阿尔泰高原洼地草原和冻土带形成的气候条件

Pub Date : 2019-11-29 DOI:10.21638/spbu07.2019.407
K. Chistyakov, M. Amosov, I. Volkov, Y. N. Kurochkin, S. Lessovaia, Maria V. Manakova, Natalia A. Nehuzhenko, I. Strelkov, G. A. Tyusov, G. N. Shastina
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引用次数: 1

摘要

本文对阿尔泰高原洼地的气候和植被资料进行了制图。确定Bertek坳陷(海拔2200 ~ 2400 m)和Khindiktig-Khol’湖坳陷(海拔2300 ~ 2400 m)为研究对象。调查是基于2018年野外调查期间获得的植被和小气候差异信息。利用Bertek和Mugur-Aksy气象站的长期观测资料分析了气候特征。草原植被是洼地的典型特征。在khindktig - khol地区,冻土带物种也与草原物种一起存在,尽管在某些情况下,冻土带和草原的内陆地区是建立的。冻土带群落在贝尔泰克洼地内无足轻重。洼地植被覆盖度在植被期较短的条件下发展,并受到夏季低温的负面影响(Bertek 7月平均气温- +9,3°С;在khindktig - khol ' - + 10.8°С)。这些数据明显低于平坦草原带的平均温度。考虑到温度数据,所调查的地区与冻土带有关。气候湿润程度不足以发展冻土带的连续覆盖(Vysotskii-Ivanov’s降水-蒸发比khindktig - khol’= 0.74,而Bertek—0.61)。综上所述,khindktig - khol洼地湿度较大,苔原群落与草原植被共生。不同冻土带和草原植被相邻区域的小气候观测表明,与圆叶桦(Betula rotundifolia)组成冻土带的物种具有独特的特征,为该群落的存在创造了有利条件。与大草原地区相比,白天的空气不仅在冻土带上更热,在冻土带下也更热。此外,矮桦树(桦圆叶)保持积雪覆盖,这导致更好的土壤加湿。因此,在Khindiktig-Khol洼地的植被覆盖更加多样化,并且可以弄清楚独家苔原和草原混合物的外观。
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Climatic Conditions of Steppe and Tundra Formations in the Altai Highland Depressions
The data on climate and vegetation of the Altai highland depressions are mapped in this paper. The Bertek depression (located 2200 – 2400 m above sea level) and the lake depression of Khindiktig-Khol’ (2300 – 2400 m a.s.l.) are decided to be the study objects. The investigation is based on the information about vegetation and microclimatic differences received during the field research in 2018. Long-term observations of Bertek and Mugur-Aksy meteorological stations are applied to climate characteristics. The steppe vegetation is typical for the depressions. The tundra species also exist alongside the steppe ones within the Khindiktig-Khol’ region, though in some cases the intarsia of tundra and steppe is founded. Tundra communities are insignificant within the Bertek depression. Vegetation cover of the depressions develops under the conditions of short-term vegetation period and undergoes the negative impact of low summer temperatures (mean July temperatures in Bertek – +9,3°С; in Khindiktig-Khol’ – +10,8°С). The data are significantly lower than the mean temperatures of the flat steppe zone. Taking into account the temperature data, the investigated areas are associated with the tundra zone. The climate humidification level is not enough to develop the continuous cover of tundra cenosis (Vysotskii-Ivanov’s precipitation-evaporation ratio of Khindiktig-Khol’ equals 0,74, whereas in Bertek – 0,61). According to the fact above, Khindiktig-Khol’ depression is more humid, and the tundra communities live together with the steppe vegetation. Microclimatic observations of the neighboring areas with the different tundra and steppe cenoses show that the species, which are composing tundra with the dwarf birch (Betula rotundifolia), have unique features, thus creating favorable conditions for the existence of this community. Comparing to the steppe area, the air during the daylight heats better not only above the tundra pattern, but also beneath it. Moreover, the dwarf birch (Betula rotundifolia) keeps the snow cover, which results in a better soil humidification. Consequently, the vegetation cover is more diverse in Khindiktig-Khol’ depression and allows to figure out the appearance of exclusive tundra and steppe mixture.
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