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Glacier geometry and elevation changes on Svalbard (1936-90): a baseline dataset

机译:Svalbard的冰川几何和高程变化(1936-90):基线数据集

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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±0.07 km3 a?1 (ice equivalent) for a geodetic annual balance of ?0.30 ma?1 w.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 show that the rate of thinning has increased dramatically since 1990.
机译:本研究采用了由高斜空拍摄的较旧地形图进行冰川高程变化研究。我们将1936/38地形地图系列斯瓦尔巴(Norwegian Polar Institute)与1990年开始的现代数字高度模型。通过分析非冰川高程差点来检查高程误差的系统和随机分量。审查了1936/38摄影空中调查,以确定冰川数据覆盖不良的地区。在Svalbard(〜5000 km2)中分析了七个区域的升高变化,其中在冰川前面发现了显着的细化,并且累积区域的上部增加了升高。虽然与气候和地形有关的区域可变性,但所有地区都经历了体积损失和负面的大地测量余额。在高程变化地图中,许多潮水很明显。该地区的估计体积变化是?1.59±0.07 km3 a?1(冰相当),用于大地平衡的?0.30 ma?1 w.e,并且冰川区域在54年的时间间隔下降了16%。 1936-90数据与南部地区的现代高程变化估计进行了比较,以表明自1990年以来自1990年以来变薄的速度急剧增加。

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