Annual layer thicknesses and age-depth (oldest estimate) of Derwael Ice Rise (IC12), Dronning Maud Land, East Antarctica: Supplement to: Philippe, M et al. (2016): Ice core evidence for a 20th century increase in surface mass balance in coastal Dronning Maud Land, East Antarctica. The Cryosphere, 10(5), 2501-2516, doi:10.5194/tc-10-2501-2016

A 120 m-long ice core was drilled in 2012 on the Derwael Ice Rise, coastal Dronning Maud Land, East Antarctica. Water stable isotopes (d18O and dD) stratigraphy is supplemented by discontinuous major ion profiles and continuous electrical conductivity measurements. The base of the ice core is dated...

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Bibliographic Details
Main Authors: Philippe, Morgane, Tison, Jean-Louis, Fjosne, Karen, Hubbard, Bryn, Kjær, Helle Astrid, Lenaerts, Jan T M, Drews, Reinhard, Sheldon, Simon S.G., De Bondt, Kevin, Claeys, Philippe, Pattyn, Frank
Format: Other/Unknown Material
Language:English
Published: 2016
Subjects:
Online Access:http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/249952
https://dipot.ulb.ac.be/dspace/bitstream/2013/249952/3/PANGAEA.857574
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Summary:A 120 m-long ice core was drilled in 2012 on the Derwael Ice Rise, coastal Dronning Maud Land, East Antarctica. Water stable isotopes (d18O and dD) stratigraphy is supplemented by discontinuous major ion profiles and continuous electrical conductivity measurements. The base of the ice core is dated to AD 1759 ± 16, providing a climate proxy for the past ~250 years. This data set presents the core's annual layer thickness history in meters water equivalent for the oldest age-depth estimate before correction for the influence of ice deformation info:eu-repo/semantics/published