関連する実験動画
Updated: Jul 14, 2026

09:32
LabVIEW-operated Novel Nanoliter Osmometer for Ice Binding Protein Investigations
Published on: February 4, 2013
過去半世紀にわたり,南極半島の氷河フロントは後退しています
A J Cook1, A J Fox, D G Vaughan
1British Antarctic Survey, Natural Environment Research Council, Madingley Road, Cambridge CB3 0ET, UK. acook@bas.ac.uk
まとめ
南極半島の氷河は急速に後退しており,研究された氷棚の87%が61年以上にわたって縮小している. この急速な氷河の退却は,大気温暖化以外の要因が変化を牽引している可能性があることを示唆しています.
科学分野:
- 氷河学 氷河学とは
- 気候科学 気候科学
- 南極研究南極研究
背景:
- 南極半島の氷棚の退却は,大気温暖化と一般的に関連しています.
- この地域の特定の氷河の縁の位置の変化に関する研究は限られている.
- 氷河の動態を理解することは,海面上昇の予測に不可欠です.
研究 の 目的:
- 61年にわたる南極半島の海洋氷河前部の位置の動向を分析するために.
- 氷河の後退と前進の空間的なパターンを調査する.
- 観測された氷河の変化の要因を評価する.
主な方法:
- 244の海洋氷河フロントの過去のデータの分析.
- 61年間の氷河のマージンポジションのマッピング.
- 観測された撤退パターンを気候データと比較.
主要な成果:
- 研究した244の氷河のうち87%が後退している.
- 氷河の前進と後退の領域を隔てる明確な境界線が南へ移動した.
- 観測された撤退パターンは大気温暖化と一致しているが,急速な移住を示している.
結論:
- 南極半島における氷河の退却は広範囲に及び,著しい.
- 撤退境界線の南への移動は,漸進的な気候の影響を示唆しています.
- 大気温暖化が原因の可能性があるが,その速度は,氷河の退却に寄与する潜在的な追加の要因を示している.
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