Gas transport in firn: Multiple-tracer characterisation and model intercomparison for NEEM, Northern Greenland

Buizert, C, Martinerie, P, Petrenko, VV, Severinghaus, JP, Trudinger, CM, Witrant, E, Rosen, JL, Orsi, AJ, Rubino, M, Etheridge, DM, Steele, LP, Hogan, C, Laube, JC, Sturges, WT, Levchenko, VA, Smith, AM, Levin, I, Conway, TJ, Dlugokencky, EJ, Lang, PM, Kawamura, K, Jenk, TM, White, JWC, Sowers, T, Schwander, J and Blunier, T (2011) Gas transport in firn: Multiple-tracer characterisation and model intercomparison for NEEM, Northern Greenland. Atmospheric Chemistry and Physics Discussions, 11 (5). pp. 15975-16021. ISSN 1680-7375

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Abstract

Compacted snow (firn) preserves a continuous record of atmospheric composition up to a century back in time. Firn air transport modeling is essential for interpretation of firn gas records. Each site needs to be characterised individually through a tuning procedure, in which the effective diffusivity at each depth is adjusted to optimise the agreement between modeled and measured mixing ratios of a selected reference gas (usually CO2). We present the characterisation of the NEEM site, Northern Greenland (77.45° N 51.06° W), where an ensemble of ten reference tracers is used to constrain the diffusivity reconstruction. By analysing uncertainties in both data and the reference gas atmospheric histories, we can objectively assign weights to each of the gases used for the model tuning, and define a root mean square criterion that is minimised in the tuning. Each tracer constrains the firn profile differently through its unique atmospheric history and free air diffusivity, making our multiple-tracer characterisation method a clear improvement over the commonly used single-tracer tuning. Six firn air transport models are tuned to the NEEM site; all models successfully reproduce the data within a 1Ï Gaussian distribution. The modern day Î"age, i.e. the difference between gas age and ice age, is calculated to be 182 ± 8 yr. We find evidence that diffusivity does not vanish completely in the firn lock-in zone, as is commonly assumed. We further present the first intercomparison study of firn air models, where we introduce diagnostic scenarios designed to probe specific aspects of the model physics. Our results show that there are major differences in the way the models handle advective transport. Furthermore diffusive fractionation of isotopes in the firn is poorly constrained by the models, which has consequences for attempts to reconstruct the isotopic composition of trace gases back in time using firn air and ice core records.

Item Type: Article
Faculty \ School: Faculty of Science > School of Environmental Sciences
Related URLs:
Depositing User: Rosie Cullington
Date Deposited: 28 Jun 2011 10:07
Last Modified: 13 Aug 2020 23:29
URI: https://ueaeprints.uea.ac.uk/id/eprint/33087
DOI: 10.5194/acpd-11-15975-2011

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