![\"\"](\"https:\/\/www.europesays.com\/ie\/wp-content\/uploads\/2026\/06\/River-in-the-Qinghai\u2013Tibet-Plateau-with-mountains-By-Liwei-Zhang-Released-by-Umea-University-.jpg\")
River studied in the Qinghai\u2013Tibet Plateau \u2013 Credit: Liwei Zhang<\/p>\n River studied in the Qinghai\u2013Tibet Plateau \u2013 Credit: Liwei Zhang<\/p>\n
Thawing permafrost is considered a growing source of greenhouse gases as our climate warms and releases ancient carbon once stored in the frozen soils.<\/p>\n
But a new study reveals an overlooked plus side: the process will also trigger a removal of emissions from the atmosphere as the landscape thaws.<\/p>\n
The research, published in the journal<\/a> Nature, shows that rock weathering increasingly counteracts river CO2 emissions, as permafrost degrades.<\/p>\n Rivers may develop a capacity to remove CO2 through intensified rock weathering. Researchers found that warming and permafrost degradation expose reactive minerals and increase water\u2013rock interactions, accelerating chemical weathering processes that consume CO2.<\/p>\n In some river catchments, this geological carbon uptake is partially or even fully offsetting river CO2 emissions.<\/p>\n The research team from Ume\u00e5 University in Sweden and East China Normal University investigated 50 rivers across the Qinghai\u2013Tibet Plateau to understand how thawing permafrost reshapes carbon cycling. Outside of polar regions, the Plateau in southwestern China is Earth\u2019s largest high-altitude cryosphere (areas with snow or ice year round). It\u2019s often called \u201cthe Roof of the World\u201d.<\/p>\n By combining measurements of river CO2 emissions, dissolved carbon, isotopic tracers, and geochemical modeling, the researchers found evidence that thawing landscapes intensify chemical weathering, transferring carbon into dissolved inorganic forms while consuming atmospheric CO2.<\/p>\n \u201cWe found that river CO2 emissions decline while carbon uptake through rock weathering increases as permafrost cover decreases,\u201d said Liwei Zhang<\/a>, biogeochemist at East China Normal University.<\/p>\n \u201cIn some catchments where permafrost has become patchier, weathering-driven carbon uptake was large enough to offset or even exceed river CO2 emissions.\u201d<\/p>\n Across the study region, the team estimated that, on average carbon uptake from rock weathering offsets roughly 35% of river CO2 emissions.<\/p>\n However, in landscapes with discontinuous or isolated permafrost, weathering-driven carbon uptake sometimes exceeded 100 percent of river CO2 emissions, suggesting that geological carbon uptake can rival biological carbon release.<\/p>\n The findings challenge a simplified view of thawing permafrost as only a carbon source.<\/p>\n MORE CLIMATE GOOD NEWS:<\/strong> As frozen soils thaw, rivers receive large inputs of ancient organic carbon that microbes convert into greenhouse gases released to the atmosphere. But the new research suggests that geological processes operating alongside biological ones may partly counterbalance these emissions.<\/p>\n The researchers argue that future climate assessments should move beyond a sole focus on biological driven carbon emissions and, instead, incorporate geological carbon sources and sinks that emerge as frozen landscapes thaw.<\/p>\n SEND THE UNIQUE CLIMATE NEWS to Friends on Social Media\u2026<\/strong><\/p>\n","protected":false},"excerpt":{"rendered":"River studied in the Qinghai\u2013Tibet Plateau \u2013 Credit: Liwei Zhang Thawing permafrost is considered a growing source of…\n","protected":false},"author":2,"featured_media":546223,"comment_status":"","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"footnotes":"","_share_on_mastodon":"0"},"categories":[77],"tags":[83936,381,3898,18,12695,19,17,172,76243,133],"class_list":["post-546222","post","type-post","status-publish","format-standard","has-post-thumbnail","category-science","tag-breakthroughs","tag-china","tag-climate","tag-eire","tag-emissions","tag-ie","tag-ireland","tag-research","tag-rivers","tag-science"],"share_on_mastodon":{"url":"https:\/\/pubeurope.com\/@ie\/116786328628409847","error":""},"_links":{"self":[{"href":"https:\/\/www.europesays.com\/ie\/wp-json\/wp\/v2\/posts\/546222","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.europesays.com\/ie\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.europesays.com\/ie\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.europesays.com\/ie\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.europesays.com\/ie\/wp-json\/wp\/v2\/comments?post=546222"}],"version-history":[{"count":0,"href":"https:\/\/www.europesays.com\/ie\/wp-json\/wp\/v2\/posts\/546222\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.europesays.com\/ie\/wp-json\/wp\/v2\/media\/546223"}],"wp:attachment":[{"href":"https:\/\/www.europesays.com\/ie\/wp-json\/wp\/v2\/media?parent=546222"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.europesays.com\/ie\/wp-json\/wp\/v2\/categories?post=546222"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.europesays.com\/ie\/wp-json\/wp\/v2\/tags?post=546222"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}![\"\"](\"https:\/\/www.europesays.com\/ie\/wp-content\/uploads\/2026\/06\/Rivers-in-the-Qinghai\u2013Tibet-Plateau-By-Liwei-Zhang-Released-by-Umea-University.jpg\")
Another river studied in the Qinghai\u2013Tibet Plateau \u2013 Credit Liwei Zhang \/ Released by Umea University
\nCarbon uptake can even exceed emissions<\/p>\n
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