Three things you should know about permafrost
As permafrost—the frozen soil layer beneath 15% of Northern Hemisphere land—thaws due to rising global temperatures, microbes break down long-frozen organic material and release greenhouse gases. This process creates a feedback loop that accelerates climate change. MIT Technology Review reports on efforts to address intensifying fires threatening permafrost and research into understanding the complex climate effects of this thaw.
Key points
- Permafrost thawing releases powerful greenhouse gases from millennia-old organic matter
- Covers ~15% of Northern Hemisphere land; most formed during last ice age
- Creates climate feedback loop that accelerates warming
Summary and key points written by AI from the headline and a short excerpt, so they can be incomplete or wrong. MIT Technology Review did the reporting; read the original for the full story.
Read the full story at MIT Technology Review