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The Transformation of Agro-Climatic Resources of the Altai Region under Changing Climate Conditions

机译:气候变化条件下阿尔泰地区农业气候资源的转化

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This research examines the transformation of the agro-climatic conditions of the Altai region as a result of climate change. The climate of the Altai region in Russia is sharply continental and characterized by dry air and significant weather variability, both in individual seasons and years. The current study is determined by the lack of detailed area-related analytical generalizations for the territory of the Altai region over the past 30 years. Most of the published data dealing with an integrated analysis of the agro-climatic conditions in the Altai region date back to the late 1960s and early 1970s; in most cases, this data is from climate reference-books based on the generalized data from the first half of the 20th century. To make accurate forecasts and to efficiently manage agricultural production in the Altai region, area-related data on the state and dynamics of agro-climatic changes have been analysed. The results reveal that in the period between 1964 and 2017, significant climatic changes occurred in the territory of the Altai region. These climatic changes affected the growing season length, which increased due to a shift in the dates of the air temperature transition above 10 °C, to earlier dates in spring and to later dates in autumn. Furthermore, the current study also revealed that the foothills of the Altai Mountains are the most moistened parts of the region and the Kulunda lowland is the most arid part. In the Altai region, the accumulated temperatures and amounts of precipitation during the growing season increased significantly, and the values of integrated coefficients and indices that reflect the moisture supply conditions for the territory also changed significantly. Based upon the results, a schematic map of the current precipitation distribution on the Altai region’s territory has been generated. These results and this map may be used to conduct more detailed studies in the field of agro-climatology and to update the current borders of agro-climatic areas and revision of the agro-climatic zonation scheme.
机译:这项研究探讨了由于气候变化而导致的阿尔泰地区农业气候条件的转变。俄罗斯阿尔泰地区的气候属于大陆性气候,并且在各个季节和年份都有干燥的空气和明显的气候多变性。当前的研究是由于过去30年来对阿尔泰地区的领土缺乏详细的与地区相关的分析概括而确定的。有关阿尔泰地区农业气候条件的综合分析的大多数公开数据可追溯到1960年代末和1970年代初。在大多数情况下,这些数据来自气候参考书,这些参考书是基于20世纪上半叶的广义数据而制成的。为了做出准确的预测并有效管理阿尔泰地区的农业生产,已经分析了有关农业气候变化的状态和动态的区域相关数据。结果表明,在1964年至2017年期间,阿尔泰地区领土发生了重大的气候变化。这些气候变化影响了生长季节的长度,这是由于气温转变温度高于10°C的日期移至春季的较早日期和秋季的较晚日期而增加的。此外,目前的研究还表明,阿尔泰山脉的山麓地区是该地区最潮湿的地区,而库伦达低地是最干旱的地区。在阿尔泰地区,生长季节的累积温度和降水量显着增加,反映该地区水分供应状况的综合系数和指数值也发生了显着变化。根据这些结果,已绘制出了阿尔泰地区当前降水分布的示意图。这些结果和该图可用于在农业气候学领域进行更详细的研究,并更新当前农业气候区的边界,并修订农业气候区划方案。

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