Journal of Siberian Federal University. Engineering & Technologies / Water Mass Dynamics in Cryolithozone of Central Siberia Based on Grace Remote Sensing Data

Full text (.pdf)
Issue
Journal of Siberian Federal University. Engineering & Technologies. 2015 8 (6)
Authors
Im, Sergey T.; Kharuk, Viacheslav I.
Contact information
Im, Sergey T.:V.N. Sukachev Institute of Forest SB RAS 50/28 Academgorodok, Krasnoyarsk, 660036, Russia; Siberian Federal University 79 Svobodniy, Krasnoyarsk, 660041, Russia; iberian State Aerospace University M.F. Reshetnev pr. Them. newspaper «Krasnoyarsk worker», Krasnoyarsk, 660014, Russia; E-mail: ; Kharuk, Viacheslav I.:V.N. Sukachev Institute of Forest SB RAS 50/28 Academgorodok, Krasnoyarsk, 660036, Russia; Siberian Federal University 79 Svobodniy, Krasnoyarsk, 660041, Russia
Keywords
GRACE; permafrost; Central Siberia; gravity data; GRACE
Abstract

An investigation of application of gravimetric data from GRACE twin satellite mission for estimation of equivalent water thickness anomalies dynamics caused by climate change were carried out. Significant trends of water mass for the period 2003-2012 were revealed. During 2003– 2008, positive trends of water mass dynamics with subsequent stabilization linked to dynamic of precipitation, temperature and potential evapotranspiration were observed. Dependence of rate of water accumulation from soil properties was determined. Significant content of gravel in soil accelerates water accumulation (r = 0.72, α < 0.02) and increased content of clay decreases rate of water accumulation (r = –0.69…–0.77, α < 0.02). Determined tendencies in water mass dynamics, probably, indicates increasing of permafrost thaw depth in Taimyr Peninsula, in Central Siberian Plateau and in the western part of the Lena River’s basin

Pages
734-743
Paper at repository of SibFU
https://elib.sfu-kras.ru/handle/2311/19839

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