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January 1, 1988Annals of Glaciology

A Bare Ice Field in East Queen Maud Land, Antarctica, Caused By Horizontal Divergence of Drifting Snow

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Authors

STShuhei TakahashiGifu UniversityRNRenji NaruseInpex (Japan)MNMasayoshi NakawoResearch Institute for Humanity and Nature

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Takahashi et al. (1988) studied this question.

synapsesocial.com/papers/6a71bda2af0c21e93929276bhttps://doi.org/10.1017/s0260305500006479
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Also Consider

Synapse has enriched 3 closely related papers on similar clinical questions. Consider them for comparative context:

  1. 1Effect Of Inversion Winds On Topographic Detail And Mass Balance On Inland Ice Sheets1975 · 60 citations
  2. 2Snow Accumulation at “Byrd” Station, Antarctica1972 · 24 citations
  3. 3Accumulation in the Region of Wilkes, Wilkes Land, Antarctica1964 · 83 citations