Petrova Olga, Denissova Natalya, Daumova Gulzhan, Ivashchenko Yelena, Sergazinov Evgeny
School of Earth Sciences, D. Serikbayev East Kazakhstan Technical University, Ust-Kamenogorsk, 070001, Kazakhstan.
Department of Information Technology, D. Serikbayev East Kazakhstan Technical University, Ust-Kamenogorsk, 070001, Kazakhstan.
Heliyon. 2025 Jan 9;11(2):e41807. doi: 10.1016/j.heliyon.2025.e41807. eCollection 2025 Jan 30.
The article examines the territory of East Kazakhstan, where a sharply continental climate prevails with hot summers, cold and snowy winters. The mountainous regions of East Kazakhstan are represented by the Kalba, Altai and Saur-Tarbagatay ranges, they are surrounded by rolling plains. The highest points are at 3000-4500 m. On average, the heights are in the range of 900-1400 m. Despite the low heights in the mountainous area, the problem of avalanche safety is acute in the region. At the same time, the situation is complicated by not always predictable weather events, the frequency of which is increasing every year. These include heavy precipitation, sometimes combined with a sharp warming in winter, and the changing wind regime of the territory. To identify regional climate changes and its connection with the avalanche-prone situation in the region, the study analyzed meteorological data from weather stations located directly near avalanche prone locations over the past 23 years since 2001, as well as data from observations of avalanche-prone areas since 2005 and information on registered spontaneous avalanches from 2013 to the present. This study is the first in the East Kazakhstan region, which presents the results of a comprehensive analysis of data on 497 avalanche-prone sites, of which 325 sites pose a threat to life and infrastructure. 10 most dangerous sites have been selected for detailed study. The analysis of climate data was carried out based on information from 7 weather stations. The article discusses the main climatic changes in the region, including an increase in air temperature, an increase in precipitation and a change in wind conditions. Data from weather stations and snow measuring routes covering the period since 2005 have been used to develop probabilistic avalanche forecasts. The use of statistical methods and the analysis of the relationships between meteorological parameters (temperature, precipitation, wind speed) made it possible to build models predicting avalanche-prone situations. Data on spontaneous avalanches were analyzed for five sites (Bogatyrevskaya site, Prokhodnaya, Sogornoye-Barlyk, Tainty and Pikhtovka). Based on these data, equations of dependence of temperature, wind and precipitation have been developed, which improves the accuracy of forecasting avalanche risks. An analysis of the data in the Statistica program showed a significant relationship between sudden warming, increased wind speed and precipitation, which precedes avalanches. Regression equations and the approximation confidence coefficient for the average values of the studied parameters are obtained. The results of the study make it possible not only to establish patterns, but also to propose effective methods for monitoring and forecasting avalanche hazard in the region. According to the data analysis, regional features of climate change in East Kazakhstan were identified, and a comparison was made with previously known works on Kazakhstan. The interrelation of climatic characteristics with avalanche hazard in the region is shown. The results obtained in the study will help us to better understand the regional manifestations of climate change. An important task for further forecasting of avalanche activity is the correct design of the avalanche collection database. The authors identified information objects (entities). An ontological database model (Entity Relationship Diagram) is constructed. Based on it, a database has been created for a system for monitoring and forecasting avalanche activity in the East Kazakhstan region.
本文研究了东哈萨克斯坦地区,这里盛行大陆性气候,夏季炎热,冬季寒冷多雪。东哈萨克斯坦的山区以卡尔巴、阿尔泰山脉和萨乌尔 - 塔尔巴哈台山系为代表,周边环绕着起伏的平原。最高点海拔3000 - 4500米,平均海拔在900 - 1400米之间。尽管山区海拔相对较低,但该地区雪崩安全问题依然严峻。与此同时,情况因天气事件难以预测而变得复杂,且此类天气事件的发生频率逐年增加。这些天气事件包括强降水,有时还伴有冬季的急剧升温,以及该地区风向的变化。为了确定区域气候变化及其与该地区雪崩易发情况的关联,本研究分析了自2001年以来过去23年中位于雪崩易发地点附近的气象站的气象数据,以及自2005年以来对雪崩易发地区的观测数据和2013年至今已记录的自发雪崩信息。这项研究是东哈萨克斯坦地区的首次研究,呈现了对497个雪崩易发地点数据的综合分析结果,其中325个地点对生命和基础设施构成威胁。已选取10个最危险的地点进行详细研究。气候数据分析基于7个气象站的信息。本文讨论了该地区的主要气候变化,包括气温升高、降水量增加和风向条件变化。利用2005年以来气象站和积雪测量路线的数据来制定概率性雪崩预报。通过运用统计方法以及分析气象参数(温度、降水量、风速)之间的关系,得以建立预测雪崩易发情况的模型。对5个地点(博加特列夫斯卡亚地点、普罗霍德纳亚、索戈尔诺耶 - 巴尔利克、泰恩蒂和皮赫托夫卡)的自发雪崩数据进行了分析。基于这些数据,得出了温度、风和降水量的依赖方程,提高了雪崩风险预报的准确性。在Statistica程序中对数据的分析表明,在雪崩发生之前,突然升温、风速增加和降水量增加之间存在显著关系。获得了所研究参数平均值的回归方程和近似置信系数。该研究结果不仅有助于建立模式,还能为该地区雪崩灾害的监测和预报提出有效方法。根据数据分析,确定了东哈萨克斯坦地区气候变化的区域特征,并与之前关于哈萨克斯坦的已知研究进行了比较。展示了气候特征与该地区雪崩灾害的相互关系。该研究所得结果将有助于我们更好地理解气候变化的区域表现。进一步进行雪崩活动预报的一项重要任务是正确设计雪崩收集数据库。作者确定了信息对象(实体)。构建了一个本体数据库模型(实体关系图)。在此基础上,创建了一个用于东哈萨克斯坦地区雪崩活动监测和预报系统的数据库。