希比尼山脉(摩尔曼斯克地区)北极山(goltsovy)沙漠带土壤温度的年动态

I. Shtabrovskaya, I. Zenkova
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引用次数: 0

摘要

作为北极最高山(goltsovy)沙漠带综合环境研究的一部分,获得了植被破碎垫层年温度动态数据。调查区域设置在Aikuayvenchorr山高原(东经1059 ~ 1063 m)和Vudyavrchorr高原(东经1023 m)。凋落物日平均温度为负值的时期在年循环中占主导地位(超过200天,占58%)。测定凋落物的正、负温度之和、温度低于0、0 ~ +5、+5 ~ + 10和+ 10以上的日数。给出了位于Aikuayvenchorr高原和Vudyavrchorr高原两个研究区高寒带凋落物年温度动态的差异。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Annual dynamics of temperature in the soil of the Mountain Arctic (goltsovy) deserts belt in Khibiny Mountains (Murmansk Region)
As part of comprehensive environmental research of the highest Arctic mountain (goltsovy) desert belt of the Khibiny, data were obtained on the annual temperature dynamics in fragmentary cushions of vegetation. Area of investigation was disposed on the plateau of Mt. Aikuayvenchorr (1059–1063 m a. s. l.) and Vudyavrchorr plateau (1023 m a. s. l.). The period with negative values of the average daily temperature of the litter prevailed in the annual cycle (more than 200 days or 58 %). The sum of positive and negative temperatures, the number of days with temperatures below 0, from 0 ̊C to +5 ̊C, from + 5 ̊C to + 10 ̊C and above + 10 ̊C in litters was determined. The differences in the annual temperature dynamics in the litters of the alpine belt for two areas of research located on the Aikuayvenchorr and Vudyavrchorr plateaus are shown.
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