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ANALYSIS OF GLACIER MASS BALANCE AND RHEOLOGY AT KEKESAYI GLACIER USING HEXAGON KH-9, ALOS-PRISM AND SAR DATA

机译:使用六边形KH-9,Alos-Prism和SAR数据分析Kekesayi冰川的冰川大量平衡和流变学

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Scanned stereoscopic spying photography of a Hexagon KH-9 mission in 1973 as well as high resolution stereo imagery of ALOS-PRISM from 2009 was used to generate multi-temporal Digital Terrain Models for the estimation of glacier thickness changes of Kekesayi glacier situated at the Mustag Ata massif at the northwestern end of the Tibetan Plateau. Glacier surface velocities were estimated by amplitude tracking techniques based on a TerraSAR-X data pair acquired in 2011. Preliminary results show ice thickness loss for the ablation area of this glacier of about -20 meters for the time period between 1973 and 2009. Surface velocities are reaching up to 15-25 cm per day at the upper part of the glacier in 2011, lowering significantly down in direction to the glacier tongue.
机译:1973年六角形KH-9使命的扫描立体间谍摄影以及2009年的Alos-Prism的高分辨率立体图像,用于估算位于Mistag的Kekesayi冰川冰川厚度变化的多时间数字地形模型ATA Massif在西北高原的西北地区。通过基于2011年获取的Terrasa-X数据对的幅度跟踪技术估算冰川表面速度。初步结果显示了1973年至2009年期间的时间段的该冰川的消融区域的冰厚度损失。表面速度2011年冰川上部达到每天高达15-25厘米,直向下降到冰川舌头的方向下降。

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