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Sea Ice Topography Profiling using Laser Altimetry from Small Unmanned Aircraft Systems

机译:使用小型无人机系统的激光测高仪进行海冰地形分析

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摘要

Arctic sea ice is undergoing a dramatic transition from a perennial ice pack with a high prevalence of old multiyear ice, to a predominantly seasonal ice pack comprised primarily of young first-year and second-year ice. This transition has brought about changes in the sea ice thickness and topography characteristics, which will further affect the evolution and survivability of the ice pack. The varying ice conditions have substantial implications for commercial operations, international affairs, regional and global climate, our ability to model climate dynamics, and the livelihood of Arctic inhabitants. A number of satellite and airborne missions are dedicated to monitoring sea ice, but they are limited by their spatial and temporal resolution and coverage. Given the fast rate of sea ice change and its pervasive implications, enhanced observational capabilities are needed to augment the current strategies.The CU Laser Profilometer and Imaging System (CULPIS) is designed specifically for collecting fine-resolution elevation data and imagery from small unmanned aircraft systems (UAS), and has a great potential to compliment ongoing missions. This altimeter system has been integrated into four different UAS, and has been deployed during Arctic and Antarctic science campaigns. The CULPIS elevation measurement accuracy is shown to be 95 +/- 25 cm, and is limited primarily by GPS positioning error (u3c25 u3ecm), aircraft attitude determination error (u3c20 u3ecm), and sensor misalignment error (u3c20 u3ecm). The relative error is considerably smaller over short flight distances, and the measurement precision is shown to beprecision, the CULPIS is well suited for measuring sea ice topography, and observed ridge height and ridge separation distributions are found to agree with theoretical distributions to within 5%. Simulations demonstrate the inability of course-resolution measurements to accurately represent the theoretical distributions, with differences up to 30%. Future efforts should focus on reducing the total measurement error tochange.
机译:北极海冰正经历着从多年老冰盛行的多年生冰袋到主要由年轻的第一年和第二年冰组成的主要季节性冰袋的剧烈转变。这种转变带来了海冰厚度和地形特征的变化,这将进一步影响冰袋的演化和生存能力。不断变化的冰层条件对商业运营,国际事务,区域和全球气候,我们模拟气候动态的能力以及北极居民的生计都具有重大影响。许多卫星和空中飞行任务专用于监测海冰,但它们受到其时空分辨率和覆盖范围的限制。鉴于海冰变化的快速速度及其普遍性,需要增强观测能力以增强当前的策略.CU激光轮廓仪和成像系统(CULPIS)专为从小型无人飞机上采集高分辨率的高程数据和图像而设计系统(UAS),并且有很大的潜力可以补充正在进行的任务。该高度计系统已集成到四个不同的UAS中,并已在北极和南极科学运动中进行了部署。 CULPIS高程测量精度显示为95 +/- 25 cm,主要受GPS定位误差( u3c25 u3ecm),飞机姿态确定误差( u3c20 u3ecm)和传感器未对准误差( u3c20 u3ecm)。相对误差在短距离飞行中要小得多,并且测量精度被证明是精确的,CULPIS非常适合于测量海冰地形,并且发现观测到的山脊高度和山脊分离分布与理论分布一致,在5%以内。仿真表明,过程分辨率测量无法准确表示理论分布,相差高达30%。未来的工作应集中在减少总测量误差变化上。

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    Crocker Roger Ian;

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