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ESSD | Articles | Volume 11, issue 1
Earth Syst. Sci. Data, 11, 409–420, 2019
https://doi.org/10.5194/essd-11-409-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Earth Syst. Sci. Data, 11, 409–420, 2019
https://doi.org/10.5194/essd-11-409-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Review article 21 Mar 2019

Review article | 21 Mar 2019

Historical and recent aufeis in the Indigirka River basin (Russia)

Olga Makarieva et al.
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Cited articles  
Alekseev, V. R.: Naledi, Novosibirsk, Nauka, Moscow, 1987 (in Russian). 
Alekseev, V. R.: Landscape indication of aufeis phenomena, Novosibirsk, Nauka, 364 p., 2005 (in Russian). 
Alekseev, V. R.: Cryogenesis and geodynamics of icing valleys, Geodyn. Tectonophys., 6, 171–224, https://doi.org/10.5800/GT-2015-6-2-0177, 2015. 
Alekseev, V. R.: Long-term variability of the spring taryn-aufeis, Ice and Snow, 56, 73–92, https://doi.org/10.15356/2076-6734-2016-1-73-92, 2016. 
Ananicheva, M. D.: Estimation of the areas, volumes and heights of the boundary of the feeding of glacier systems of the Northeast of Russia from the space images of the beginning of the 21st century, Ice and Snow, 1, 35–48, 2014. 
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Short summary
Aufeis is formed through a complex interconnection between river water and groundwater. The dynamics of aufeis assessed by the analysis of remote sensing data can be viewed as an indicator of groundwater changes in warming climate which are otherwise difficult to be observed naturally in remote arctic areas. The spatial geodatabase developed shows that aufeis formation conditions may have changed between the mid-20th century and the present in the Indigirka River basin.
Aufeis is formed through a complex interconnection between river water and groundwater. The...
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