Modeling of Explosive Pingo-like Structures and Fluid-Dynamic Processes in the Arctic Permafrost: Workflow Based on Integrated Geophysical, Geocryological, and Analytical Data

• Published in: Remote Sensing
• Main Authors: Igor Buddo, Natalya Misyurkeeva, Ivan Shelokhov, Alexandr Shein, Vladimir Sankov, Artem Rybchenko, Anna Dobrynina, Alexey Nezhdanov, Anna Parfeevets, Marina Lebedeva, Alena Kadetova, Alexander Smirnov, Oxana Gutareva, Alexey Chernikh, Lyubov Shashkeeva, Gleb Kraev
• Format: Article in Journal/Newspaper
• Language: English
• Published: MDPI AG 2024
• Subjects: permafrost; periglacial landforms; frost heaving; pingo; mound; fluid dynamics; Science; Q; Yamal Peninsula
• Online Access: https://doi.org/10.3390/rs16162948; https://doaj.org/article/afb2ab4200a043809ba2429a0979d0d5

Understanding the mechanisms responsible for the origin, evolution, and failure of pingos with explosive gas emissions and the formation of craters in the Arctic permafrost requires comprehensive studies in the context of fluid dynamic processes. Properly choosing modeling methods for the joint interpretation of geophysical results and analytical data on core samples from suitable sites are prerequisites for predicting pending pingo failure hazards. We suggest an optimal theoretically grounded workflow for such studies, in a site where pingo collapse induced gas blowout and crater formation in the Yamal Peninsula. The site was chosen with reference to the classification of periglacial landforms and their relation to the local deformation pattern, according to deciphered satellite images and reconnaissance geophysical surveys. The deciphered satellite images and combined geophysical data from the site reveal a pattern of periglacial landforms matching the structural framework with uplifted stable permafrost blocks (polygons) bounded by eroded fractured zones (lineaments). Greater percentages of landforms associated with permafrost degradation fall within the lineaments. Resistivity anomalies beneath pingo-like mounds presumably trace deeply rooted fluid conduits. This distribution can be explained in terms of fluid dynamics. N–E and W–E faults, and especially their junctions with N–W structures, are potentially the most widely open conduits for gas and water which migrate into shallow sediments in the modern stress field of N–S (or rather NEN) extension and cause a warming effect on permafrost. The results obtained with a new workflow and joint interpretation of remote sensing, geophysical, and analytical data from the site of explosive gas emission in the Yamal Peninsula confirm the advantages of the suggested approach and its applicability for future integrated fluid dynamics research.