A Greenland ice core record of H2 reveals enhanced sensitivity to climate

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The study analyzes the first Greenland ice-core record of atmospheric hydrogen (H2) spanning the last millennium to evaluate how H2 responds to climate and anthropogenic changes. Using ice-core H2 measurements despite H2’s high permeability in ice, the authors report a 60% rise in atmospheric H2 from preindustrial to modern times, interpret it as consistent with increased direct emissions from fossil-fuel burning and elevated H2 precursor concentrations, and find a 16% decrease during the Little Ice Age, with no more than half of that decrease attributable to changes in biomass burning. The authors also state that their results limit the strength of a previously proposed geologic source of H2 and demonstrate that conventional estimates likely underestimate the climate sensitivity of H2 biogeochemistry. The paper does not explicitly discuss endometriosis or adenomyosis; it was included in the corpus via a keyword match in the upstream search index.

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Abstract

Abstract Anthropogenic emissions of hydrogen (H2) are expected to rise with increasing production and use during the green energy transition. Although atmospheric H2 is not radiatively active, it warms the Earth’s climate via chemical effects on methane, ozone, and water vapor1-6. Predicting the atmospheric response to anthropogenic perturbations is challenging due to the limitations of the modern instrumental record. Ice core measurements of H2 can greatly extend the observational record and provide enhanced dynamic range to test theories about the global biogeochemistry and climate sensitivity of H2. Ice core measurements of H2 are challenging because of the uniquely high permeability of H2 in ice. Here we present the first ice core record of atmospheric H2 recovered from a Greenland ice core, spanning the last millennium. The record shows a 60% rise in atmospheric H2 from the preindustrial to the modern, consistent with increasing direct emissions from fossil fuel burning and increased atmospheric concentrations of H2 precursors. The results limit the strength of the previously proposed geologic source of H2. The record also shows a 16% decrease in H2 levels during the Little Ice Age. No more than half of that decrease can be attributed to biomass burning changes. These results demonstrate that conventional estimates likely underestimate the climate sensitivity of H2 biogeochemistry. This sensitivity must be accounted for in estimates of the radiative consequences of anthropogenic emissions in a warming climate.
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A Greenland ice core record of H2 reveals enhanced sensitivity to climate | Research Square window.SnipcartSettings = { analytics: { enabled: false } }; (function() { var accessVector = localStorage.getItem('access_vector') || ''; window.dataLayer = window.dataLayer || []; if (accessVector) { window.dataLayer.push({ user: { profile: { profileInfo: { snid: accessVector } } } }); } })(); (function(w,d,s,l,i){w[l]=w[l]||[];w[l].push({'gtm.start':new Date().getTime(),event:'gtm.js'});var f=d.getElementsByTagName(s)[0],j=d.createElement(s),dl=l!='dataLayer'?'&l='+l:'';j.async=true;j.src='https://www.googletagmanager.com/gtm.js?id='+i+dl;f.parentNode.insertBefore(j,f);})(window,document,'script','dataLayer','GTM-K279D39R'); Browse Preprints In Review Journals COVID-19 Preprints AJE Video Bytes Research Tools Research Promotion AJE Professional Editing AJE Rubriq About Preprint Platform In Review Editorial Policies Our Team Advisory Board Help Center Sign In Submit a Preprint Cite Share Download PDF Physical Sciences - Article A Greenland ice core record of H2 reveals enhanced sensitivity to climate John Patterson, Murat Aydin, Miranda Miranda, Eric Saltzman This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-7320711/v1 This work is licensed under a CC BY 4.0 License Status: Published Journal Publication published 04 Feb, 2026 Read the published version in Nature → Version 1 posted You are reading this latest preprint version Abstract Anthropogenic emissions of hydrogen (H2) are expected to rise with increasing production and use during the green energy transition. Although atmospheric H2 is not radiatively active, it warms the Earth’s climate via chemical effects on methane, ozone, and water vapor1-6. Predicting the atmospheric response to anthropogenic perturbations is challenging due to the limitations of the modern instrumental record. Ice core measurements of H2 can greatly extend the observational record and provide enhanced dynamic range to test theories about the global biogeochemistry and climate sensitivity of H2. Ice core measurements of H2 are challenging because of the uniquely high permeability of H2 in ice. Here we present the first ice core record of atmospheric H2 recovered from a Greenland ice core, spanning the last millennium. The record shows a 60% rise in atmospheric H2 from the preindustrial to the modern, consistent with increasing direct emissions from fossil fuel burning and increased atmospheric concentrations of H2 precursors. The results limit the strength of the previously proposed geologic source of H2. The record also shows a 16% decrease in H2 levels during the Little Ice Age. No more than half of that decrease can be attributed to biomass burning changes. These results demonstrate that conventional estimates likely underestimate the climate sensitivity of H2 biogeochemistry. This sensitivity must be accounted for in estimates of the radiative consequences of anthropogenic emissions in a warming climate. Earth and environmental sciences/Climate sciences/Palaeoclimate Earth and environmental sciences/Climate sciences/Atmospheric science/Atmospheric chemistry Earth and environmental sciences/Biogeochemistry/Element cycles Full Text Additional Declarations There is NO Competing Interest. Cite Share Download PDF Status: Published Journal Publication published 04 Feb, 2026 Read the published version in Nature → Version 1 posted You are reading this latest preprint version Research Square lets you share your work early, gain feedback from the community, and start making changes to your manuscript prior to peer review in a journal. As a division of Research Square Company, we’re committed to making research communication faster, fairer, and more useful. We do this by developing innovative software and high quality services for the global research community. Our growing team is made up of researchers and industry professionals working together to solve the most critical problems facing scientific publishing. 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