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Image-based Lagrangian Particle Tracking in Bed-load Experiments
Published on: July 20, 2017
氷床の侵食によるフィードバックの安定化
R B Alley1, D E Lawson, G J Larson
1Department of Geosciences and EMS Environment Institute, Pennsylvania State University, University Park, Pennsylvania 16802, USA. ralley@essc.psu.edu
Nature
|August 15, 2003
まとめ
氷河の侵食率は,氷河以外の環境よりも高いが,それらをモデル化することは困難である. この研究は,氷河の地形における安定化フィードバックを特定し,氷河床の斜面が氷の表面の斜面にどのように調整されるかを明らかにします.
科学分野:
- 地球科学 地球科学 地球科学
- 氷河学 氷河学とは
- ジオモルフォロジー ジオモルフォロジー
背景:
- 氷河は,急速な沈殿プロセスを通して,山帯と盆地進化に大きく影響を与えます.
- 氷河侵食のモデリングは,河川システムとは異なり,特定された安定化フィードバックの欠如のために複雑です.
研究 の 目的:
- 氷河の地形における安定化フィードバックを特定する.
- 氷河床と表面の斜面の関係を理解するために.
- 氷河堆積物の流動に起因する干渉の影響を調査する.
主な方法:
- 氷河の形態学と進化過程の分析.
- 異なる氷河環境からの新しいデータと既存のデータの統合.
主要な成果:
- 高度に侵食性の氷河は,安定状態の床の長いプロフィールを示します.
- 氷床の斜面は,氷空間の表面の斜面よりも急さがあります.
- 非氷河期過程は,亜氷河期の深化に不可欠である.
結論:
- 氷河の地形における安定化フィードバックが特定されています.
- 氷床の斜面の動態は,氷の表面の斜面と関連しています.
- これらのフィードバックを理解することは,氷河の侵食とその影響をモデル化するための鍵です.
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