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AGU: Geophysical Research Letters

 

Index Terms

  • Hydrology: Glaciology
  • Meteorology and Atmospheric Dynamics: Paleoclimatology
  • Global Change: Atmosphere

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 30, 2019, 4 PP., 2003
doi:10.1029/2003GL018290

Glaciochemical investigation of an ice core from Belukha glacier, Siberian Altai

Susanne Olivier

Paul Scherrer Institute, Villigen, Switzerland

Department of Chemistry and Biochemistry, University of Bern, Bern, Switzerland

Margit Schwikowski

Paul Scherrer Institute, Villigen, Switzerland

Sabina Brütsch

Paul Scherrer Institute, Villigen, Switzerland

Stella Eyrikh

Institute for Water and Environmental Problems, Siberian Branch of the Russian Academy of Sciences, Barnaul, Russia

Heinz W. Gäggeler

Paul Scherrer Institute, Villigen, Switzerland

Department of Chemistry and Biochemistry, University of Bern, Bern, Switzerland

Martin Lüthi

Versuchsanstalt für Wasserbau, Hydrologie und Glaziologie, ETH Zürich, Zürich, Switzerland

Tatyana Papina

Institute for Water and Environmental Problems, Siberian Branch of the Russian Academy of Sciences, Barnaul, Russia

Matthias Saurer

Paul Scherrer Institute, Villigen, Switzerland

Ulrich Schotterer

Department of Chemistry and Biochemistry, University of Bern, Bern, Switzerland

Leonhard Tobler

Paul Scherrer Institute, Villigen, Switzerland

Edith Vogel

Department of Chemistry and Biochemistry, University of Bern, Bern, Switzerland

During summer 2001, a 140 m long ice core was recovered from the Belukha glacier (49°48′26″N, 86°34′43″E, 4062 m a.s.l.) in the Siberian Altai. The englacial temperature of −17°C indicates that this unique glaciochemical record is well preserved and suitable for the reconstruction of air pollution levels in this previously unexplored region. The upper 86 m were dated by 210Pb and cover the period 1862–2001. A lack of strong winter minima was observed in the δ18O record and attributed to the small amount of precipitation during that season and to wind erosion. The ion concentrations are comparable to those observed in Swiss glaciers, except for ammonium and formate, where enhanced concentrations indicate biogenic emissions from Siberian forests. Sulfate, ammonium and nitrate records all show anthropogenic impacts despite the remoteness of this site.

Received 31 July 2003; accepted 10 September 2003; published 15 October 2003.

Citation: Olivier, S., et al. (2003), Glaciochemical investigation of an ice core from Belukha glacier, Siberian Altai, Geophys. Res. Lett., 30(19), 2019, doi:10.1029/2003GL018290.

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