| 2005 Salt Lake City Annual Meeting (October 16–19, 2005) | |
| Paper No. 203-8 | |
| Presentation Time: 10:00 AM-10:15 AM | ||
QUANTIFYING THE EFFECTS OF URBANIZATION ON TWO WATERSHEDS: HOW DOES DISCHARGE SCALE WITH DRAINAGE AREA IN AN URBAN AREA? | ||
|
GALSTER, Joshua C., Earth & Environmental Sciences, Lehigh University, 31 Williams Dr, Lehigh University, Bethlehem, PA 18015, jcg6@lehigh.edu and PAZZAGLIA, Frank J., Earth and Environmental Sciences, Lehigh University, 31 Williams Drive, Bethlehem, PA 18015 The negative influence of urbanization on streams is generally assumed, but poorly quantified. We select two contiguous watersheds in east-central Pennsylvania, the Little Lehigh River and Sacony Creek, with similar watershed area, annual precipitation, relief, and underlying substrate, but different amounts of urbanized land to test the dependence of discharge on drainage area. The Little Lehigh watershed has been rapidly urbanizing and now contains over 20% urbanized land, while the Sacony Creek watershed is mostly rural and has less than 5% urbanized land. Pressure sensors were installed in the trunk channels of each stream allowing a rating curve to be developed at each site. The sites were chosen to maximize the variation in upstream drainage area (A) in order to explore its influence on discharge (Q). Both base flow and peak discharges from storm events over several seasons were calculated for the two streams. Discharge grows as a power function with respect to area following the general equation Q = kAc, where k is a crude measure of stream baseflow, and c is the power dependency. For many watersheds, discharge scales linearly or nearly linearly with drainage area (c ~1). This simple relationship is assumed and enjoys widespread application in research including the stream power law for bedrock erosion. In our small watersheds, c varies from 1 to nearly 2, an effect that we attribute to degree of urbanization. To test this interpretation, we assemble several decades of USGS gage data on other, nearby watersheds to calculate c through time. Our results show systematic drift in the value of c that appears to track with changes in landuse, most notably, the increase in urbanization in these watersheds. Although in its initial phases, these trends in how discharge scales with drainage basin area could have major sedimentologic, ecologic, and geomorphic impacts on watersheds undergoing land use changes. | ||
|
2005 Salt Lake City Annual Meeting (October 16–19, 2005)
General Information for this Meeting | ||
| Session No. 203 Environmental Geoscience Salt Palace Convention Center: 254 B 8:00 AM-12:00 PM, Wednesday, 19 October 2005 Geological Society of America Abstracts with Programs, Vol. 37, No. 7, p. 454 | ||
© Copyright 2005 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions. | ||