Large Earthquakes in Subduction Zones around the Polar Regions as a Possible Reason for Rapid Climate Warming in the Arctic and Glacier Collapse in West Antarctica

Author:

Lobkovsky Leopold I.1234,Baranov Alexey A.5ORCID,Garagash Igor A.67,Ramazanov Mukamay M.78,Vladimirova Irina S.19,Gabsatarov Yurii V.19,Alekseev Dmitry A.2346,Semiletov Igor P.24

Affiliation:

1. Shirshov Institute of Oceanology of the Russian Academy of Sciences, 117997 Moscow, Russia

2. Science Department, Tomsk State University, 634050 Tomsk, Russia

3. Moscow Institute of Physics and Technology (MIPT), Phystech School of Radio Engineering and Computer Technology, 141700 Dolgoprudny, Russia

4. V.I. Il’ichev Pacific Oceanological Institute, Far Eastern Branch Russian Academy of Sciences, 690041 Vladivostok, Russia

5. Institute of Earthquake Prediction Theory and Mathematical Geophysics, Russian Academy of Sciences, 117997 Moscow, Russia

6. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, 123242 Moscow, Russia

7. Sadovsky Institute of Geosphere Dynamics, Russian Academy of Sciences, 119334 Moscow, Russia

8. Geothermal Research and Renewable Energy—Branch of Joint Institute for High Temperatures of the Russian Academy of Sciences, 367032 Makhachkala, Russia

9. Geophysical Survey of the Russian Academy of Sciences, 249035 Obninsk, Russia

Abstract

A correlation is observed between changes in the level of Earth’s seismic activity and increments of the atmospheric methane concentration over the past 40 years. Trigger mechanisms are proposed for methane emissions and glacier collapse in polar regions. These mechanisms are due to deformation waves caused by large earthquakes in subduction zones located near the polar regions: the Aleutian and Kuril–Kamchatka subduction zones, closest to the Arctic, and the Antarctica–Chilean and Tonga–Kermadec–Macquarie subduction zones. Disturbances of the lithosphere are transmitted over the distances of 3000–4000 km and more at a speed of about 100 km/year. Additional associated stresses come to the Arctic and Antarctica several decades after the occurrence of large earthquakes. In the Arctic zone, additional stresses affect the low-permeability structure of gas bearing sedimentary strata, causing increased methane emission and climate warming. In West Antarctica, deformation waves could trigger the acceleration and intensive collapse of West Antarctic glaciers, which has been observed since the 1970s. These waves are also capable of activating dormant volcanoes located under the sheet glaciers of West Antarctica, leading to an increase in heat flux, to the melting of ice at the glaciers’ base, and to their accelerated sliding towards the ocean, as is happening with the Thwaites Glacier.

Funder

P.P. Shirshov Institute of Oceanology

Tomsk State University

Institute of Earthquake Prediction Theory and Mathematical Geophysics of the Russian Academy of Sciences

Russian Scientific Foundation

Russian Science Foundation

Publisher

MDPI AG

Subject

General Earth and Planetary Sciences

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