PM IAS MAINS GS 1 SYNOPSIS

Introduction:

Permafrost, defined by NASA as ground that remains frozen at 32°F (0°C) or colder for two consecutive years, is prevalent in high mountainous regions and polar latitudes.

About 25% of the Northern Hemisphere’s land area features permafrost, composed of soil, rocks, and sand bound by ice. Although frozen, these areas don’t always have snow cover.

Body:

Consequences of Thawing Permafrost:

Greenhouse Gas Emissions: Thawing permafrost has dire global repercussions. A major concern is the release of greenhouse gases into the atmosphere.

Massive Carbon Reservoir: NASA’s 2022 report highlighted that Arctic permafrost holds a staggering 1,700 billion metric tons of carbon, including methane and carbon dioxide. This surpasses fossil fuel emissions in 2019 by a factor of 51.

Carbon Release: Decomposition of plant matter trapped in permafrost begins as it thaws, liberating carbon into the air. This process can also unleash latent viruses and bacteria.

Industrial and Contamination Risks: The warming Arctic, with its rapid permafrost thaw, threatens numerous industrial sites and linked contaminated zones. This could result in the dissemination of hazardous substances throughout the region.

Accelerated Arctic Warming: The Arctic’s warming at almost four times the global rate due to climate change expedites permafrost thaw. This not only jeopardizes industrial sites but also contamination hotspots.

Industrial Waste Impact: The region houses diverse industrial waste such as mining and drilling byproducts, toxic substances, heavy metals, and radioactive waste.

Conclusion:

Thawing permafrost carries significant repercussions for both society and the environment. It triggers the transformation of ice-filled permafrost into a slurry, incapable of supporting overlying soil and vegetation, thus endangering infrastructure like buildings, roads, and pipelines. The situation necessitates urgent attention and remedial measures to avert the escalating consequences.

Comments

No comments yet. Why don’t you start the discussion?

Leave a Reply

Your email address will not be published. Required fields are marked *