IngentaConnect Seasonal and spatial variations of snow chemistry on Mount Logan,...

Authors: Goto-Azuma, Kumiko; Koerner, Roy M.; Demuth, Michael N.; Watanabe, Okitsugu

Source: Annals of Glaciology, Volume 43, Number 1, September 2006 , pp. 177-186(10)

Publisher: International Glaciological Society

Abstract:

Three ice cores were recovered on or near Mount Logan, Yukon, Canada, at 3017, 4135 and 5340 m a.s.l. in 2002. Prior to ice-core drilling, we collected snow-pit and shallow core samples from Mount Logan in 2001 to study seasonal and spatial variations of snow chemistry. We dug snow pits at six sites between 2420 and 5340 m a.s.l. before the beginning of the melt season, with the exception of a pit at 3180 m a.s.l., where the melt season had just started but had affected only the near-surface stratigraphy. Three of the pits were extended deeper with a shallow core. The snow-pit and core samples were analyzed for ion chemistry and δ¹⁸O. A series of depth profiles of ions and δ¹⁸O shows spatial variations, though characteristic peaks can usually be traced across all the profiles. Concentrations and deposition fluxes of Na⁺ and Cl⁻, which are mainly of sea-salt origin, decrease with altitude. On the other hand, deposition fluxes of NO₃⁻, SO₄²⁻, Ca²⁺ and NH₄⁺ show a weak positive relationship with elevation below the summit plateau. Stable isotopes (δ¹⁸O) decrease with altitude, with a distinctive jump between 3200 and 4500 m a.s.l., as was reported previously. Stable isotopes (δ¹⁸O), Cl⁻, CH₃SO₃⁻(MSA), Na⁺ and Ca²⁺ show clear seasonal variations, which would enable us to date the cores by annual-layer counting.

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Seasonal and spatial variations of snow chemistry on Mount Logan, Yukon, Canada