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Volume 12, issue 3 | Copyright
The Cryosphere, 12, 1069-1090, 2018
https://doi.org/10.5194/tc-12-1069-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 26 Mar 2018

Research article | 26 Mar 2018

New insights into the use of stable water isotopes at the northern Antarctic Peninsula as a tool for regional climate studies

Francisco Fernandoy1, Dieter Tetzner2, Hanno Meyer3, Guisella Gacitúa4, Kirstin Hoffmann3, Ulrike Falk5, Fabrice Lambert6, and Shelley MacDonell7 Francisco Fernandoy et al.
  • 1Facultad de Ingenieria, Universidad Andres Bello, Viña del Mar, 2531015, Chile
  • 2Center for Climate and Resilience Research, Universidad de Chile, Santiago, 8370361, Chile
  • 3Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Research Unit Potsdam, Telegrafenberg A43, 14473 Potsdam, Germany
  • 4Programa GAIA-Antártica, Universidad de Magallanes, Punta Arenas, 6210427, Chile
  • 5Climate Lab, Geography Department, University Bremen, 28334 Bremen, Germany
  • 6Department of Physical Geography, Pontificia Universidad Católica de Chile, Santiago, Chile
  • 7Centro de Estudios Avanzados en Zonas Áridas (CEAZA), La Serena, Chile

Abstract. Due to recent atmospheric and oceanic warming, the Antarctic Peninsula is one of the most challenging regions of Antarctica to understand in terms of both local- and regional-scale climate signals. Steep topography and a lack of long-term and in situ meteorological observations complicate the extrapolation of existing climate models to the sub-regional scale. Therefore, new techniques must be developed to better understand processes operating in the region. Isotope signals are traditionally related mainly to atmospheric conditions, but a detailed analysis of individual components can give new insight into oceanic and atmospheric processes. This paper aims to use new isotopic records collected from snow and firn cores in conjunction with existing meteorological and oceanic datasets to determine changes at the climatic scale in the northern extent of the Antarctic Peninsula. In particular, a discernible effect of sea ice cover on local temperatures and the expression of climatic modes, especially the Southern Annular Mode (SAM), is demonstrated. In years with a large sea ice extension in winter (negative SAM anomaly), an inversion layer in the lower troposphere develops at the coastal zone. Therefore, an isotope–temperature relationship (δT) valid for all periods cannot be obtained, and instead the δT depends on the seasonal variability of oceanic conditions. Comparatively, transitional seasons (autumn and spring) have a consistent isotope–temperature gradient of +0.69‰ °C−1. As shown by firn core analysis, the near-surface temperature in the northern-most portion of the Antarctic Peninsula shows a decreasing trend (−0.33°C year−1) between 2008 and 2014. In addition, the deuterium excess (dexcess) is demonstrated to be a reliable indicator of seasonal oceanic conditions, and therefore suitable to improve a firn age model based on seasonal dexcess variability. The annual accumulation rate in this region is highly variable, ranging between 1060 and 2470kg m−2 year−1 from 2008 to 2014. The combination of isotopic and meteorological data in areas where data exist is key to reconstruct climatic conditions with a high temporal resolution in polar regions where no direct observations exist.

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Through the geochemical analysis of the surface snow of a glacier at the northern tip of the Antarctic Peninsula, we aimed to investigate how atmosphere and ocean conditions of the surrounding region are varying under the present climate scenario. We found that meteorological conditions strongly depend on the extension of sea ice. Our results show a slight cooling of the surface air during the last decade at this site. However, the general warming tendency for the region is still on-going.
Through the geochemical analysis of the surface snow of a glacier at the northern tip of the...
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