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首页> 外文期刊>Annals of Glaciology >Glacier geometry and elevation changes on Svalbard (1936–90): a baseline dataset
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Glacier geometry and elevation changes on Svalbard (1936–90): a baseline dataset

机译:斯瓦尔巴群岛上的冰川几何形状和海拔变化(1936–90年):基准数据集

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This study uses older topographic maps made from high-oblique aerial photographs for glacier elevation change studies. We compare the 1936/38 topographic map series of Svalbard (Norwegian Polar Institute) to a modern digital elevation model from 1990. Both systematic and random components of elevation error are examined by analyzing non-glacier elevation difference points. The 1936/38 photographic aerial survey is examined to identify areas with poor data coverage over glaciers. Elevation changes are analyzed for seven regions in Svalbard ( 5000 km2), where significant thinning was found at glacier fronts, and elevation increases in the upper parts of the accumulation areas. All regions experience volume losses and negative geodetic balances, although regional variability exists relating to both climate and topography. Many surges are apparent within the elevation change maps. Estimated volume change for the regions is –1.59±0.07km3 a–1 (ice equivalent) for a geodetic annualbalance of –0.30ma–1w.e., and the glaciated area has decreased by 16% in the 54 year time interval.The 1936–90 data are compared to modern elevation change estimates in the southern regions, to showthat the rate of thinning has increased dramatically since 1990.
机译:这项研究使用由高斜度航拍照片制成的较旧的地形图进行冰川海拔变化研究。我们将1990年的Svalbard(挪威极地研究所)的1936/38地形图系列与1990年以来的现代数字高程模型进行了比较。通过分析非冰川的高程差点,对高程误差的系统分量和随机分量进行了检验。检查了1936/38年的摄影航空勘测,以识别冰川上数据覆盖范围较差的区域。分析了斯瓦尔巴群岛(5000平方公里)中七个区域的海拔变化,这些区域在冰川前缘明显变薄,并且堆积区上部的海拔升高。尽管存在与气候和地形有关的区域变异性,但所有区域都经历了体积损失和负大地平衡。在高程变化图中可以看到许多波动。对于大地年平衡为–0.30ma–1w.e,该地区的估计体积变化为–1.59±0.07km3 a-1(冰当量),并且在54年的时间间隔内,冰川面积减少了16%。将1936–90年的数据与南部地区的现代海拔变化估计值进行了比较,以显示自1990年以来稀疏率急剧增加。

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