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WSP11909
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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 />An accuracy assessment of UDAR data acquired over Atlantic coastal beaches abo showed <br />LIDAR dala to he parallel 10. but oflset from. the true ."Jur/lce (Shrestha el al.. 19QQ). Thc obse("\ed <br />offst"ts ranged from +0.20 m to -0.10 m. The ohse("\'ed oflSefs r-ere used to adjust the U[)AR data down <br />or up to the true ground surface. This adjustment approach could be l'mploy ed in the Grand Canyon. but <br />(he approach \\ould require careful selection of the "ground truth". points 10 maKe thc adjustmenls. The <br />ground truth points would ha\e 10 tle much larger in area than the hori1olllal positional accuracy of <br />UDAR and the elevations of the ground truth points "ould have to t.: stable. similar to a lopographic <br />control networK. <br /> <br />Assuming that elevation otTsels could be accurately dc-tennined in an operational sense lor <br />UDAR data acquired in the Grand Cany(m. \.loe applied the elevation offsets found at each study area (0 <br />Iheir respecti\c L1D..\R data and recomputed the elevation errors at each sludy area. The adjusted <br />ele\'alion errors for the RAMS L1DAR data are lo\\er than their unadjusted elevation errors in all the <br />stud~ areas; the adjusted elevation errors range from 0.06 In to 0.17 m n able :2). In contrast. the adjusted <br />elevation errors for the ALMS L1DAR data are nearly Ihe same as the unadjusted error values at most <br />sites (ranging from 0.:21 m to a.85m: Table 2). This disparily bct""een the datasets reflects the- fact that the <br />RAf\.IS UDAR data has a consistent parallel otTset from the surface (and is therefore potentially <br />correctable). \\hile the A Lf\'1S L1DAR data Iluctuates in an inconsistent manner Ihal maKes it impossiblt.' <br />10 appl~ a correction factor. <br /> <br />fJoo.'"-____....'.1 <br /> <br />~ <br /> <br />-- <br />j <br />! <br />i- <br />! <br />'- <br />j <br />I <br />'- <br /> <br />c..-_.... O......,~I-.....UIM._....,.}V' "". <br />.'Il' <br />R'_O...... <br /> <br />.' <br /> <br />,.' <br /> <br />~' <br />- <br /> <br />- <br /> <br />- - <br />....,L<oO<_,_....' <br /> <br />- <br /> <br />- <br /> <br />1....-............-........'.1 <br /> <br />., <br /> <br /> <br />~- <br />. <br />. <br />'- <br />! <br />; <br /> <br />u,,___... .......,U..~UD............ '""'. <br />..110 <br />"'0'" <br /> <br />;- <br />. <br />I <br />,- <br /> <br /> <br />"' <br />., <br /> <br />- <br /> <br />- - <br />......."........_-~... <br /> <br />"' <br /> <br />"' <br /> <br />fWW': c....,p..-.....'" ~l\l, ..dlt...\lSLln,~R ond..-~......... ok>........htw. <br />~~ ..>I<ool' .nR\I:" f..,..""'........,..""",......"...:I'o~~.....~ ~"."""I"'" <br />ho.,..lIDAR 1""'" .dh..O ~",""",ci....o.N""''''' r<><n 8\... h"'I<J""e><tt<.,,"_, <br />f"ci","rk-"~ f1luoh...~......~<"'~._....,,""...".1ao..... <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />6 <br /> <br />I <br />
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