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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 13, issue 1
Clim. Past, 13, 61–71, 2017
https://doi.org/10.5194/cp-13-61-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: International Partnerships in Ice Core Sciences (IPICS) Second...

Clim. Past, 13, 61–71, 2017
https://doi.org/10.5194/cp-13-61-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 16 Jan 2017

Research article | 16 Jan 2017

Climatic variability in Princess Elizabeth Land (East Antarctica) over the last 350 years

Alexey A. Ekaykin et al.

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Altnau, S., Schlosser, E., Isaksson, E., and Divine, D.: Climatic signals from 76 shallow firn cores in Dronning Maud Land, East Antarctica, The Cryosphere, 9, 925–944, https://doi.org/10.5194/tc-9-925-2015, 2015.
Carril, A. F. and Navarra, A.: Low-frequency varibility of the Antarctic Circumpolar Wave, Geophys. Res. Lett., 28, 4623–4626, 2001.
Divine, D. V., Isaksson, E., Kaczmarska, M., Godtliebsen, F., Oerter, H., Schlosser, E., Johnsen, S. J., van den Broeke, M., and van de Wal, R. S. W.: Tropical Pacific – high latitude south Atlantic teleconnections as seen in δ18O variability in Antarctic coastal ice cores, J. Geophys. Res., 114, D11112, https://doi.org/10.1029/2008JD010475, 2009.
Dong, B. and Dai, A.: The influence of the Interdecadal Pacific Oscillation on temperature and precipitation over the globe, Clim. Dynam., 15, 2667, https://doi.org/10.1007/s00382-015-2500-x, 2015.
Ekaykin, A. A.: Meteorological regime of central antarctica and its role in the formation of isotope composition of snow thickness, Universite Joseph Fourier, Grenoble, 136 pp., 2003.
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Understanding the Antarctic climate system is crucial in the context of the present-day global environmental changes, but key gaps arise from limited observations. We present a new reconstructed stacked climate record for Princess Elizabeth Land, East Antarctica. Records show 1 °C warming over the last 350 years, with a particularly cold period from the mid-18th to mid-19th century. Temperature variability with a period > 27 years is mainly related to the anomalies of the Indian Ocean Dipole mode.
Understanding the Antarctic climate system is crucial in the context of the present-day global...
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