维德玛冰川末端运动分析的计算机视觉方法

E. Moya-Albor, Armin Schwartzman, J. Brieva, Mauricio Pardo, Hiram Ponce, Rodrigo Chávez-Domínguez
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引用次数: 0

摘要

本文提出了一种自动分割Viedma冰川终点的方法。该方法使用来自Landsat-5卫星的多光谱图像,通过计算机视觉技术确定冰川的面积。估算冰川面积,拟合线性模型,得到实测面积与拟合线性回归模型的相关系数为0.968。另一方面,采用生物启发的光流估计方法来计算和可视化冰川随时间的位移。此外,还分析了南锥的温度变化与冰川的减少随时间的变化关系。线性趋势(r2=0.95)表明,在观测季节,冰川的分析面积每年减少约1.9%。它揭示了冰川大小的变化与全球变暖之间的反比关系,表明如果相同的条件保持不变,本研究分析的冰川带将在70年左右接近其消失,这一时间间隔将达到全球温度升高1.24 oC。
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A Computer Vision Approach to Terminus Movement Analysis of Viedma Glacier
In this paper, an automatic segmentation approach of the Viedma glacier terminus is proposed. The method uses multi-spectral images from the Landsat-5 satellite to determine the area of the glacier through computer vision techniques. The area of the glacier is estimated, and a linear model is fitted, obtaining a correlation of 0.968 between the measured area and a fit linear regression model. On the other hand, a bio-inspired optical flow estimation approach is used to calculate and visualize the displacement of the glacier through time. In addition, an analysis is performed between the temperature variation in the Southern Cone and the decrease of the glacier in the function of time. A linear trend (r2=0.95) shows that the analyzed area of the glacier has decreased by about 1.9% annually in the observation season. It reveals an inverse relationship between the change in the size of the glacier and global warming, showing that if the same conditions remain, the glacier’s zone analyzed in this work would be close to its disappearance in around 70 years, the time lapse in which a global temperature increase of 1.24 oC would be reached.
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