Journal of Geoscience and Environment Protection

Volume 9, Issue 2 (February 2021)

ISSN Print: 2327-4336   ISSN Online: 2327-4344

Google-based Impact Factor: 0.98  Citations  

Warming of Antarctica as a Degassing Consequence

HTML  XML Download Download as PDF (Size: 3817KB)  PP. 17-41  
DOI: 10.4236/gep.2021.92002    101 Downloads   357 Views  
Author(s)

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.

Share and Cite:

Retejum, A. (2021) Warming of Antarctica as a Degassing Consequence. Journal of Geoscience and Environment Protection, 9, 17-41. doi: 10.4236/gep.2021.92002.

Cited by

No relevant information.

Copyright © 2020 by authors and Scientific Research Publishing Inc.

Creative Commons License

This work and the related PDF file are licensed under a Creative Commons Attribution 4.0 International License.