Ice velocities of the Lambert Glacier from static GPS observations
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概要
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Between 1988 and 1995, five seasons of Global Positioning System (GPS) data were collected at seventy-three locations near the 2500 metre contour of the Lambert Glacier Drainage Basin (LGB). These data have been processed using GAMIT/GlobK software to determine surface velocities at the surveyed sites. Results show that velocities along the traverse route vary between 0.5 ma-1 and 63 ma-1 with the location of the major outlet glaciers inside the LGB clearly identifiable within the data. A subset of the LGB GPS data has been studied to investigate an efficient method for determination of ice velocities at remote sites within a single field season. Results from this study have shown that ice velocities within 2% of the long-term estimate may be determined using two to four hour GPS site occupations separated in time by a minimum of forty days.
- 公益社団法人 日本地震学会、地球電磁気・地球惑星圏学会 、特定非営利活動法人 日本火山学会、日本測地学会、日本惑星科学会の論文
著者
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Morgan Peter
School Of Computing University Of Canberra
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KING Matt
Centre for Spatial Information Science, University of Tasmania
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COLEMAN Richard
Centre for Spatial Information Science, University of Tasmania
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Manson Rachael
Centre for Spatial Information Science, University of Tasmania
関連論文
- Treatment of horizontal and vertical tidal signals in GPS data: A case study on a floating ice shelf
- Ice velocities of the Lambert Glacier from static GPS observations
- Treatment of horizontal and vertical tidal signals in GPS data: A case study on a floating ice shelf
- Ice velocities of the Lambert Glacier from static GPS observations