{"title":"小冰河时期的进展Kvískerjajöklar, Öræfajökull,冰岛。对自18世纪末以来冰岛冰川变化的评估作出贡献","authors":"Snaevarr Gudmundsson, H. Bjornsson","doi":"10.33799/JOKULL2020.70.073","DOIUrl":null,"url":null,"abstract":"We describe the changes of the Kvískerjajöklar outlet glaciers in SE Iceland (presently ranging 600–1600 m a.s.l.), from their Little Ice Age maximum (LIAmax) to the present. We assume that glacier extent of the late 19th century approximately describes LIAmax although the glaciers already reached their peak extent in the 18th century. The former glacier margins were delineated from moraines, historical descriptions, topographical maps, aerial and oblique photographs, Landsat images and a lidar DEM. Along the previous glacier margins, elevation differences with respect to the lidar DEM of 2011 were estimated and contour maps of the glacier drawn at selected dates, maintaining the shape of the glacier surface as available maps. During the period 1890 to 2011, the outlets lost -0.4 m a-1 water equivalent evenly distributed over their surface and their area was reduced by 37% (from 10 km2 to 6.4 km2, 0.03 km2 a-1, 0.43 km3 water equivalent in total, i.e. 0.003 km3 w.e. a-1).","PeriodicalId":56284,"journal":{"name":"Jokull","volume":"70 1","pages":"73-85"},"PeriodicalIF":0.5000,"publicationDate":"2021-04-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Little Ice Age advance of Kvískerjajöklar, Öræfajökull, Iceland.\\nA contribution to the assessment of glacier variations in Iceland\\nsince the late 18th century\",\"authors\":\"Snaevarr Gudmundsson, H. Bjornsson\",\"doi\":\"10.33799/JOKULL2020.70.073\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"We describe the changes of the Kvískerjajöklar outlet glaciers in SE Iceland (presently ranging 600–1600 m a.s.l.), from their Little Ice Age maximum (LIAmax) to the present. We assume that glacier extent of the late 19th century approximately describes LIAmax although the glaciers already reached their peak extent in the 18th century. The former glacier margins were delineated from moraines, historical descriptions, topographical maps, aerial and oblique photographs, Landsat images and a lidar DEM. Along the previous glacier margins, elevation differences with respect to the lidar DEM of 2011 were estimated and contour maps of the glacier drawn at selected dates, maintaining the shape of the glacier surface as available maps. During the period 1890 to 2011, the outlets lost -0.4 m a-1 water equivalent evenly distributed over their surface and their area was reduced by 37% (from 10 km2 to 6.4 km2, 0.03 km2 a-1, 0.43 km3 water equivalent in total, i.e. 0.003 km3 w.e. a-1).\",\"PeriodicalId\":56284,\"journal\":{\"name\":\"Jokull\",\"volume\":\"70 1\",\"pages\":\"73-85\"},\"PeriodicalIF\":0.5000,\"publicationDate\":\"2021-04-15\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Jokull\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.33799/JOKULL2020.70.073\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Jokull","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.33799/JOKULL2020.70.073","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
摘要
本文描述了冰岛东南部Kvískerjajöklar出口冰川(目前范围为600-1600米a.s.l.)从小冰期最大值(LIAmax)到现在的变化。虽然冰川在18世纪已经达到顶峰,但我们假设19世纪末的冰川范围大致描述了LIAmax。以前的冰川边缘是根据冰碛、历史描述、地形图、航空和倾斜照片、陆地卫星图像和激光雷达DEM绘制的。沿着以前的冰川边缘,估计了2011年激光雷达DEM的高程差,并在选定的日期绘制了冰川等高线图,保持了冰川表面的形状作为可用的地图。在1890 - 2011年期间,分布在其表面上的出口平均损失了-0.4 m a-1水当量,其面积减少了37%(从10 km2减少到6.4 km2, 0.03 km2 a-1,总计0.43 km3水当量,即0.003 km3 w.e.a -1)。
Little Ice Age advance of Kvískerjajöklar, Öræfajökull, Iceland.
A contribution to the assessment of glacier variations in Iceland
since the late 18th century
We describe the changes of the Kvískerjajöklar outlet glaciers in SE Iceland (presently ranging 600–1600 m a.s.l.), from their Little Ice Age maximum (LIAmax) to the present. We assume that glacier extent of the late 19th century approximately describes LIAmax although the glaciers already reached their peak extent in the 18th century. The former glacier margins were delineated from moraines, historical descriptions, topographical maps, aerial and oblique photographs, Landsat images and a lidar DEM. Along the previous glacier margins, elevation differences with respect to the lidar DEM of 2011 were estimated and contour maps of the glacier drawn at selected dates, maintaining the shape of the glacier surface as available maps. During the period 1890 to 2011, the outlets lost -0.4 m a-1 water equivalent evenly distributed over their surface and their area was reduced by 37% (from 10 km2 to 6.4 km2, 0.03 km2 a-1, 0.43 km3 water equivalent in total, i.e. 0.003 km3 w.e. a-1).
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