Hydrometeorological hazards during the winter periods in the Northern Caspian and dynamics under the influence of climatic changes

A. Magaeva, N. Yaitskaya
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Abstract

Hydrometeorological hazards of the Northern Caspian during the winter periods 1950–2020—due to climatic changes were investigated. Hydrometeorological hazards for the period 1950–2020 are considered: severe winter periods, early ice freeze-up, storm waves, wind surge, as well as cumulative hydrometeorological hazards—combinations of storm waves and surge. Geographic information system (GIS) “Ice regime of the southern seas of Russia” is the information basis for the study of the ice regime of the Caspian Sea. Storm activity in the Caspian Sea were reconstructed using SWAN spectral wave model. Based on the cumulative freezing-degree days winters were divided by severity—mild, moderate and severe. During the study period, moderate types of winters prevail (59.4 %), and the number of severe and mild winters is the same and amounts to 14 pcs. (20.3 %) of each type. Due to climate change, the number of mild winters is increasing, and the number of severe ones is decreasing. Since 1985, 3 severe winters (2002/03, 2007/08, 2011/12) have been recorded. As a result, the ice cover area decreased by ∼7–10 %, and the duration of the ice season at the observation point Peshnoy was reduced by 5 days. 157 situations of combinations of storm surge and storm waves are identified: 140 are cases of potential situations of cumulative phenomena of a combination of storm and surge phenomena with a speed of 15 m/s or more of winds of effective directions. The largest number of cases of cumulative dangerous hydrometeorological hazards with a wind speed of more than 15 m/s is observed in March. After the 2000s there was an increase in the number of cases and duration of dangerous hydrometeorological hazards in November and March. A direct relationship between the number of cases of cumulative dangerous hydrometeorological hazards and the severity of winters has not been found.
北里海冬季水文气象灾害及其在气候变化影响下的动态
研究了1950 - 2020年冬季气候变化对北里海水文气象灾害的影响。考虑了1950-2020年期间的水文气象灾害:严冬期、早期结冰、风暴潮、风暴潮以及风暴潮和风暴潮组合的累积水文气象灾害。地理信息系统(GIS)“俄罗斯南部海域冰况”是研究里海冰况的信息基础。利用SWAN谱波模式对里海风暴活动进行了重建。根据累积结冰日数将冬季分为轻度、中度和重度。研究期间以中度冬季为主(59.4%),严冬和暖冬数量相同,共14个。(20.3%)。由于气候变化,暖冬的数量在增加,严冬的数量在减少。自1985年以来,记录了3次严冬(2002/03、2007/08、2011/12)。结果,冰覆盖面积减少了~ 7 - 10%,在Peshnoy观测点的冰季持续时间减少了5天。确定了157种风暴潮与风暴波结合的情况;140种风暴潮与风暴潮结合的潜在情况,风速为15米/秒或以上的有效风向风。风速大于15米/秒的水文气象灾害累计发生次数最多的是3月份。2000年后,11月和3月的水文气象灾害发生次数和持续时间有所增加。累积水文气象危险灾害的次数与冬季的严重程度之间没有直接的关系。
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来源期刊
CiteScore
0.90
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0.00%
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2
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8 weeks
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