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A first chronology for the North Greenland Eemian Ice Drilling (NEEM) ice core

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Title A first chronology for the North Greenland Eemian Ice Drilling (NEEM) ice core
Names Rasmussen, S. O. (creator)
Abbott, P. M. (creator)
Blunier, T. (creator)
Bourne, A. J. (creator)
Brook, Edward J. (creator)
Buchardt, S. L. (creator)
Buizert, Christo (creator)
Chappellaz, J. (creator)
Clausen, H. B. (creator)
Cook, E. (creator)
Dahl-Jensen, D. (creator)
Davies, S. M. (creator)
Guillevic, M. (creator)
Kipfstuhl, S. (creator)
Laepple, T. (creator)
Seierstad, I. K. (creator)
Severinghaus, J. P. (creator)
Steffensen, J. P. (creator)
Stowasser, C. (creator)
Svensson, A. (creator)
Vallelonga, P. (creator)
Vinther, B. M. (creator)
Wilhelms, F. (creator)
Winstrup, M. (creator)
Date Issued 2013 (iso8601)
Note This is the publisher’s final pdf. The published article is copyrighted by the author(s) and published by Copernicus Publications on behalf of the European Geosciences Union. The published article can be found at: http://www.clim-past.net/volumes_and_issues.html.
Abstract A stratigraphy-based chronology for the North
Greenland Eemian Ice Drilling (NEEM) ice core has been
derived by transferring the annual layer counted Greenland
Ice Core Chronology 2005 (GICC05) and its model extension
(GICC05modelext) from the NGRIP core to the NEEM
core using 787 match points of mainly volcanic origin identified
in the electrical conductivity measurement (ECM) and
dielectrical profiling (DEP) records. Tephra horizons found
in both the NEEM and NGRIP ice cores are used to test the
matching based on ECM and DEP and provide five additional
horizons used for the timescale transfer.
A thinning function reflecting the accumulated strain
along the core has been determined using a Dansgaard–Johnsen flow model and an isotope-dependent accumulation
rate parameterization. Flow parameters are determined from
Monte Carlo analysis constrained by the observed depth-age
horizons.
In order to construct a chronology for the gas phase, the ice
age–gas age difference (Δage) has been reconstructed using
a coupled firn densification-heat diffusion model. Temperature
and accumulation inputs to the Δage model, initially derived
from the water isotope proxies, have been adjusted to optimize the fit to timing constraints from δ¹⁵N of nitrogen
and high-resolution methane data during the abrupt onset of
Greenland interstadials.
The ice and gas chronologies and the corresponding thinning
function represent the first chronology for the NEEM
core, named GICC05modelext-NEEM-1. Based on both the
flow and firn modelling results, the accumulation history
for the NEEM site has been reconstructed. Together, the
timescale and accumulation reconstruction provide the necessary
basis for further analysis of the records from NEEM.
Genre Article
Access Condition http://creativecommons.org/licenses/by/3.0/us/
Identifier Rasmussen, S. O., Abbott, P. M., Blunier, T., Bourne, A. J., Brook, E., Buchardt, S. L., Buizert, C., Chappellaz, J., Clausen, H. B., Cook, E., Dahl-Jensen, D., Davies, S. M., Guillevic, M., Kipfstuhl, S., Laepple, T., Seierstad, I. K., Severinghaus, J. P., Steffensen, J. P., Stowasser, C., Svensson, A., Vallelonga, P., Vinther, B. M., Wilhelms, F., and Winstrup, M.: A first chronology for the North Greenland Eemian Ice Drilling (NEEM) ice core, Climate of the Past, 9, 2713-2730, doi:10.5194/cp-9-2713-2013, 2013.

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