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DOI | 10.21782/KZ1560-7496-2018-4(15-24 |
The temperature regime of soils in Northern Yakutia | |
Fedoryov-Davydov D.G.; Davydov S.P.; Davydova A.I.; Ostroymov V.E.; Kholodov A.L.; Sorokovikov V.A.; Shmelev D.G. | |
发表日期 | 2018 |
ISSN | 15607496 |
卷号 | 22期号:4 |
英文摘要 | Soils in Northern Yakutia differ in average duration of the season of positive temperatures, the difference being 2.3 times between soil types and 1.8 between zonal loam soils, at a depth of 20 cm. The seasons of >0°C and >5°C soil temperatures may be shorter in wetter boggy areas with thicker organic horizons. The durations of fall freezing and persistent near-zero temperatures vary from 1-2 months for tundra cryozems and gleyzem (Turbic Glacic Cryosols) to 2.5-3.5 months for taiga cryometamorphic soils (Cambic Turbic Cryosols), peatcryozem (Folic Cryosol), and tundra podburs (Spodic Turbic Cryosols). The active layer freezes mostly from above (top to base), except some years of cool summers mainly in the tundra zone when it freezes partly from below. The tundra and taiga soils show a warming trend of the soil climate since the late 1990s according to dynamics of annual freezing degree-day sums. The soils of Northern Yakutia vary in total heat spent on the active layer warming Qt > 0, the difference reaching 10 times. © 2018 Academic Publishing House Geo. All rights reserved. |
英文关键词 | Active layer; Freezing of active layer from above and from below; Near-zero temperatures; Northern Yakutia; Soil climate change; Soil temperature regime; Zero curtain |
学科领域 | active layer; climate change; cryosphere; frozen ground; loam; permafrost; seasonal variation; soil temperature; summer; warming; Russian Federation; Sakha |
语种 | 英语 |
scopus关键词 | active layer; climate change; cryosphere; frozen ground; loam; permafrost; seasonal variation; soil temperature; summer; warming; Russian Federation; Sakha |
来源期刊 | Earth's Cryosphere
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/119111 |
作者单位 | Institute of Physicochemical and Biological Problems in Soil Science, RAS, 2, Institutskaya str., Pushchino, Moscow region, 142290, Russian Federation; North-Eastern Science Station, Pacific Geographical Institute, FEB RAS, P/O box 18, Cherskiy, Nizhnekolymskiy Region, Yakutia, 678830, Russian Federation |
推荐引用方式 GB/T 7714 | Fedoryov-Davydov D.G.,Davydov S.P.,Davydova A.I.,et al. The temperature regime of soils in Northern Yakutia[J],2018,22(4). |
APA | Fedoryov-Davydov D.G..,Davydov S.P..,Davydova A.I..,Ostroymov V.E..,Kholodov A.L..,...&Shmelev D.G..(2018).The temperature regime of soils in Northern Yakutia.Earth's Cryosphere,22(4). |
MLA | Fedoryov-Davydov D.G.,et al."The temperature regime of soils in Northern Yakutia".Earth's Cryosphere 22.4(2018). |
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