Iceberg danger in the seas of the Russian Federation Arctic Zone under modern climate change conditions

I. Bychkova, V. Smirnov, S. V. Mikhaltseva, E. Platonova
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Abstract

The aim of the research was to study the relationship between the intensity of iceberg formation in the Russian Arctic including the number of icebergs calving annually from outlet glaciers and surface air temperature anomalies. The research was carried out on the basis of satellite monitoring using non-commercial, freely distributed satellite information from optical-electronic satellites Landsat-8 (spatial resolution 15 m) and Sentinel-2 (spatial resolution 10 m) and the radar satellite Sentinel-1 (pixel size 20×40 m). To achieve the aim, an iceberg detection technique was used based on statistical criteria for searching for gradient zones in the analysis of two-dimensional fields of satellite images. Based on the analysis of satellite data of the visible spectral range of the Landsat-8 and Sentinel-2 satellites and Sentinel-1 radar data the maximum spatial dimensions of icebergs formed by the outlet glaciers of Severnaya Zemlya, Franz Josef Land (ZFI) and Novaya Zemlya in 2012–2022 were estimated. Satellite monitoring of the Severnaya Zemlya region was carried out using visible range images in the spring season (March–May), characterized by the best observation conditions in terms of cloudiness, natural light, and monitoring of icebergs most of which are located in fast ice at this time. Monitoring of the ZFI area was carried out using radar data in the period August-September, corresponding to the minimal ice cover conditions. Satellite monitoring of the Novaya Zemlya region was carried out using visible images in the summer season. In total, about 500 satellite images were analyzed. The discusses the dependence of the intensity of the iceberg formation process on the ice shelf and outlet glaciers with a floating edge on the surface air temperature and the maximum thickness of fast ice. It is shown that the abnormally warm weather that set in 2020 during the period of ice melting led to a sharp intensification of the process of glacier melting in the Russian Arctic and the formation of almost 8,000 icebergs near Severnaya Zemlya, more than 6,600 icebergs near ZFI and over 1,000 icebergs near the western coast of Novaya Zemlya. For all the areas of the Russian Arctic studied in the period 2012–2022 an increase was noted in the maximum observed sizes of icebergs calving from glaciers. The largest iceberg, whose length was 5 km, broke off in 2020 from the Matusevich ice shelf.
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现代气候变化条件下俄罗斯联邦北极区海域的冰山危险
这项研究的目的是研究俄罗斯北极地区冰山形成的强度(包括每年从出口冰川上 形成的冰山数量)与地表空气温度异常之间的关系。研究是在卫星监测的基础上进行的,使用了非商业性的、免费分发的卫星信息,这些信息来自光学电子卫星 Landsat-8(空间分辨率为 15 米)和 Sentinel-2(空间分辨率为 10 米)以及雷达卫星 Sentinel-1(像素大小为 20×40 米)。为了实现这一目标,在分析卫星图像的二维区域时,使用了一种基于统计标准的冰山探测技术来寻找梯度区。根据对 Landsat-8 和 Sentinel-2 卫星可见光谱范围的卫星数据以及 Sentinel-1 雷达数据的分析,估算了 2012-2022 年塞夫纳亚-泽姆利亚、弗朗兹约瑟夫地(ZFI)和新泽姆利亚出口冰川形成的冰山的最大空间尺寸。对塞韦纳亚泽姆利亚地区的卫星监测是在春季(3 月至 5 月)利用可见光范围图像进行的,春季的特点是云量、自然光和冰山监测条件最好,此时大部分冰山位于快速冰层中。在 8 月至 9 月期间,利用雷达数据对 ZFI 地区进行了监测,这一时期的冰层覆盖率最低。在夏季,利用可见光图像对新谢姆利亚地区进行了卫星监测。总共分析了约 500 幅卫星图像。研究讨论了冰架和有浮边的出口冰川上冰山形成过程的强度与地表气温和速冻冰最大厚度的关系。研究表明,2020 年冰雪融化期间出现的异常温暖天气导致俄罗斯北极地区冰川融化过程急剧加剧,在塞维利亚泽姆利亚附近形成了近 8000 座冰山,在泽姆利亚冰架附近形成了 6600 多座冰山,在新泽姆利亚西海岸附近形成了 1000 多座冰山。在 2012-2022 年期间研究的俄罗斯北极所有地区,观测到的冰川崩落冰山的最大尺寸都有所增加。最大的冰山长度为 5 千米,于 2020 年从马图塞维奇冰架上断裂。
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