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On the performance of twentieth century reanalysis products for Antarctic snow accumulation

  • Yetang WangEmail author
  • Shugui Hou
  • Minghu Ding
  • Weijun Sun
Article

Abstract

The strengths and weakness of the Twentieth-Century Reanalysis (20CR), the Pilot reanalysis of the twentieth-century (ERA-20C), a coupled twentieth-century climate reanalysis product (CERA-20C), and an ensemble of ten twentieth-century atmospheric model integrations (ERA-20CM), are examined for Antarctic snow accumulation based on 3265 Antarctic multi-year averaged surface mass balance observations and 79 ice core snow accumulation time series, which provides an independent estimate because they are not assimilated into the reanalyses and not used to force ERA-20CM. The ECMWF “Interim” reanalysis (ERA-Interim) and two regional climate models (RACMO2 and MAR) are also used as a complementary analysis. Despite the magnitude discrepancy between simulations and observations, large-scale spatial variability in multi-year averaged snow accumulation observations are reasonably well reproduced by all the twentieth century datasets. The four datasets capture a large fraction (> 40%) of the interannual variability in the ice core snow accumulation composite over the Antarctic Peninsula from 1901 to 2010. However, none of the twentieth century datasets alone is able to explain > 20% of variance in ice core records at the other Antarctic regions during the twentieth century. Even for the modern satellite era (from 1979 onwards), their performance for Antarctic snow accumulation is still poorer, relative to ERA-Interim, RACMO2 and MAR. Considerable inhomogeneities and spurious changes in atmospheric circulation are found in these datasets, and thus the precipitation minus evaporation/sublimation (P–E) changes and trends during the past 100 years are largely artificial over Antarctica.

Keywords

Antarctic Ice Sheet Reanalysis assessment Precipitation minus evaporation In-situ observations 

Notes

Acknowledgements

This work was supported by the National Natural Science Foundation of China (41971081 and 41576182), the Strategic Priority Research Program of the Chinese Academy of Sciences (XAD19070103), and the Outstanding Youth Fund of Shandong Provincial Universities (ZR2016JL030). We thank the two anonymous referees for their constructive and thoughtful comments to improve this paper. Thanks to the ECMWF Data Center for providing the CERA-20C, ERA-20C, ERA-20CM and ERA-Interim datasets, and to NOAA’s Earth System Research Lab for providing the 20CR dataset. RACMO2.3p2 snow accumulation data come from M. R. van de Broeke and J. M. van Wessem. The output of MAR snow accumulation fields data is available at ftp.climato.be/fettweis/MARv3.6/Antarctic/. We are also grateful to Elisabeth Schlosser and Elizabeth R. Thomas for improving English.

Supplementary material

382_2019_5008_MOESM1_ESM.docx (1.2 mb)
Supplementary material 1 (DOCX 1243 kb)

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Copyright information

© Springer-Verlag GmbH Germany, part of Springer Nature 2019

Authors and Affiliations

  1. 1.College of Geography and EnvironmentShandong Normal UniversityJinanChina
  2. 2.MOE, Key Laboratory for Coast and Island Development, School of Geographic and Oceanographic SciencesNanjing UniversityNanjingChina
  3. 3.Institute of Tibetan Plateau and Polar MeteorologyChinese Academy of Meteorological SciencesBeijingChina

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