コメントへの返信 "海底バチメトリーの気象による気象変動に対する感受性"
1Lamont-Doherty Earth Observatory, Columbia University, Palisades NY, USA. jaolive@ldeo.columbia.edu.
まとめ
急速に広がる海底の水位測定は 10万年のサイクルを明らかにし これらの山脊は海面の変化を記録する 鍵となるものだと示唆しています この発見は,長期の海面変動を理解する彼らの可能性を強調しています.
科学分野:
- 地理学
- 海洋学
- 気候科学
背景:
- 急速に広がる海底バチメトリの10万年周期が以前報告されていた.
- 海面の変化が地球上の海底の形状にどの程度影響するかについては,まだ議論が続いている.
研究 の 目的:
- 異なる広がり速度における海底バチメトリにおける地質学とミランコビッチ周期性の関係を評価する.
- 急速に広がる山脊が 海面の標識を記録する役割を 再度強調する
主な方法:
- 海底のバチメトリーデータ分析
- 構造周期とミランコビッチ周期の比較
- 様々な海底の広がり率を評価する
主要な成果:
- 特徴的な10万年の期間は,急速に広がる海底の水量で確認されています.
- 海平面の変化を記録する最も強い可能性を示している.
結論:
- 急速に広がる山脊は,海底の水位測定で海水位信号を検出するのに最適な場所です.
- バチメトリーの10万年周期は,これらの特定の場所の海底形態学に対する海面変化の影響を支持しています.
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