Long-term monitoring of aridization in agriculture before change and for climate change in Ukraine

E. Dehodyuk, S. Dehodyuk, Yulia Borko, O. Litvinova, Yu. O. Ihnatenko, A. Mulyarchuk
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Abstract

The results of systematic monitoring in Ukraine of drought manifestations by the method of generalization of spring, summer and autumn droughts conducted by I. Ye. Buchynsky for 1872-1969 and our meteorological generalizations by types of weather (1951-1984) and clearly expressed zonal climate changes (1985-2006) and statistical and local signs of climate aridization at the meteorological station in the northern part of the Forest-Steppe (" Shepherds ") – 2006-2020, covering a total historical period of 150 years. According to the spatial distribution of droughts, determined by a single method, from 1982 to the late 60s of the twentieth century. Mainly in the south of Ukraine, in 2 years. The number of moderate and extensive droughts since the early twentieth century. (11-30 % of the area of distribution), characteristic of the summer period, and they are repeated in the south in 4-5 years. Catastrophic droughts (more than 50%) are characteristic of large areas for every tenth year, which, since the last quarter of the nineteenth century and to the 50s of the twentieth century. Ended in famine for the population (especially the droughts of 1891, 1921, 1947). Subsequent droughts in 1963 and 1968 were characterized by abnormal weather conditions, but without a food crisis, which was associated with the beginning of chemicalization and the increase in agricultural crops. Meteorological indicators of six stations in different climatic zones for 1951-1981 and 1985-2008 indicate a zonal systematic increase in positive air temperatures with decreasing precipitation, the deficit of which is compensated by the system of agriculture with moderate saturation of organic and mineral fertilizers, which have a stabilizing effect extreme years. From the last quarter of the twentieth century. Climate change has been identified, which is related not only to the greenhouse effect, but also to the frequency that depends on the ecliptic of the globe. Particularly noticeable climate change in recent decades, accompanied by a systematic increase in air temperature and increasing aridity of the climate, and requires humanity to new technical and technological solutions.
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乌克兰变化前农业干旱化和气候变化的长期监测
叶氏(I. Ye.)采用春、夏、秋干旱概化方法对乌克兰干旱表现进行系统监测的结果。布金斯基(Buchynsky)的1872-1969年,以及我们按天气类型的气象概括(1951-1984),并清楚地表达了地域性气候变化(1985-2006)和2006-2020年森林草原北部(牧羊人)气象站气候干旱化的统计和局部迹象,涵盖了150年的总历史时期。根据1982年至20世纪60年代末的单一方法确定的干旱空间分布。主要是在乌克兰南部,在两年内。自二十世纪初以来,中度和广泛干旱的次数。(分布面积的11- 30%),以夏季为特征,在南方每4-5年重复发生一次。从19世纪最后25年到20世纪50年代,灾难性干旱(超过50%)是每10年大面积发生一次的特征。以饥荒结束(尤其是1891年、1921年和1947年的干旱)。随后的1963年和1968年的干旱以异常的天气条件为特征,但没有发生粮食危机,这与化学化的开始和农作物的增加有关。1951—1981年和1985—2008年不同气候带6个站点的气象指标表明,正气温呈地带性系统增加,降水减少,正气温的不足由有机肥和矿肥适度饱和的农业系统弥补,在极端年份具有稳定作用。从20世纪最后25年开始。气候变化已被确定,它不仅与温室效应有关,而且与取决于地球黄道的频率有关。近几十年来,气候变化尤其引人注目,伴随着气温的系统性升高和气候的日益干旱,需要人类提出新的技术和技术解决方案。
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