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<br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br />1 <br /> <br /> <br />1 <br />1 <br /> <br /> <br /> <br />1 <br />We derived two base maps from different data sources: a 1993 Landsat thematic mapper <br />(TM) image at a resolution of 30 meters, and low-altitude aerial photographs at a resolution of 2 <br />meters. Base maps serve as points of reference for identifying and quantifying changes in the <br />size and distribution of vegetation types. Because digital analysis is more efficient, and often <br />more accurate, than manual interpretation (Snook et al. 1987), aerial photographs were scanned <br />and processed for digital analysis. Rectification of the digital photographs against 1:24,000 <br />orthophotographs corrected for areal distortion. Due to the data-intensity of high-resolution <br />photographs, only floodplain restoration sites were included in the analysis. TM imagery was <br />obtained in digital form and was pre-processed to adjust for atmospheric distortion. Analysis of <br />the TM data included the area between the Bonanza and Ouray bridges. Both data types were <br />classified with an unsupervised classification algorithm, which divides reflectance data into <br />classes that are spectrally similar and makes no a priori assumptions about the reflectance data. <br />Field data were collected to identify the vegetation types represented by each spectral <br />class. Between July 1996 and August 1998, ground-truth data were collected from 235 plots <br />within the study area. Variables included geographic location, plot size and configuration, <br />relative soil brightness, a list of species present at greater than 5% cover, and ocular estimates of <br />average height and percent cover for each species. Ocular estimation methods were chosen for <br />two reasons. First, they require much less time than traditional transect or quadrat methods. <br />Second, unlike more traditional survey methods, ocular methods do not imply that vegetative <br />cover is static and known to the nearest percentage (Daubenmire 1959). Vegetative cover may <br />change significantly within the growing season, and from one season to the next. <br />Eighty-five of the 235 plots were used for classification of the TM data. These plots were <br />at least 90 by 90 meters to ensure that the sampling frame was large enough to be accurate at the <br />resolution of the TM data. All 235 plots were used to develop the map based on aerial <br />photographs. To identify the vegetation type represented by each spectral class, the spectral <br />classes created by the unsupervised classification algorithm were summarized with field plot <br />locations in a geographic information system. Each pixel was classified into one of the <br />following eight cover types based on the dominant vegetation type: <br />1) Water <br />2) Emergent vegetation (Carex and Typha sps.) <br />3) Native tree (Populus sps.) <br />4) Exotic tree (Elaeagnus angustifolia) <br />5) Native shrub (Salix sps., Rhus trilobatum) <br />6) Exotic shrub (Tamarix ramosissima) <br />7) Native terrestrial herb (many species) <br />8) Exotic terrestrial herb (primarily Lepidium latifolium, Centaurea repens) <br />The TM data was further classified into 17 vegetation types (see Table 3.1). The overall ' <br />accuracy of each classification was assessed by generating 100 random points, and comparing <br />the classified vegetation type with the actual vegetation type at those points. All digital analy <br />were performed in ERDAS/Imagine 8.2. <br />a <br />22