Climate Change and Its Influence on the Active Layer Depth in Central Yakutia

Alexey Desyatkin, Pavel Fedorov, Nikolay Filippov and Roman Desyatkin
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Alexey Desyatkin: Institute for Biological Problems of Cryolithozone, Siberian Branch, Russian Academy of Science, Yakutsk 677980, Russia
Pavel Fedorov: Institute for Biological Problems of Cryolithozone, Siberian Branch, Russian Academy of Science, Yakutsk 677980, Russia
Nikolay Filippov: Institute for Biological Problems of Cryolithozone, Siberian Branch, Russian Academy of Science, Yakutsk 677980, Russia
Roman Desyatkin: Institute for Biological Problems of Cryolithozone, Siberian Branch, Russian Academy of Science, Yakutsk 677980, Russia

Land, 2020, vol. 10, issue 1, 1-13

Abstract: Analysis of climatic conditions for the period of instrumental measurement in Central Yakutia showed three periods with two different mean annual air temperature (MAAT) shifts. These periods were divided into 1930–1987 (base period A), 1988–2006 (period B) and 2007–2018 (period C) timelines. The MAAT during these three periods amounted −10.3, −8.6 and −7.4 °C, respectively. Measurement of active layer depth (ALD) of permafrost pale soil under the forest (natural) and arable land (anthropogenic) were carried out during 1990–2018 period. MAAT change for this period affected an early transition of negative temperatures to positive and a later establishment of negative temperatures. Additionally, a shortening of the winter season and an extension of the duration of days with positive temperatures was found. Since the permafrost has a significant impact on soil moisture and thermal regimes, the deepening of ALD plays a negative role for studied soils. An increase in the ALD can cause thawing of underground ice and lead to degradation of the ice-rich permafrost. This thaw process causes a change of the ecological balance and leads to the destruction of natural landscapes, sometimes with a complete or prolonged loss of their biological productivity. During this observation (1990–2018 period) the active layer of permafrost is characterized by high dynamics, depending on climatic parameters such as air temperature, as well as thickness and duration of snow cover. A significant increase in ALD of forest permafrost soils—by 80 cm and 65 cm—on arable land was measured during the observation period (28 years).

Keywords: permafrost; forest soils; climate change; meteorological conditions; soil thermal regime; active layer depth (search for similar items in EconPapers)
JEL-codes: Q15 Q2 Q24 Q28 Q5 R14 R52 (search for similar items in EconPapers)
Date: 2020
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