Hydrologic landscape regions (HLRs) in the United States were delineated
by using geographic information system (GIS) tools and statistical
methods including principal components and cluster analyses. The GIS and
statistical analyses were applied to land-surface form, geologic texture
(permeability of the soil and bedrock), and climate variables that
describe the physical and climatic setting of 43,931 small (roughly 200
square kilometers) watersheds in the United States. The analyses then
grouped the watersheds into 20 noncontiguous regions (the HLRs) on the
basis of similarities in land-surface form, geologic texture, and
climate characteristics.
This hydrologic landscape regions dataset contains for each of the
43,931 watersheds the (1) watershed identification number, (2)
land-surface form, geologic texture, and climate characteristics for
each watershed, and (3) hydrologic landscape region number for each watershed.
The HLRs derived in this study are specific to several choices made in
the analysis: (1) the particular set of variables used, (2) details in
the statistical analyses, and (3) details in the GIS analyses. Using a
different set of watershed characteristics would have affected the
derived HLR map. In addition, averaging the variables over smaller areas
would have produced a map with finer spatial detail. Changing any of
these factors likely would lead to other regional maps that could be
equally valid and useful.
The methods used to define HLRs are expected to be sensitive to the
spatial scale of the analysis. In the study described herein, the
spatial extent of the analysis covered all 50 States; this was the
appropriate spatial scale for the purpose of identifying HLRs to help
design a national water-quality assessment. Satisfying a different
objective may require a different spatial scale of analysis and might
result in a different set of regions.
The concept of hydrologic landscapes proposed by Winter (2001)
represents the natural landscape and climate factors expected to affect
hydrologic processes. There are important water-resources management
activities, such as reservoir and canal construction, irrigation, and
subsurface drainage, that have a significant effect on hydrologic
processes. These water-resources management activities were not included
as factors in defining the HLRs.
Cited references:
Winter, T.C., 2001, The concept of hydrologic landscapes: Journal of the
American Water Resources Association, v. 37, p. 335-349.