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  2. プレオセンの温暖期における北極風と弱まった西風
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  2. プレオセンの温暖期における北極風と弱まった西風

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プレオセンの温暖期における北極風と弱まった西風

Jordan T Abell1,2, Gisela Winckler3,4, Robert F Anderson3,4

  • 1Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY, USA. jabell@ldeo.columbia.edu.

Nature
|January 7, 2021

PubMed で要約を見る

まとめ
この要約は機械生成です。

プレオセンの時代は,氷河期と比較して,より弱く,極西風を経験しました. これは 将来の温暖化が 地球規模の風のパターンに 類似した変化をもたらす可能性があることを示唆しています

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科学分野:

  • 古代気候学
  • 大気科学
  • 海洋学

背景:

  • 中緯度西風 (ウエスターリー) は,海洋循環と気候の調節に不可欠です.
  • 西風帯は 人間の活動によって 極に向かって 移動しているようです
  • プレオセンのような温暖な時代における 過去の西風の理解は 将来の気候予測を助けます

研究 の 目的:

  • プレオセンの西風の位置と強さを再構築する.
  • 過去の暖かい期間の西風シフトのドライバーを調査する.
  • 地球温暖化による将来の風のパターンの変化を予測する.

主な方法:

  • プリオセーンとプレイストセンの初期からの塵と輸出生産性の再構築.
  • 北太平洋の塵の流れを分析する
  • 気候モデルの結果と世界の他の塵の記録との比較

主要な成果:

  • プレオセンの西風は,iNHG後の氷河期よりも弱く,より極性であった.
  • 北太平洋の塵の流れが 北半球の氷河期と一致した.
  • 粉塵と生産性の変化は,プレオ・プレイストセンの氷河期と氷河期間のサイクルを追跡した.

結論:

  • 西風の移動は主にプレオ・プレイストセンの熱グラデーションと氷の量によって引き起こされた.
  • 西風の変化は 世界的に同期していました
  • 将来の温暖化により,北極への移動が継続され,西風が弱まる可能性があります.