Warming of Antarctica as a Degassing Consequence

Alex Retejum

doi:10.4236/gep.2021.92002

Abstract

The warming of Antarctica observed in recent years is one of the consequences of deep degassing associated with the northward drift of the Earth’s core. Ascending streams of hydrogen and other gases move along the tectonic faults of the lithosphere. When they get into an oxidizing environment, there is an increase in the amount of water in the ocean and air, which is accompanied by a decrease in oxygen concentrations and the release of huge amounts of energy. The provisions of the proposed theory were tested using the method of mental critical experiment. The reality of atmospheric effects of subsurface degassing is confirmed by the facts of synchronous destruction of ozone in the stratosphere and an increase in the temperature of the surface air layer. These events usually coincide with releases of ozone-depleting and heat-generating hydrogen from the subsurface.

Highlights

The warming of Antarctica observed in recent years is one of the consequences of deep degassing associated with the northward drift of the Earth’s core
The reality of atmospheric effects of subsurface degassing is confirmed by the facts of synchronous destruction of ozone in the stratosphere and an increase in the temperature of the surface air layer
For the first time in the history of meteorological observations in the Antarctica, maximum air temperature above 20 ̊ was recorded at the Argentine station Marambio on February 9, 2020

Summary

Introduction

For the first time in the history of meteorological observations in the Antarctica, maximum air temperature above 20 ̊ was recorded at the Argentine station Marambio on February 9, 2020. A. Retejum deep degassing of hydrogen caused by the accelerated drift of the Earth’s core from the Southern Hemisphere to the Northern. When they enter the oxidizing environment, the amount of water in the ocean and air dramatically increase, which is accompanied by reduced oxygen concentrations and the release of gigantic amounts of energy. The reality of the atmospheric effects of subsoil degassing must be confirmed by the facts of synchronous destruction of ozone in the stratosphere and increased temperature of the surface air layer, and it should be demonstrated that these events usually coincide in time with emissions of ozone-depleting and heat-generating hydrogen from the Earth’s subsurface.

Heat Waves and Negative Ozone Anomalies

Warm Ice

The Roles of the Erebus Volcano

The Earth’s Core Motion and Its Significance

Findings

Retejum DOI