A national glacier inventory and variations in glacier extent in Iceland from the Little Ice Age maximum to 2019

IF 0.5 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY
Jokull Pub Date : 2021-12-08 DOI:10.33799/jokull2020.70.001
H. Hannesdóttir, O. Sigurðsson, R. Þrastarson, S. Guðmundsson, J. M. Belart, F. Pálsson, E. Magnússon, S. Víkingsson, I. Kaldal, T. Jóhannesson
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引用次数: 4

Abstract

A national glacier outline inventory for several different times since the end of the Little Ice Age (LIA) in Iceland has been created with input from several research groups and institutions, and submitted to the GLIMS (Global Land Ice Measurements from Space, nsidc.org/glims) database, where it is openly available. The glacier outlines have been revised and updated for consistency and the most representative outline chosen. The maximum glacier extent during the LIA was not reached simultaneously in Iceland, but many glaciers started retreating from their outermost LIA moraines around 1890. The total area of glaciers in Iceland in 2019 was approximately 10,400 km2, and has decreased by more than 2200 km2 since the end of the 19th century (corresponding to an 18% loss in area) and by approximately 750 km2 since ~2000. The larger ice caps have lost 10–30% of their maximum LIA area, whereas intermediate-size glaciers have been reduced by up to 80%. During the first two decades of the 21st century, the decrease rate has on average been approximately 40 km2 a-1. During this period, some tens of small glaciers have disappeared entirely. Temporal glacier inventories are important for climate change studies, for calibration of glacier models, for studies of glacier surges and glacier dynamics, and they are essential for better understanding of the state of glaciers. Although surges, volcanic eruptions and jökulhlaups influence the position of some glacier termini, glacier variations have been rather synchronous in Iceland, largely following climatic variations since the end of the 19th century.
从小冰期最大值到2019年,冰岛全国冰川清查和冰川范围变化
根据几个研究小组和机构的输入,冰岛小冰期(LIA)结束以来几个不同时期的国家冰川概要清单已经创建,并提交给GLIMS(全球陆地冰测量从空间,nsidc.org/glims)数据库,在那里它是公开可用的。冰川轮廓已被修订和更新,以保持一致性,并选择了最具代表性的轮廓。冰岛冰川并没有同时达到冰期的最大范围,但在1890年左右,许多冰川开始从冰期最外层的冰碛上退缩。2019年冰岛冰川总面积约为10400平方公里,自19世纪末以来减少了2200平方公里以上(相当于面积减少了18%),自2000年以来减少了约750平方公里。较大的冰冠已经失去了其最大冰凌面积的10-30%,而中等大小的冰川已经减少了多达80%。在21世纪的头二十年,减少的速度平均约为每平方公里40平方公里。在此期间,几十个小冰川完全消失了。时间冰川清查对于气候变化研究、冰川模型校准、冰川涌流和冰川动态研究都很重要,而且对于更好地了解冰川状态至关重要。虽然涌浪、火山爆发和jökulhlaups会影响一些冰川终点的位置,但冰岛的冰川变化是相当同步的,主要跟随19世纪末以来的气候变化。
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来源期刊
Jokull
Jokull 地学-地球科学综合
自引率
22.20%
发文量
1
审稿时长
1 months
期刊介绍: Jökull publishes research papers, notes and review articles concerning all aspects of the Earth Sciences. The journal is primarily aimed at being an international forum for geoscience research in Iceland. Specific areas of coverage include glaciology, glacial geology, physical geography, general geology, petrology, volcanology, geothermal research, geophysics, meteorology, hydrology and oceanography. Jökull also publishes research notes and reports from glacier expeditions, book reviews, and material of interest to the members of the Icelandic Glaciological and Geological Societies
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