Splinter, D. K., D. C. Dauwalter, R. A. Marston, and W. L. Fisher. 2011. Watershed morphology of highland and moutain ecoregions in eastern Oklahoma. The Professional Geographer 63:1-13.
Abstract
The fluvial system represents a nested hierarchy that reflects the relationship among different spatial and
temporal scales. Within the hierarchy, larger scale variables influence the characteristics of the next lower
nested scale. Ecoregions represent one of the largest scales in the fluvial hierarchy and are defined by recurring
patterns of geology, climate, land use, soils, and potential natural vegetation. Watersheds, the next largest
scale, are often nested into a single ecoregion and therefore have properties that are indicative of a given
ecoregion. Differences in watershed morphology (relief, drainage density, circularity ratio, relief ratio, and
ruggedness number) were evaluated among three ecoregions in eastern Oklahoma: Ozark Highlands, Boston
Mountains, and OuachitaMountains. These ecoregions were selected because of their high-quality stream resources
and diverse aquatic communities and are of special management interest to theOklahomaDepartment
of Wildlife Conservation. One hundred thirty-four watersheds in first- through fourth-order streams were
compared. Using a nonparametric, two-factor analysis of variance (α = 0.05) we concluded that the relief,
drainage density, relief ratio, and ruggedness number all changed among ecoregion and stream order, whereas
circularity ratio only changed with stream order. Our study shows that ecoregions can be used as a broad-scale
framework for watershedmanagement.