The Changes in Distribution of Total Ozone over the Kamchatka Region and Hazardous Endogenous Geological Phenomena, That Occurred Here in 2016-2025

A. V. Kholoptsev

Section

Research Articles

Issue

Volume 1 Issue 1 (2025): In Progress

How to Cite

Kholoptsev, A. V. (2025). The Changes in Distribution of Total Ozone over the Kamchatka Region and Hazardous Endogenous Geological Phenomena, That Occurred Here in 2016-2025. Polar and Cold Regions Research, 1(1). https://journals.explorerpress.com/index.php/pcrr/article/view/11

Authors

A. V. Kholoptsev

Sevastopol, General Ostryakov Avenue, 229/3,299020,Russia

Abstract

A pressing problem in aerology, geophysics and emergency safety is the identification of links between changes in average daily values of total ozone content (hereinafter referred to as TO) over the Kamchatka region, as well as hazardous endogenous geological phenomena occurring there (volcanic eruptions and earthquakes). Such connections may be causal in nature, since the mentioned phenomena result in a significant activation of degassing of the earth's interior, which leads to an increase in the flow of hydrogen entering the stratosphere. Since hydrogen is one of the catalysts for ozone destruction reactions, the phenomenon in question can lead to a decrease in the TO over the corresponding region. A hypothesis has been put forward that during the phenomena under consideration, a significant decrease in TO over some points in the Kamchatka region occurs more frequently than in the intervals between them. The aim of the work is to test it for the period 2016-2025, in which the indicated phenomena in the region occurred almost annually. To achieve this goal, information obtained using the OMI instrument (artificial Earth satellite AURA (NASA)) was analyzed. It was established that a significant decrease in TO over many points in the region for all the phenomena under consideration was observed with a delay of several days in relation to their onset dates. The frequencies with which this decrease occurs during periods of volcanic eruptions and earthquakes are significantly greater than in the intervals between them. The values of these frequencies are increased over areas close to the epicenters of the mentioned cataclysms. Significant decreases in TO over the region in the period under consideration occurred before the onset of the studied phenomena. This allows the identified features to be used in long-term earthquake forecasting.

Keywords:

kamchatka region, total ozone content, dangerous endogenous geological phenomena, hydrogen degassing, response, frequency

References

[1] Kholoptsev, A. V., Nikiforova, M. P., & Bolshikh, A. V. (2014). The world ocean and the ozonosphere. LAP Lambert Academic Publishing.

[2] Ali, S. M., Dash, N. K., Pradhan, A., et al. (2012). Effects of stratospheric ozone depletion on the environment and agriculture. International Journal of Advancements in Research & Technology, 1(4), 31–36. DOI:https://doi.org/10.7753/IJART0104.1005

[3] Zepp, R. G., Callaghan, T. V., & Erickson, D. J. (2003). Interactive effects of ozone depletion and climate change on biogeochemical cycles. Photochemical & Photobiological Sciences, 2, 51–61. DOI:https://doi.org/10.1039/B211445H

[4] United Nations Environment Programme (UNEP). (2010). Environmental effects of ozone depletion and its interactions with climate change: 2010 assessment. Nairobi: Author.

[5] McMichael, A. J., Lucas, R., Ponsonby, A.-L., & Edwards, S. J. (2010). Stratospheric ozone depletion, ultraviolet radiation and health. In Climate change and human health (pp. 159–180).

[6] Muller, R. (2012). Stratospheric ozone depletion and climate change. RSC Publishing. DOI:https://doi.org/10.1039/9781849734155

[7] Syvorotkin, V. L. (2016). On the nature of natural fires. Almanac Space and Time, 11(1), 22–44.

[8] Khrgian, A. Kh. (1973). Physics of atmospheric ozone [in Russian]. Gidrometeoizdat.

[9] Dessler, A. (2000). The chemistry and physics of stratospheric ozone. Academic Press. DOI:https://doi.org/10.1016/B978-012219245-8.X5000-6

[10] Mohanakumar, K. (2011). Interaction of the stratosphere and troposphere (R. Yu. Lukyanova, Trans.) [in Russian]. Fizmatlit.

[11] Syvorotkin, V. L. (2024). Degassing concept of global catastrophes. Biosphere Compatibility: Man, Region, Technology, 4, 2–11.

[12] Syvorotkin, V. L. (2019). Degassing concept of global catastrophes: Basic provisions, new results. Voprosy Geografii [Questions of Geography], 149, 35–51.

[13] Syvorotkin, V. L. (2022). Deep degassing of the Earth and volcanoes - where do terrible eruptions come from? IA Regnum, 1.05, 32–43.

[14] Syvorotkin, V. L. (2017). Volcanic eruptions. Space and Time, 1(27), 196–213.

[15] Ozerov, A. Yu. (2019). Klyuchevskoy volcano: Substance, dynamics, model [in Russian]. GEOS.

[16] Seynova, I. B., Chernomorets, S. S., Tutubalina, O. V., Barinov, A. Yu., & Sokolov, I. A. (2010). Conditions of mudflow formation in areas of active volcanism (using Klyuchevskoy and Shiveluch volcanoes, Kamchatka as an example). Part 1. Earth's Cryosphere, 14(2), 29–45. DOI:https://doi.org/10.1134/S1029334510020041

[17] Syvorotkin, V. L. (2011). Earthquakes. Space and Time, 2(4), 124–137.

[18] Gushchin, G. P. (1999). Observations of total ozone at the network of stations in Russia and the CIS. Meteorology and Hydrology, 6, 37–42.

[19] Newman, P. A. (2003). Stratospheric ozone: An electronic textbook. Studying Earth's environment from space. NASA.

[20] Hoffman, M. J. (2005). Ozone depletion and climate change. State University Press.

[21] National Oceanic and Atmospheric Administration (NOAA). Time series of TO based on information obtained by the OMI instrument. Retrieved from https://www.esrl.noaa.gov/gmd/grad/neubrew/SatO3DataTimeSeries.jsp

[22] Landau, L. D., & Lifshits, E. M. (1986). Hydrodynamics [in Russian]. Nauka.

[23] Obukhov, A. M. (1988). Turbulence and dynamics of the atmosphere [in Russian]. Gidrometeoizdat. ISBN 5-286-00059-2

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