in the Pacific Rim International Association of Hydrological Sciences, Pages 27–37

  • Dietrich WE, Wilson CJ, Reneau SL (1986) Hollows, colluvium, and landslides in soil-mantled landscapes. In Abrahams AD (ed.) Hillslope processes. Allen and Unwin, London, Pages 361–388

    Google Scholar 

  • Dietrich WE, Wilson CJ, Montgomery DR, McKean J (1993) Analysis of erosion thresholds, channel networks, and landscape morphology using a digital terrain model. J Geol 101:259–278

    Article  Google Scholar 

  • Dietrich WE, Wilson CJ, Montgomery DR, McKean J, Bauer R (1992) Erosion thresholds and land surface morphology. Geology 20:675–679

    Article  Google Scholar 

  • Dunne T (1980) Formation and controls of channel networks. Progr Phys Geogr 4:211–239

    Article  Google Scholar 

  • Dunne T (1990) Hydrology, mechanics, and geomorphic implications of erosion by subsurface flow. In Higgins CG, Coates DR (eds.) Groundwater Geomorphology, Pages 1–28

  • Freer J, McDonnell JJ, Beven K, Burns D, Hooper R, Aulenbach B, Kendall C, Peters N (2002) Understanding the spatial and temporal dynamic contributions of subsurface storm runoff at the hillslope scale. Water Resources Res 38:1269–1284

    Article  Google Scholar 

  • Gandolfi C, Bischetti GB (1997) Influence of drainage network identification method on geomorphological properties and hydrological response. Hydrolog Processes 11:353–375

    Article  Google Scholar 

  • Gomi T, Sidle RC, Richardson JS (2002) Understanding processes and downstream linkages of headwater systems. BioScience 52:905–916

    Article  Google Scholar 

  • Gomi T, Sidle RC, Swanson DN (2004) Hydrogeomorphic linkages of sediment transport in headwater streams, Maybeso Experimental Forest, southeast Alaska. Hydrolog Processes 18:667–683

    Article  Google Scholar 

  • Hewlett JD, Hibbert AR (1967) Factors affecting the response of small watersheds to precipitation in humid areas. In Sopper WE, Lull HW (eds.) International symposium on forest hydrology. Pergamon, New York, Pages 275–290

    Google Scholar 

  • Hunter MA, Quinn T, Hayes MP (2005) Low flow spatial characteristics in forested headwater channels of Southwest Washington. J Am Water Resources Assoc 41:503–516

    Article  Google Scholar 

  • Jones JA, Swanson FJ, Wemple BC, Snyder KU (2000) Effects of roads on hydrology, geomorphology, and disturbance patches in stream networks. Conserv Biol 14:76–85

    Article  Google Scholar 

  • LaMarche J, Lettenmaier DP (2001) Effects of forest roads on flood flows in the Deschutes River Basin, Washington. Earth Surf Processes Landforms 26:115–134

    Article  Google Scholar 

  • Lasmanis RL (1991) The geology of Washington. Rocks Minerals 66:262–277

    Google Scholar 

  • Logan RL (1987a) Geologic map of the Chehalis River and Westport Quadrangles, Washington. Olympia, Washington Division of Geology and Earth Resources, OFR-87-8, 1 sheet, Scale 1:100,000

  • Logan RL (1987b) Geologic map of the south half of the Shelton and south half of the Copalis Beach Quadrangles, Washington

  • May CL, Gresswell RE (2003) Processes and rates of sediment and wood accumulation in headwater streams of the Oregon Coast Range, USA. Earth Surf Processes Landforms 28:409–424

    Article  Google Scholar 

  • McDonnell JJ (2003) Where does water go when it rains? Moving beyond the variable source area concept of rainfall-runoff response. Hydrolog Processes 17:1869–1875

    Article  Google Scholar 

  • Montgomery DR (1994) Road surface drainage, channel-initiation, and slope instability. Water Resources Res 30:1925–1932

    Article  Google Scholar 

  • Montgomery DR, Dietrich WE (1995) Hydrologic processes in a low-gradient source area. Water Resources Res 31:1–10

    Article  Google Scholar 

  • Montgomery DR, Foufoula-Georgiou E (1993) Channel network source representation using digital elevation models. Water Resources Res 29:3925–3934

    Article  Google Scholar 

  • Montgomery DR, Dietrich WE (1988) Where do channels begin? Nature 336:232–234

    Article  Google Scholar 

  • Montgomery DR, Dietrich WE (1989) Source areas, drainage density, and channel-initiation. Water Resources Res 25:1907–1918

    Article  Google Scholar 

  • Montgomery DR, Dietrich WE (1992) Channel-initiation and the problem of landscape scale. Science 255:826–830

    Article  CAS  Google Scholar 

  • Montgomery DR, Dietrich WE (1994) Landscape dissection and drainage area-slope thresholds. In Kirkby MJ (ed.) Process models and theoretical geomorphology. John Wiley and Sons Ltd., pp 221–246

  • Montgomery DR, Dietrich WE (2002) Runoff generation in a steep, soil-mantled landscape. Water Resources Res 38:1168–1175

    Google Scholar 

  • Montgomery DR, Dietrich WE, Heffner JT (2002) Piezometric response in shallow bedrock at C1B: implications for runoff generation and landsliding. Water Resources Res 38:1274–1291

    Google Scholar 

  • Montgomery DR, Dietrich WE, Torres R, Anderson SP, Heffner JT, Loague K (1997) Hydrologic response of a steep, unchanneled valley to natural and applied rainfall. Water Resources Res 33:91–109

    Article  Google Scholar 

  • Ness AO (1958) Soil survey of Thurston County, Washington. Soil Conservation Service

    Google Scholar 

  • Pringle RF (1986) Soil survey of Grays Harbor Area, Pacific County, and Wahkiakum County, Washington. Soil Conservation Service

  • Prosser I, Abernethy B (1996) Predicting the topographic limits to gully network using a digital terrain model and process thresholds. Water Resources Res 32:2289–2298

    Article  Google Scholar 

  • Prosser I, Soufi M (1998) Controls on gully formation following forest clearing in a humid temperate environment. Water Resources Res 34:3661–3671

    Article  Google Scholar 

  • Rivenbark BL, Jackson CR (2004) Average discharge, perennial flow initiation, and channel initiation—small Southern Appalachian basins. J Am Water Resources Assoc 40:639–646

    Article  Google Scholar 

  • Shreve RL (1969) Stream lengths and basin areas in topographically random channel networks. J Geol 77:397–414

    Article  Google Scholar 

  • Smakhtin VU (2001) Low flow hydrology: A review. J Hydrol 240:147–186

    Article  Google Scholar 

  • TFWC (Timber, Fish and Wildlife Committee) (1999) Forests and fish report. Washington State Department of Natural Resources: WAC 222–Forest Practices Rules. Available at http://www.dnr.wa.gov/forestpractices/rules/forestandfish.pdf Accessed on September 15, 2005

    Google Scholar 

  • Tucker GE, Bras RL (1998) Hillslope processes, drainage density, and landscape morphology. Water Resources Res 34:2751–2764

    Article  Google Scholar 

  • USGS (1981) Topographic map of Summit Lake Quadrangle, Washington. 1:24,000

  • USGS (1986) Topographic map of Menlo Quadrangle, Washington. 1:24,000

  • USGS (1993) Topographic map of Littlerock Quadrangle, Washington. 1:24,000

  • USGS (1994a) Topographic map of East of Raymond Quadrangle, Washington. 1:24,000

  • USGS (1994b) Topographic map of Dean Creek Quadrangle, Washington. 1:24,000

  • Vandekerckhove L, Poesen J, Oostwoud WijDenes D, Nachtergaele J, Kosmas D, Roxo MJ, De Figueredo T (2000) Thresholds for gully initiation and sedimentation in Mediterranean Europe. Earth Surface Processes Landforms 25:1201–1220

    Article  Google Scholar 

  • Wemple BC, Jones JA, Grant GE (1996) Channel network extension by logging roads in two basins, Western Cascades Oregon. Water Resources Bull 32:1195–1207

    Article  Google Scholar 

  • WFPB (Washington Forest Practices Board) (2002) Washington State Forest Practices Rules. Section 222-16-030: water typing system, contained in WAC 222-16—definitions and RMAP emergency rule. Washington State Department of Natural Resources. Available at http://www.dnr.wa.gov/forestpractices/rules Accessed on September 15, 2005

  • Wilkins RN, Peterson NP (2000) Factors related to amphibian occurrence and abundance in headwater streams draining second-growth Douglas-fir forests in southwestern Washington. Forest Ecol Manage 129:79–91

    Article  Google Scholar 

  • Zar JH (1999) Biostatistical analysis. 4th ed. Prentice Hall, New Jersey

    Google Scholar 

Download references

Acknowledgments

The Washington Department of Natural Resources provided funding for this project. The authors would like to thank Ellen Wohl for reviewing earlier drafts, and also appreciate the comments of C.R. Jackson and Brian Nerbonne.

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Correspondence to Kristin L. Jaeger.

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Jaeger, K.L., Montgomery, D.R. & Bolton, S.M. Channel and Perennial Flow Initiation in Headwater Streams: Management Implications of Variability in Source-Area Size. Environmental Management 40, 775–786 (2007). https://doi.org/10.1007/s00267-005-0311-2

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