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WSP11909
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Last modified
1/26/2010 3:19:15 PM
Creation date
10/12/2006 5:15:50 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8220.101.10.B
Description
Colorado River-Water Projects-Glen Canyon Dam/Lake Powell-Glen Canyon Adaptive Management-TWG
Basin
Colorado Mainstem
Water Division
5
Date
2/26/2003
Title
Packet for Distribution to TWG-GCMR Bibliography-Aerial Imagery Inventory-Remote Sensing Reports
Water Supply Pro - Doc Type
Report/Study
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<br />I <br /> <br />I <br /> <br />1506 <br /> <br />I <br /> <br />,. <br />Results <br /> <br />I <br /> <br />SlakeoUl Surveys <br /> <br />The average errors in the LI DAR elevation data are reported in Table I as two values: (I) the <br />average elevation offset between the L1DAR point elevations and the surveyed ground elevations and (2) <br />the average elevation error (accuracy) of the L1DAR data at a particular study area (determined by <br />averaging absolute elevation difference within a study site). The stakeout spot survey data for all bare <br />ground surfaces except rock ledges indicate that (I) the L1DAR elevations are generally higher than the <br />ground survey elevations, (2) the RAMS elevation data are consistently more accurate than the ALMS <br />elevation data, (3) the accuracy of the RAMS elevation data ranges from 0.12-0.23 m, except at RM 46 <br />and RM 59 where accuracies are 0.77 m and 0.53 m. respectively, and (4) the accuracy of the ALMS <br />elevation data ranges from 0.14-0.60 m. except at RM 45 where accuracy is 0.79 m. Both the RAMS and <br />ALMS systems claim an absolute vertical accuracy of 15 em. The stakeout survey showed that the <br />RAMS met or exceeded the contract specification of 15 cm at only two sites, while the ALMS met this <br />specification at only one site. <br /> <br />The cumulative elevation errors for all study areas for bare sand surfaces, boulder and cobble <br />surfaces, and for rock ledges revealed some counterintuitive results. One would expect that the uneven <br />boulder/cobble topographic surface would create greater vertical errors than the unifonn. flat sand <br />beaches. However. our findings show that the elevation errors for bare sand and boulder-cobble surfaces <br />have similar ranges and similar average error values (0.35 m for bare sand and 0.31 m for boulder-cobble <br />surfaces). The rock ledges at study area RM 59 have a higher elevation error (0.67 m) than the other bare <br />ground surfaces, which is anributed in part to the higher elevation errors found at study area RM 59 for all <br />types of surfaces (0.53 m for bare sand and boulder-cobble surfaces; Table I) and in part to uncertainties <br />in the exact horizontal location of the L1DAR pulse returns on the ledges with overhangs. <br /> <br />Sandbar mapping Surveys <br /> <br />Comparisons between sandbar mapping ground survey data and RAMS L1DAR data for the five <br />long-tenn monitoring areas were made by creating x-y scatter plots and frequency distributions of <br />elevation differences. An example is shown in Figure 2 for Site RM 2.8. The x-y scatter plots show that <br />the RAMS LI DAR point elevations are generally parallel to the ground survey elevations. except at study <br />areas RM 59 and RM 62.7, and that on average the RAMS L1DAR elevations are higher than the ground <br />survey elevations (0.09-0.28 m; Table 2). The average elevation errors for the five study areas range from <br />0.11 m to 0.28 m (Table 2), with only one site meeting the contract specification of 15 cm. Study area RM <br />59 has the sparsest sandbar mapping ground survey data and the highest elevation error (0.28 m), <br />however. this elevation error is much less than that found by the stakeout spot surveys conducted in the <br />study (0.53 m; Table I), <br /> <br />The ALMS elevation data for bare ground surfaces were similarly evaluated. The point distribution in its <br />x-y scatter plots show a more scattered distribution than that shown by the RAMS data. In addition, <br />unlike the RAMS data. the ALMS data is not generally parallel to the ground survey data and therefore <br />could not be corrected with a simple offset adjustment. For all study sites except one (RM 30 is offset by <br />-0.06m; Table 2). the ALMS elevations are higher than the ground survey data (0.06-0.75m; Table 2). <br />The average elevation errors for the five study areas range from 0.33m to 0.84 m (Table 2), with no sites <br />'\leeting the remtract specification of 15 cm. The ALMS elevation errors are significantly larger than the <br />RAMS errors, which correspond to the findings of the stakeout survey. <br /> <br />5 <br />
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