宇宙 から 地図 に 描かれた 南極 の 下 に ある 複雑 な 半球 規模 の 景観
Helen Ockenden1,2, Robert G Bingham2, Daniel Goldberg2
1L'Institut des Géosciences de l'Environnement, Université Grenoble-Alpes, Saint-Martin-d'Hères, France.
まとめ
この研究は氷の流れの物理と衛星データを用いて 南極の隠れた氷河下の地形を地図化しています 氷床の下の詳細な地形を明らかにし 氷床の歴史や 気候変動への対応について 理解を深めます
科学分野:
- 地理学
- 氷河学
- リモートセンシング
背景:
- 南極の氷河下の風景は 氷床の歴史と 気候への反応を理解するために 極めて重要です
- 以前の氷河下マッピングは 稀少な地質学的データに依存し 空間的なバイアスを引き起こしました
- 氷の表面のトポグラフィは 基礎の岩石を反映し 新しいマッピングアプローチを提供します
研究 の 目的:
- 南極大陸の氷河下の地形図を作成する
- 氷河下の地図作成のための伝統的な地質学的調査の限界を克服する.
- メソスケールの亜氷河地形と地形を明らかにする
主な方法:
- 高解像度衛星の氷の表面の高さ地図に アイスフロー物理学を応用した.
- 氷の厚さに関する地質学的観測
- 大陸規模の亜氷河地形図を作成した.
主要な成果:
- 南極の氷河下の地形を 新しく高解像度で描いた
- メソスケール (2〜30km) の亜氷河地形を特定した.
- 氷河下の荒らしさと地質学的分布を明らかにした.
結論:
- 衛星による氷面の地形図は 氷床下マッピングの 変革のツールです
- この新しい地図は,氷河下の地形学と氷の流れへの影響の理解を深めています.
- この研究は,氷と気候の相互作用に関する将来の研究のための基礎を提供します.
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