Annual trajectory of global glacial lake variations and the interactions with glacier mass balance during 2013–2022

IF 5.4 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
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Abstract

Global warming accelerates glacier melting and the growth of glacial lakes. Existing research on glacial lake changes primarily concentrates on specific regions or decadal timescales, impeding a comprehensive understanding of the spatial and temporal variation of glacial lakes. This study tracks the annual evolution of global glacial lakes larger than 1 km2 (totally 3,133) from 2013 to 2022 based on Landsat OLI imagery. We investigated the lake area variation and glacier mass balance to explore interactions between glacial lake expansion and glacier mass loss. We aim to reveal the potentially diverse changes in the area of glacial lakes in various regions and of different types over the past decade. Our results show that, for the study glacial lakes, the total area has increased remarkably from 14,612 ± 21.13 km2 to 15,034 ± 18.54 km2 from 2013 to 2022. Among them, the glacier-contacted lakes experienced a rapid increase from 6,220 km2 to 6,625 km2, contributing to ∼ 96 % of the net area increment of the glacial lakes worldwide, whereas non-glacier-contacted lakes remain relatively stable at approximately 8,400 km2. Overall, glacier-contacted lakes grew relatively fast in the sub-periods of 2013–2014 and 2018–2019 and maintained slightly slow growth in other years. Remarkable expansion of glacial lakes was observed in Alaska, Iceland, and New Zealand. The significant expansion of glacier-contacted lakes was primarily attributed to the water inundation sprawl upward to the glacier tongues, which accelerated melting rates of the mother glaciers as feedback. Our analysis of the trend and inter-annual variation of glacial lake area reveal contrasting evolution of glacial lakes in different regions and of different types, which serves as a key reference for comprehending the impact of climate change, the interaction between glaciers and glacial lakes, and mitigating natural disasters like glacial lake outbursts.

2013-2022 年全球冰川湖变化的年度轨迹以及与冰川质量平衡的相互作用
全球变暖加速了冰川融化和冰川湖的增长。现有的冰川湖变化研究主要集中在特定区域或十年时间尺度上,阻碍了对冰川湖时空变化的全面了解。本研究基于大地遥感卫星 OLI 图像,追踪了 2013 年至 2022 年全球 1 公里以上冰川湖泊(共 3,133 个)的年度变化。我们研究了湖泊面积变化和冰川质量平衡,以探索冰川湖泊扩张与冰川质量损失之间的相互作用。我们旨在揭示过去十年中不同地区、不同类型冰川湖泊面积的潜在多样性变化。我们的研究结果表明,从 2013 年到 2022 年,研究冰川湖泊的总面积从 14,612 ± 21.13 km 显著增加到 15,034 ± 18.54 km。其中,与冰川接触的湖泊从 6,220 km 快速增加到 6,625 km,占全球冰川湖泊净面积增量的 96%,而未与冰川接触的湖泊则相对稳定,约为 8,400 km。总体而言,与冰川接触的湖泊在 2013-2014 年和 2018-2019 年这两个子时期增长相对较快,在其他年份则保持略微缓慢的增长。阿拉斯加、冰岛和新西兰的冰川湖泊显著扩大。与冰川接触湖泊的显著扩大主要归因于水淹没向上蔓延至冰川舌,从而作为反馈加速了母冰川的融化速度。我们对冰川湖泊面积的变化趋势和年际变化的分析揭示了不同地区、不同类型冰川湖泊的对比演变,为理解气候变化的影响、冰川与冰川湖泊之间的相互作用以及减轻冰川湖泊溃决等自然灾害提供了重要参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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