The ice regime of the northeastern Russia

A. Zemlianskova, N. Nesterova, O. Makarieva
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Abstract

Transport links and provision of hard-to-reach settlements and mining enterprises play an important role in the economic development of the Arctic regions. In winter, winter roads are used as transport arteries; their mode of operation depends on the characteristics of the ice. Winter roads are used in Russia, Canada, USA, Finland, and China. Due to climate warming, the timing of the formation of ice cover on rivers is shifting to later times, and in the spring the ice is destroyed earlier. This could affect the delivery of vital supplies to remote regions. According to recent forecasts, it is assumed that heavy vehicles will not be able to use winter roads by the end of the 21st century. The purpose of the study is to analyze changes in the characteristics of ice cover on the rivers of the Northeast of Russia. To do this, a series of data was collected for the period 1940–2018 on the thickness of the ice cover at 80 hydrological stations located in the basins of the Yana, Indigirka, Kolyma rivers, rivers of the Chukotka Peninsula and the Sea of Okhotsk basin. The catchment areas range from 18.3 to 635,000 km2, and the duration of the continuous series ranges from 2 to 67 years. Three statistical nonparametric tests (Mann-Kendall, Pettitt and Theil-Sen) were used for evaluation. The following characteristics were considered: the maximum ice thickness and the date of its formation, the dates when the ice thickness reached 60 and 90 cm. During the period under review, the maximum ice thickness decreased by an average of 40 cm, while the date of reaching the maximum values remained almost unchanged. The period for the formation of river ice with a thickness of 60 and 90 cm, necessary for the passage of cars and trucks, respectively, has shifted by almost a month. The start date of freeze-up occurs on average 3–4 days later, and the end date of freeze-up occurs 5–8 days earlier. On average, the duration of freeze-up decreased by 5–15 days. The results obtained must be taken into account when drawing up the work schedule for winter roads. This is especially important for regions where communication between populated areas and mining enterprises is possible only through river arteries.
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俄罗斯东北部的冰情
在北极地区的经济发展中,运输连接和为难以到达的定居点和采矿企业提供运输服务发挥着重要作用。冬季,冬季公路被用作运输干线;其运行方式取决于冰的特性。俄罗斯、加拿大、美国、芬兰和中国都在使用冬季公路。由于气候变暖,河流冰盖形成的时间变晚,春季冰层被破坏的时间提前。这可能会影响向偏远地区运送重要物资。根据最近的预测,预计到 21 世纪末,重型车辆将无法使用冬季道路。这项研究的目的是分析俄罗斯东北部河流冰盖特征的变化。为此,研究人员在亚纳河、因迪吉尔卡河、科雷马河流域、楚科奇半岛河流和鄂霍次克海流域的 80 个水文站收集了 1940-2018 年期间冰盖厚度的一系列数据。流域面积从 18.3 平方公里到 63.5 万平方公里不等,连续序列的持续时间从 2 年到 67 年不等。评估采用了三种非参数统计检验方法(Mann-Kendall、Pettitt 和 Theil-Sen)。考虑了以下特征:最大冰层厚度及其形成日期,冰层厚度达到 60 厘米和 90 厘米的日期。在本报告所述期间,最大冰层厚度平均减少了 40 厘米,而达到最大值的日期几乎没有变化。汽车和卡车通行所需的河冰厚度分别为 60 厘米和 90 厘米的形成期缩短了近一个月。结冰开始日期平均推迟 3-4 天,结冰结束日期平均提前 5-8 天。冻结期平均缩短了 5-15 天。在制定冬季道路施工计划时,必须考虑到所取得的结果。这一点对于只有通过河流干道才能在居民区和采矿企业之间进行交流的地区尤为重要。
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