Calving front monitoring at a subseasonal resolution: a deep learning application for Greenland glaciers

Erik Loebel, M. Scheinert, M. Horwath, Angelika Humbert, Julia Sohn, Konrad Heidler, Charlotte Liebezeit, X. Zhu
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Abstract

Abstract. The mass balance of the Greenland Ice Sheet is strongly influenced by the dynamics of its outlet glaciers. Therefore, it is of paramount importance to accurately and continuously monitor these glaciers, especially the variation in their frontal positions. A temporally comprehensive parameterization of glacier calving is essential for understanding dynamic changes and constraining ice sheet modeling. However, many current calving front records are limited in terms of temporal resolution as they rely on manual delineation, which is laborious and not appropriate considering the increasing amount of satellite imagery available. In this contribution, we address this problem by applying an automated method to extract calving fronts from optical satellite imagery. The core of this workflow builds on recent advances in the field of deep learning while taking full advantage of multispectral input information. The performance of the method is evaluated using three independent test datasets. For the three datasets, we calculate mean delineation errors of 61.2, 73.7, and 73.5 m, respectively. Eventually, we apply the technique to Landsat-8 imagery. We generate 9243 calving front positions across 23 outlet glaciers in Greenland for the period 2013–2021. Resulting time series not only resolve long-term and seasonal signals but also resolve subseasonal patterns. We discuss the implications for glaciological studies and present a first application for analyzing the effect of bedrock topography on calving front variations. Our method and derived results represent an important step towards the development of intelligent processing strategies for glacier monitoring, opening up new possibilities for studying and modeling the dynamics of Greenland's outlet glaciers.
亚季节分辨率的褶皱前沿监测:格陵兰冰川的深度学习应用
摘要格陵兰冰原的质量平衡受到其出口冰川动态的强烈影响。因此,准确、持续地监测这些冰川,特别是其正面位置的变化至关重要。在时间上对冰川崩落进行全面参数化,对于了解动态变化和制约冰盖建模至关重要。然而,目前许多冰川塌陷前沿记录的时间分辨率有限,因为它们依赖于人工划定,而人工划定既费力又不合适,因为卫星图像的数量在不断增加。在本文中,我们采用一种自动方法从光学卫星图像中提取冰结锋面,从而解决了这一问题。该工作流程的核心建立在深度学习领域的最新进展之上,同时充分利用了多光谱输入信息。我们使用三个独立的测试数据集对该方法的性能进行了评估。对于这三个数据集,我们计算出的平均划分误差分别为 61.2 米、73.7 米和 73.5 米。最后,我们将该技术应用于 Landsat-8 图像。我们生成了 2013-2021 年期间格陵兰 23 个出口冰川的 9243 个冰川融化前沿位置。生成的时间序列不仅能解析长期和季节性信号,还能解析亚季节性模式。我们讨论了对冰川学研究的影响,并首次应用于分析基岩地形对冰川崩塌前沿变化的影响。我们的方法和推导结果代表了冰川监测智能处理策略发展的重要一步,为格陵兰出口冰川的动态研究和建模开辟了新的可能性。
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