14-CO in glacial ice from Law Dome, Antarctica as a tracer of changes in atmospheric OH abundance from 1870 AD to present

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dc.contributor.authorSmith, AMen_AU
dc.contributor.authorNeff, PDen_AU
dc.contributor.authorPetrenko, VVen_AU
dc.contributor.authorEtheridge, DMen_AU
dc.contributor.authorCrosier, EMen_AU
dc.contributor.authorHmiel, Ben_AU
dc.contributor.authorThornton, DPen_AU
dc.contributor.authorJong, LMen_AU
dc.contributor.authorBeaudette, Ren_AU
dc.contributor.authorHarth, CMen_AU
dc.contributor.authorLangenfelds, RLen_AU
dc.contributor.authorMitrevski, Ben_AU
dc.contributor.authorCurran, MAJen_AU
dc.contributor.authorBuizert, Cen_AU
dc.contributor.authorMurray, LTen_AU
dc.contributor.authorTrudinger, CMen_AU
dc.contributor.authorDyonisius, MNen_AU
dc.contributor.authorNg, Jen_AU
dc.contributor.authorSeveringhaus, JPen_AU
dc.contributor.authorWeiss, RFen_AU
dc.date.accessioned2022-05-27T03:16:00Zen_AU
dc.date.available2022-05-27T03:16:00Zen_AU
dc.date.issued2021-11-15en_AU
dc.date.statistics2022-05-27en_AU
dc.description.abstractHydroxyl, OH, is the main tropospheric oxidant and determines the lifetime of methane and most other trace gases in the atmosphere, thereby controlling the amount of greenhouse warming produced by these gases. Changes in OH concentration ([OH]) in response to large changes in reactive trace gas emissions (which may occur in the future) are uncertain. Measurements of 14C containing carbon monoxide (14CO) and other tracers such as methyl chloroform over the last ≈25 years have been successfully used to monitor changes in average [OH], but there are no observational constraints on [OH] further back in time. Reconstructions of 14CO from ice cores could in principle provide such constraints but are complicated by in-situ production of 14CO by cosmic rays directly in the ice. Recent work in Antarctica and Greenland shows that this in-situ component would be relatively small and can be accurately corrected for at sites with very high snow accumulation rates. A joint US and Australian team sampled and measured firn air and ice at Law Dome, Antarctica (2018-19 season, site DE08-OH, 1.2 m a-1 ice-equivalent snow accumulation), to a maximum depth of 240 m. Trapped air was extracted from the ice using an onsite large-volume ice melting system. Preliminary comparisons of methane measured in the samples to existing ice core records and atmospheric measurements suggest ice core air sample ages spanning from the 1870s to the early 2000s. Firn-air samples from the snow surface to 81 m depth capture air from the early 2000s to present. Analyses of [CO] and halocarbons in the samples show a relatively low and stable procedural CO blank and demonstrate that the samples are unaffected by ambient air inclusion. 14CO analyses in these firn and ice core air samples have been successfully completed. Corrections for in-situ 14CO production, validated against direct atmospheric measurements for the more recent samples, have allowed us to develop a preliminary 14CO history. This history will be interpreted with the aid of the GEOS-Chem chemistry-transport model to place the first observational constraints on the variability of Southern Hemisphere [OH] since ≈1870 AD. © The Authorsen_AU
dc.identifier.citationSmith, A., Neff, P., Petrenko, V., Etheridge, D., Crosier, E., Hmiel, B., Thornton, D., Jong, L., Beaudette, R., Harth, C., Langenfelds, R., Mitrevski, B., Buizert, C. Murray, L., Trudinger, C., Dyonisius, M., Ng, J., Severinghaus, J. & Weiss, R. (2021). 14-CO in glacial ice from Law Dome, Antarctica as a tracer of changes in atmospheric OH abundance from 1870 AD to present. Paper presented to the 15th International Conference on Accelerator Mass Spectrometry, ANSTO, Sydney, Australia, November 15th – 19th. (pp. 23). Retrieved from: https://ams15sydney.com/wp-content/uploads/2021/11/AMS-15-Full-Program-and-Abstract-Book-R-1.pdfen_AU
dc.identifier.conferenceenddate19 November 2021en_AU
dc.identifier.conferencename15th International Conference on Accelerator Mass Spectrometryen_AU
dc.identifier.conferenceplaceSydney, Australiaen_AU
dc.identifier.conferencestartdate15 November 2021en_AU
dc.identifier.pagination23en_AU
dc.identifier.urihttps://ams15sydney.com/wp-content/uploads/2021/11/AMS-15-Full-Program-and-Abstract-Book-R-1.pdfen_AU
dc.identifier.urihttps://apo.ansto.gov.au/dspace/handle/10238/13218en_AU
dc.language.isoenen_AU
dc.publisherAustralian Nuclear Science and Technology Organisationen_AU
dc.subjectCarbon 14en_AU
dc.subjectGlaciersen_AU
dc.subjectAntarcticaen_AU
dc.subjectGasesen_AU
dc.subjectControlled atmospheresen_AU
dc.subjectGreenhouse effecten_AU
dc.subjectGreenhouse gasesen_AU
dc.subjectCarbon monoxideen_AU
dc.subjectIceen_AU
dc.subjectDrill coresen_AU
dc.subjectSnowen_AU
dc.subjectSouthern Hemisphereen_AU
dc.title14-CO in glacial ice from Law Dome, Antarctica as a tracer of changes in atmospheric OH abundance from 1870 AD to presenten_AU
dc.typeConference Abstracten_AU
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