1 דקות קריאה

Abstract Methane (CH4) is a potent greenhouse gas with significant implications for global warming. In recent years, the release of methane from Siberian permafrost has garnered considerable attention due to its potential to exacerbate climate change. This paper examines the causes of methane release in Siberia, its contribution to global warming, and the feedback mechanisms involved. Through an analysis of scientific studies and environmental data, the paper explores the interactions between permafrost thaw, microbial activity, and climate dynamics.

For more articles visit my blog

הערות
* כתובת הדואר האלקטרוני לא תוצג באתר.