Duration of the growth phase in cases of ice deposits of category SHP (spontaneous) in the territory of Ukraine in the months of the cold period of the year during 1991–2016

S. Pyasetska
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Abstract

The data on the duration of the growth phase of cases of ice storms of the category of SHР in the territory of Ukraine for certain periods of time during 1991–2016 in the month of the cold period of the year and the separate months of the transitional seasons are considered. It has been established that the duration of the growth phase varies from a few hours to several dozen and sometimes hundreds of hours in a row. It was found that, for the most part, slight duration of the growth phase of icing of the category of SHP is predominant. They are usually calculated several dozens of hours, but there are longer ones. The most prolonged were the growth phases in the cases of ice deposits in the category of SHP in the winter months. You can make a number of conclusions from the conducted research, such as: – The duration of the growth phase of ice-oily deposits in the category of SHP is within a fairly wide time range from several hours to tens or hundreds of hours, depending on the current conditions. – It has been established that for the most part, the duration of the growth phase of ice deposits is insignificant and lasts from several hours to several dozens of hours, regardless of the place where the sediment was formed. - Most often, longer phases of growth are observed in the months of the winter season, especially in January and December, as well as in November. This refers to the 1991–2000 and 2001–2010 periods. - The most prolonged phases of the accumulation of ice deposits of the CSF category, which exceeded 48 hours in a row, were observed during 1991-2000 in February 1995 at MS Play, November 1991 and 2000 in Lyubashivka, 1999 in Mariupol, November 2000, in Razdelna and Nova Ushytsia, December 1992 in Lyubashitsa, December 1997 in Pomechna, Kryvyi Rih and Loshkarovka. During 2001–2010, the longest phases of the increase in ice deposits of the CSF category were observed in January and December 2007 at MS Play, December 2007 in Debaltseve, 2008 in Ovruch, Vinnytsia. During 2011-2016, cases of ice deposition with such prolonged phases of an increase in ice of the SНР category were observed in Poltava in January 2013. – For cases where the duration of the growth phase of ice deposits was negligible, it would have a long duration of the preservation and destruction phase. Because due to the considerable duration of this phase, the danger of emergency situations in the ice-and-frost deposits depending on the sectors of the economy will increase.
1991-2016年寒冷时期乌克兰境内SHP(自发)类冰沉积生长阶段的持续时间
考虑了1991-2016年期间乌克兰境内特定时期内一年中寒冷月份和过渡季节的单独月份中SHР类冰暴病例增长阶段持续时间的数据。已经确定,生长阶段的持续时间从几个小时到几十小时,有时连续数百小时不等。结果表明,在绝大多数情况下,SHP类型的结冰生长阶段的轻微持续时间占主导地位。它们通常计算几十个小时,但也有更长的。在冬季月份,SHP类冰沉积的生长阶段最长。从所进行的研究中可以得出一些结论,例如:—SHP类冰油沉积物生长阶段的持续时间在一个相当宽的时间范围内,从几小时到几十小时或几百小时,取决于当前的条件。-已经确定,在大多数情况下,冰沉积物生长阶段的持续时间微不足道,持续时间从几小时到几十小时不等,而与沉积物形成的地点无关。-最常见的是,在冬季的几个月里,特别是在1月和12月,以及11月,观察到较长的生长阶段。这指的是1991-2000年和2001-2010年期间。1995年2月在MS Play、1991年11月和2000年在柳巴什夫卡、1999年在马里乌波尔、2000年11月在拉兹尔纳和新乌希察、1992年12月在柳巴希察、1997年12月在波梅契纳、克里维伊里赫和洛什卡观察到CSF类冰沉积物积累的最长阶段,连续超过48小时。在2001-2010年期间,观察到CSF类冰沉积增加的最长阶段是2007年1月和12月在MS Play, 2007年12月在Debaltseve, 2008年在Vinnytsia的Ovruch。2011-2016年期间,2013年1月在Poltava观测到SНР类冰增加周期延长的冰沉积案例。-在冰沉积物生长阶段的持续时间可以忽略不计的情况下,保存和破坏阶段的持续时间会很长。因为由于这一阶段持续时间相当长,根据经济部门的不同,霜冻沉积物出现紧急情况的危险将会增加。
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