Permafrost Thaw Emits and Absorbs CO2: New Study on Qinghai-Tibet Plateau Shows Rock Weathering Offsets 35% of River Emissions
valleyvanguardonline.comA new study on the Qinghai-Tibet Plateau reveals that permafrost thaw does more than release carbon. As frozen ground melts, rivers expose reactive minerals that accelerate rock weathering, pulling CO2 out of the environment. Researchers found that this geological process offsets about 35% of river CO2 emissions on average, and in some areas it more than cancels them out entirely. The findings challenge the common view of permafrost as a one-way carbon source. Most climate models focus on microbial decomposition of organic carbon, but this study shows that geological carbon uptake can be a significant counterweight. The balance between emissions and absorption depends on local geology, permafrost continuity, and hydrology. Scientists recommend expanding monitoring to other permafrost regions and integrating weathering models into Earth system models. Better mapping of permafrost patterns and seasonal sampling will help predict where weathering-driven uptake is most likely. This research points to a more complex carbon story in thawing landscapes.
