Stable water isotopologues of arrays of high resolution 1 m snow cores from across Dronning Maud Land, East Antarctic Plateau

• Main Authors: Hirsch, Nora, Hörhold, Maria, Dallmayr, Remi, Laepple, Thomas, Freitag, Johannes, Meyer, Hanno, Weiner, Mikaela
• Format: Dataset
• Language: English
• Published: PANGAEA 2023
• Subjects: 2018_Kohnen_C4; 2018_Kohnen_C5; 2018_Kohnen_D2; 2018_Kohnen_D24; 2018_Kohnen_D38; 2018_Kohnen_D7; AWI_Envi; AWI_SPACE; Cavity Ring-Down Spectrometer (CRDS); PICARRO; L2140i; Date/Time of event; DEPTH; ice/snow; bottom/maximum; top/minimum; Deuterium excess; standard deviation; Dronning Maud Land; East Antarctic plateau; Event label; FIRNC; Firn corer; Kohnen_based; Kohnen Station; LATITUDE; Location ID; LONGITUDE; Polar Terrestrial Environmental Systems @ AWI; Position; Profile ID; Sample number; snow cores; Snow height; Space-time structure of climate change @ AWI; stable water isotopes; δ18O; water; δ Deuterium; Antarctic; Kohnen; Alfred Wegener Institute; Antarc*
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.956273; https://doi.org/10.1594/PANGAEA.956273

A set of 1 m firn profiles was sampled in December 2018 across a traverse of ~ 100 km near Kohnen Station to quantify stratigraphic noise in high resolution isotope records. At each of six different locations (D2, C4, C5, D7, D24, D38), 5 profiles were extracted on one line, perpendicularly to the overall large scale wind direction and with an interprofile spacing of 10 m. Each firn profile was vertically extracted from the snow surface by inserting a 1 m pipe of carbon fiber at the sidewall of a snow-pit. Vertical target resolution was 1.1 cm in the upper 16.5 cm and 3.3 cm in the lower part. Due compression and expanding while handling, transportation and cutting at site, we assume a maximum depth uncertainty from these steps of 2 cm. All samples (N = 1249) were packed in plastic bags and transported to Germany in a constantly frozen state. Measurements of the stable water isotopic composition (δ¹⁸O, δD) of the firn samples were done using a Cavity Ring-Down Spectroscopy instrument (CRDS) of PICARRO Inc (model L2140-i) in the Stable Isotope Facility at the Alfred Wegener Institute in Potsdam, Germany. Post-run correction was done as described in Münch et al., (2016 - doi:10.5194/cp-12-1565-2016). Scaling to the VSMOW/SLAP (Vienna Standard Mean Ocean Water/StandardLight Antarctic Precipitation) scale results in the δ-notation, describing the ratio of heavy to light isotopes in ‰. In-house standards were used for quality control. The mean combined measurement uncertainty is 0.07‰ for δ¹⁸O and 0.5‰ for δD (root mean square deviation, RMSD).