Seasonal to decadal dynamics of supraglacial lakes on debris-covered glaciers in the Khumbu region, Nepal

Lucas Zeller, D. McGrath, S. McCoy, J. Jacquet
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Abstract

Abstract. Supraglacial lakes (SGLs) play an important role in debris-covered glacier (DCG) systems by enabling efficient interactions between the supraglacial, englacial, and subglacial environments. Developing a better understanding of the short-term and long-term development of these features is needed to constrain DCG evolution and the hazards posed to downstream communities, ecosystems, and infrastructure from rapid drainage. In this study, we present an analysis of supraglacial lakes on eight DCGs in the Khumbu region of Nepal by automating SGL identification in PlanetScope, Sentinel-2, and Landsat 5–9 images. We identify a regular annual cycle in SGL area, with lakes covering approximately twice as much area during their maximum annual extent (in the pre-monsoon season) than their minimum annual extent (in the post-monsoon season). The high spatiotemporal resolution of PlanetScope imagery (∼ daily, 3 m) shows that this cycle is driven by the appearance and expansion of small lakes in the upper debris-covered regions of these glaciers throughout the winter. Decadal-scale expansion of large, near-terminus lakes was identified on four of the glaciers (Khumbu, Lhotse, Nuptse, and Ambulapcha), while the remaining four showed no significant increases over the study period. The seasonal variation in SGL area is of comparable or greater magnitude as decadal-scale changes, highlighting the importance of accounting for this seasonality when interpreting long-term records of SGL changes from sparse observations. The complex spatiotemporal patterns revealed in our analysis are not captured in existing regional-scale glacial lake databases, suggesting that more targeted efforts are needed to capture the true variability of SGLs on large scales.
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尼泊尔昆布地区碎屑覆盖冰川上的超冰川湖的季节至十年动态变化
摘要。超冰川湖(SGL)在碎屑覆盖冰川(DCG)系统中发挥着重要作用,使超冰川、冰川和冰川下环境之间能够有效互动。我们需要更好地了解这些地貌的短期和长期发展,以制约DCG的演化以及快速排水对下游社区、生态系统和基础设施造成的危害。在本研究中,我们通过自动识别 PlanetScope、哨兵-2 和 Landsat 5-9 图像中的超冰川湖,对尼泊尔昆布地区 8 个 DCG 上的超冰川湖进行了分析。我们发现,SGL 面积的年周期是有规律的,湖泊面积最大年周期(季风前季节)是湖泊面积最小年周期(季风后季节)的两倍。PlanetScope 图像的高时空分辨率(每天∼ 3 米)显示,这一周期是由这些冰川上部碎屑覆盖区整个冬季出现和扩大的小湖泊所驱动的。有四条冰川(昆布冰川、洛子峰冰川、努布齐峰冰川和安布拉巴查冰川)的大型近端点湖泊出现了十年尺度的扩张,而其余四条冰川在研究期间没有出现明显的扩张。SGL面积的季节性变化与十年尺度变化的幅度相当或更大,这突出表明了在解释来自稀少观测数据的SGL长期变化记录时考虑这种季节性的重要性。现有的区域尺度冰川湖数据库无法捕捉到我们的分析所揭示的复杂时空模式,这表明需要更有针对性的努力来捕捉大尺度 SGL 的真实变化。
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