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パタゴニアの氷河は,氷河期末からホロセンの移行期に,氷河の反応を示していた

Robert P Ackert1, Richard A Becker, Brad S Singer

  • 1Department of Earth and Planetary Science, Harvard University, 20 Oxford Street, Cambridge, MA 02138, USA. rackert@fas.harvard.edu

Science (New York, N.Y.)
|July 19, 2008
PubMed
まとめ

南半球の氷河は,ヤング・ドライアス (YD) 期間に冷たくなかった. 代わりに,南パタゴニア氷河場 (SPI) は,降水量の増加により進み,南西風のシフトを示した.

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