Identification of Frozen/Thawed Soils in the Areas of Anadyr (Chukotka) and Belaya Gora (Sakha) from the Sentinel 1 Radar Data
- Authors: Rodionova N.V.1
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Affiliations:
- Kotelnikov Institute of Radio Engineering and Electronics, Russian Academy of Sciences
- Issue: Vol 55, No 9 (2019)
- Pages: 1314-1321
- Section: Use of Space Information about the Earth Studying Circumpolar Regions Using Remote Sensing
- URL: https://journals.rcsi.science/0001-4338/article/view/148820
- DOI: https://doi.org/10.1134/S0001433819090433
- ID: 148820
Cite item
Abstract
This paper is focused on the problem of distinguishing between thawed and frozen soils in the 5-cm upper layer at meteorological stations of Belaya Gora (Sakha) (68.5° N) and Anadyr (Chukotka) (64.78° N) with the use of the Sentinel 1 C‑band radar data for the period of 2014–2016. The state of a frozen soil is determined in three ways: (i) by a significant difference (3–5 dB) in the backscattering coefficient σ0 (BSC) during the transition of a soil between frozen and thawed states observed in multitemporal radar data, (ii) by a threshold value of \(\sigma _{{{\text{threshold}}}}^{0}\) at which the temperature in the upper soil layer falls below 0°С, and (iii) by textural features for one-channel images. Diagrams of the air-freezing index (AFI) and its trend for the 2012–2018 period have been constructed from the archive data containing the air temperature for the study areas.
About the authors
N. V. Rodionova
Kotelnikov Institute of Radio Engineering and Electronics, Russian Academy of Sciences
Author for correspondence.
Email: rnv@ire.rssi.ru
Russian Federation, Fryazino, Moscow oblast, 141120