Abstract

Permafrost landscapes are particularly susceptible to the observed climate change due to the presence of ice in the ground. This paper presents the results of the mapping and assessment of landscapes and their vulnerability to potential human impact and further climate change in the remote region of Eastern Chukotka. The combination of field studies and remote sensing data analysis allowed us to identify the distribution of landscapes within the study polygon, reveal the factors determining their stability, and classify them by vulnerability to the external impacts using a hazard index, H. In total, 33 landscapes characterized by unique combinations of vegetation cover, soil type, relief, and ground composition were detected within the 172 km2 study polygon. The most stable landscapes of the study polygon occupy 31.7% of the polygon area; they are the slopes and tops of mountains covered with stony-lichen tundra, alpine meadows, and the leveled summit areas of the fourth glacial-marine terrace. The most unstable areas cover 19.2% of the study area and are represented by depressions, drainage hollows, waterlogged areas, and places of caterpillar vehicle passage within the terraces and water-glacial plain. The methods of assessment and mapping of the landscape vulnerability presented in this study are quite flexible and can be adapted to other permafrost regions.

Highlights

  • In recent years, climate change has had a significant impact on the state of natural geosystems through an increase in the frequency of natural disasters [1] and shifts in weather characteristics

  • The aim of this paper was to study the distribution of permafrost geosystems of the Eastern Chukotka coastal plains and assess their vulnerability to climate change and potential anthropogenic impact

  • Estimation of cryogenic landscape vulnerability using an integrated multi qualitativequantitative technique was conducted for the Eastern Chukotka coastal plains and foothills

Read more

Summary

Introduction

Climate change has had a significant impact on the state of natural geosystems through an increase in the frequency of natural disasters [1] and shifts in weather characteristics. The Arctic territories are experiencing an air temperature increase twice as high as the global average [2]. The transformation of northern landscapes under the influence of climate change is complicated by the fact that their lithogenic base is represented by permafrost rocks susceptible to air temperature fluctuations. 2017, the mean annual ground temperature (MAGT) in the Arctic increased by 0.5 ◦ C [3]. These changes are accompanied by active layer thickening [4] and intensive degradation of the ice complex [5], along with thermokarst and thaw slumps development [6,7,8]. Predicting the future state of the Arctic geosystems is complicated by the formation of positive and negative feedbacks [12,13,14]

Objectives
Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call