Historical porosity data in polar firn

Abstract. In the 1990s, closed and open porosity volumes of firn samples were measured by J.-M. Barnola using the technique of gas pycnometry, on firn from three different polar sites. They are the basis of a parameterization of closed porosity in polar firn, first introduced in Goujon et al. (2003) and used in several firn physics models (e.g., Buizert et al., 2012). However, these data and their processing have not been published in their own right yet. In this short article, we detail how they were processed by J.-M. Barnola and how the closed porosity parameterization was obtained. We show that the original data processing only partially accounts for the presence of reopened bubbles in the samples. Since the proper correction to apply for this effect is hard to estimate, we also processed the data without including a correction for reopened bubbles. Finally, we made these pycnometry data available in order to be used by the glaciology community, notably for the study of polar ice formation and of the composition of gas records in ice cores. They are hosted on the PANGAEA database: https://doi.org/10.1594/PANGAEA.907678 (Fourteau et al., 2019a).

[1]  X. Faïn,et al.  Gas pycnometry firn porosity data of firn ice cores from three polar sites , 2019 .

[2]  X. Faïn,et al.  Multi-tracer study of gas trapping in an East Antarctic ice core , 2019, The Cryosphere.

[3]  O. Eisen,et al.  Critical porosity of gas enclosure in polar firn independent of climate , 2017 .

[4]  D. Etheridge,et al.  A new multi-gas constrained model of trace gas non-homogeneous transport in firn: evaluation and behaviour at eleven polar sites , 2011 .

[5]  P. M. Lang,et al.  Gas transport in firn: multiple-tracer characterisation and model intercomparison for NEEM, Northern Greenland , 2011 .

[6]  T. Stocker,et al.  High-resolution carbon dioxide concentration record 650,000–800,000 years before present , 2008, Nature.

[7]  T. Stocker,et al.  Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years , 2008, Nature.

[8]  C. Ritz,et al.  Modeling the densification of polar firn including heat diffusion: Application to close‐off characteristics and gas isotopic fractionation for Antarctica and Greenland sites , 2003 .

[9]  D. Etheridge,et al.  Reconstructing atmospheric histories from measurements of air composition in firn , 2002 .

[10]  J. Barnola,et al.  Reconstructing recent atmospheric trace gas concentrations from polar firn and bubbly ice data by inverse methods , 1997 .

[11]  D. Etheridge,et al.  Modeling air movement and bubble trapping in firn , 1997 .

[12]  Paul Duval,et al.  Bubbly-ice densification in ice sheets: II. Applications , 1997, Journal of Glaciology.

[13]  D. Etheridge,et al.  Natural and anthropogenic changes in atmospheric CO2 over the last 1000 years from air in Antarctic ice and firn , 1996 .

[14]  V. Lipenkov,et al.  Air content paleo record in the Vostok ice core (Antarctica): A mixed record of climatic and glaciological parameters , 1994 .

[15]  B. Stauffer,et al.  The age of the air in the firn and the ice at Summit, Greenland , 1993 .

[16]  D. Etheridge,et al.  Changes in tropospheric methane between 1841 and 1978 from a high accumulation‐rate Antarctic ice core , 1992 .

[17]  V. Lipenkov,et al.  Correction Of Air-content Measurements In Polar Ice For The Effect Of Cut Bubbles At The Surface Of The Sample , 1990, Journal of Glaciology.

[18]  C. Lorius,et al.  Vostok ice core provides 160,000-year record of atmospheric CO2 , 1987, Nature.

[19]  H. Oeschger,et al.  Enclosure of Air During Metamorphosis of Dry Firn to Ice , 1985, Annals of Glaciology.

[20]  B. Stauffer,et al.  Age difference between polar ice and the air trapped in its bubbles , 1984, Nature.

[21]  H. Bader Density of ice as a function of temperature and stress , 1964 .