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PANGAEA.
Data Publisher for Earth & Environmental Science
Abstract:
The RECAP ice core was drilled at the Renland ice cap (71.30°N, 26.72°W, 2315 m asl) in 2015 from the surface to bedrock at a final depth of 584 m. Due to its close proximity to the east Greenland coast the record provides us with climate information reflecting past changes at the margins of the Greenland Ice Sheet. Stable water isotope ratios in polar ice record hydrological cycle changes due to isotope fractionation processes, occurring during evaporation, transportation and condensation. Here we present ultra high resolution water isotope measurements (δ18O, δ2H) obtained with Infrared-Laser Spectroscopy coupled to a state-of-the-art continuous melting system for ice core analysis. The measurements are calibrated to the VSMOW-SCALE following a daily two-point calibration. We used well defined local water standards calibrated against the primary IAEA standard waters. Using the results from the repeated VSMOW-SLAP calibrations we deduce an accuracy level of 0.02 and 0.3 ‰ for δ18O, δ2H respectively. Using spectral methods we estimate the compound noise level of the measurements directly from the δ18O and δ2H signals to be 0.08 and 0.2 ‰ respectively. Gaps in the record are filled using an iterative Maximum Entropy Method interpolation algorithm by Fahlmann and Ulrych (1982). The age scale is based on a linear interpolation of the water isotope record on the RECAP GICC05modelext Time Scale (version 1/3-2018 - PANGAEA, https://doi.org/10.1594/PANGAEA.906108).
Keyword(s):
Greenland; high-resolution; Ice cap; Ice core; Infrared Spectroscopy; oxygen and hydrogen stable isotopes; Paleoclimate; RECAP; Renland; water isotopes
References:
Fahlman, G G; Ulrych, T J (1982): A new method for estimating the power spectrum of gapped data. Monthly Notices of the Royal Astronomical Society, 199(1), 53-65, https://doi.org/10.1093/mnras/199.1.53
Gkinis, Vasileios; Popp, Trevor; Blunier, Thomas; Bigler, Matthias; Schüpbach, Simon; Kettner, E; Johnsen, Sigfús Jóhann (2011): Water isotopic ratios from a continuously melted ice core sample. Atmospheric Measurement Techniques, 4(11), 2531-2542, https://doi.org/10.5194/amt-4-2531-2011 (This introduces and describes the analytical technique for measuring stable water isotopes in ice cores using laser spectroscopy and Continuous Flow Analysis.)
Funding:
Danish National Research Foundation (DG), grant/award no. Centre for Ice and Climate
Danmarks Frie Forskningsfond, grant/award no. 2032-00228B: Iso-Deepice
European Research Council (ERC), grant/award no. 610055: Arctic Sea Ice and Greenland Ice Sheet Sensitivity
National Science Foundation (NSF), grant/award no. 1304109: Collaborative Research: Refining Long-term Climate Records from the Renland Ice Cap
Villum Fonden, grant/award no. 00022995: Unraveling paleo-climate knots with lasers
Coverage:
Latitude: 71.303667 * Longitude: -26.713111
Minimum DEPTH, ice/snow: 5.0075 m * Maximum DEPTH, ice/snow: 584.0725 m
Event(s):
RECAP * Latitude: 71.303667 * Longitude: -26.713111 * Elevation: 2340.0 m * Recovery: 584 m * Location: Renland Ice Cap, East Greenland * Method/Device: Ice drill (ICEDRILL) * Comment: drilled May to June 2015
Comment:
Technical note on the MEM gap-filling methodology:
The MEM infilled data have been generated using the Fahlmann and Ulrych (1982) MEM #interpolation scheme. The MEM infilling is carried out iteratively by first filling out the smallest gap in the #data, and then use progressively larger and larger data sections (connected by small infilled gaps) to infill larger and larger gaps in the data series. The AR order of the MEM infilling routine is adaptive (as it is limited by the length of the data sections without gaps used to calculate the AR coefficients), but the AR order #has nevertheless been capped at a maximum of 500 irrespective of data availability.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, ice/snowDepth ice/snowmGkinis, VasileiosGeocode – Centre depth of each interval
2δ18O, waterδ18O H2O‰ SMOWGkinis, VasileiosMeasured and calibrated on the SMOW/SLAP scale
3δ18O, waterδ18O H2O‰ SMOWGkinis, VasileiosMaximum Entropy Method gap-filled d18
4δ18O, water, standard deviationδ18O H2O std dev±Gkinis, VasileiosCompound measurement noise estimation for δ18O
5δ Deuterium, waterδD H2O‰ SMOWGkinis, VasileiosMeasured and calibrated on the SMOW/SLAP scale
6δ Deuterium, waterδD H2O‰ SMOWGkinis, VasileiosMaximum Entropy Method gap-filled dD
7δ Deuterium, water, standard deviationδD H2O std dev±Gkinis, VasileiosCompound measurement noise estimation for δD
8AGEAgeka BPGkinis, VasileiosGeocode – based on linear interpolation on the Simonasen et al 2019 age scale
9AgeAgeka b2kGkinis, Vasileiosbased on linear interpolation on the Simonasen et al 2019 age scale
10AgeAgea AD/CEGkinis, Vasileiosbased on linear interpolation on the Simonasen et al 2019 age scale
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0) (License comes into effect after moratorium ends)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
910280 data points

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