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Interannual sea ice thickness variability in the Bay of Bothnia

机译:博特尼亚湾的年际海冰厚度变化

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While variations of Baltic Sea ice extent and thickness have been extensively studied, there is little information about drift ice thickness, distribution, and its variability. In our study, we quantify the interannual variability of sea ice thickness in the Bay of Bothnia during the years 2003–2016. We use various different data sets: official ice charts, drilling data from the regular monitoring stations in the coastal fast ice zone, and helicopter and shipborne electromagnetic soundings. We analyze the different data sets and compare them to each other to characterize the interannual variability, to discuss the ratio of level and deformed ice, and to derive ice thickness distributions in the drift ice zone. In the fast ice zone the average ice thickness is 0.58±0.13 m. Deformed ice increases the variability of ice conditions in the drift ice zone, where the average ice thickness is 0.92±0.33 m. On average, the fraction of deformed ice is 50?% to 70?% of the total volume. In heavily ridged ice regions near the coast, mean ice thickness is approximately half a meter thicker than that of pure thermodynamically grown fast ice. Drift ice exhibits larger interannual variability than fast ice.
机译:尽管对波罗的海冰的范围和厚度的变化进行了广泛的研究,但有关流冰厚度,分布及其变化性的信息很少。在我们的研究中,我们量化了2003年至2016年期间博特尼亚湾海冰厚度的年际变化。我们使用各种不同的数据集:官方冰图,沿海快速冰区常规监测站的钻探数据以及直升机和舰载电磁测深仪。我们分析了不同的数据集并进行了比较,以表征年际变化,讨论了冰的水平与变形比,并得出了流冰区的冰厚分布。在快速冰区,平均冰层厚度为0.58±0.13 m。变形的冰增加了流冰区冰条件的可变性,该区域的平均冰层厚度为0.92±0.33 m。平均而言,变形冰的比例为总体积的50%至70%。在靠近海岸的重脊冰区,平均冰层厚度比纯热力学快速生长的冰层厚约半米。与快冰相比,流冰的年际变化更大。

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