俄罗斯西北北极区土壤温度的时间变异性。第一部分:基于温度计测量和再分析数据的年际线性趋势

IF 0.7 Q4 GEOSCIENCES, MULTIDISCIPLINARY
Sergey Lebedev, Andrey Kostianoy, Il'ya Tretiyak
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引用次数: 0

摘要

本文研究了白海地区、摩尔曼斯克州、阿尔汉格尔斯克州和卡累利阿共和国四个深度的近地表空气温度(NSAT)和土壤温度变化。在分析中,我们使用了 NOAA-CIRES-DOE 20 世纪再分析(第 3 版)1980-2015 年期间的再分析数据,以及 1985-2021 年期间 5、10、15、20 厘米深度的弯杆温度计和 20、60、80、120、240 和 320 厘米深度的提取温度计数据。利用线性趋势估算出 NSAT 的平均变化率为 +0.028 ◦C/年。地表(0 厘米)土壤温度的线性趋势为 +0.0137 ◦C/年,10 厘米深度为 +0.0136 ◦C/年,40 厘米深度为 +0.0142 ◦C/年,100 厘米深度为 +0.0133 ◦C/年。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Temporal Variability of Soil Temperature in the North-West Arctic Zone of Russia. Part I: Interannual Linear Trends Based on Thermometer Measurements and Reanalysis Data
In this article we investigate near-surface air temperature (NSAT) and soil temperature variability at four depths in the region of the White Sea, Murmansk and Arkhangelsk Regions, and Republic of Karelia. For the analysis we used NOAA-CIRES-DOE 20th Century Reanalysis (Version 3) reanalysis data for the 1980–2015 time period and data of bent-stem thermometers at 5, 10, 15, 20 cm depths and extraction thermometers at 20, 60, 80, 120, 240 and 320 cm depths for 1985-2021 time period. Average variability of NSAT is estimated using linear trend as +0.028 ◦C/year. For soil temperature a linear trend is of +0.0137 ◦C/year on surface (0 cm), +0.0136 ◦C/year at 10 cm depth, +0.0142 ◦C/year at 40 cm depth and +0.0133 ◦C/year at 100 cm depth.
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来源期刊
Russian Journal of Earth Sciences
Russian Journal of Earth Sciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
1.90
自引率
15.40%
发文量
41
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