High-resolution aerosol concentration data from the Greenland NorthGRIP and NEEM deep ice cores ...

Records of chemical impurities from ice cores enable us to reconstruct the past deposition of aerosols onto polar ice sheets and alpine glaciers. Through this they allow us to gain insight into changes of the source, transport and deposition processes that ultimately determine the deposition flux at...

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Bibliographic Details
Main Authors: Erhardt, Tobias, Bigler, Matthias, Federer, Urs, Gfeller, Gideon, Leuenberger, Daiana, Stowasser, Olivia, Röthlisberger, Regine, Schüpbach, Simon, Ruth, Urs, Twarloh, Birthe, Wegner, Anna, Goto-Azuma, Kumiko, Kuramoto, Takayuki, Kjær, Helle A., Vallelonga, Paul T., Siggaard-Andersen, Marie-Louise, Hansson, Margareta E., Benton, Ailsa K., Fleet, Louise G., Mulvaney, Rob, Thomas, Elizabeth R., Abram, Nerilie, Stocker, Thomas F., Fischer, Hubertus
Format: Text
Language:unknown
Published: Copernicus Publications 2022
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Online Access:https://dx.doi.org/10.48350/167498
https://boris.unibe.ch/167498/
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Summary:Records of chemical impurities from ice cores enable us to reconstruct the past deposition of aerosols onto polar ice sheets and alpine glaciers. Through this they allow us to gain insight into changes of the source, transport and deposition processes that ultimately determine the deposition flux at the coring location. However, the low concentrations of the aerosol species in the ice and the resulting high risk of contamination pose a formidable analytical challenge, especially if long, continuous and highly resolved records are needed. Continuous flow analysis, CFA, the continuous melting, decontamination and analysis of ice-core samples has mostly overcome this issue and has quickly become the de facto standard to obtain high-resolution aerosol records from ice cores after its inception at the University of Bern in the mid-1990s. Here, we present continuous records of calcium (Ca2+), sodium (Na+), ammonium (NH4+), nitrate (NO3−) and electrolytic conductivity at 1 mm depth resolution from the NGRIP (North ...