海の最大級の酸素不足地帯における 10 年の振動
N N Duprey1, A D Foreman1, J D Carriquiry2
1Max Planck Institute for Chemistry (Otto Hahn Institute), Mainz, Germany.
まとめ
海洋温暖化は酸素不足地域 (ODZ) に影響を及ぼします 珊瑚の窒素同位体は,東熱帯北太平洋の脱窒化における10年間のシフトを明らかにし,長期の地球温暖化傾向ではなく,太平洋の10年間の変動に関連しています.
科学分野:
- 海洋化学
- 古代海洋学
- 気候科学
背景:
- 酸素不足地帯 (ODZ) に及ぼす海洋温暖化の影響は,限られた過去のデータのために不明である.
- 過去のODZの変化を理解することは 将来の海洋脱酸素化を予測するのに不可欠です
研究 の 目的:
- 東部熱帯北太平洋 (ETNP) ODZの過去の脱窒化を再構築する.
- ODZのダイナミクスに対する10年間の気候変動の影響を調査する.
主な方法:
- 毎月解明された記録のために,サンゴの骨格に結合した窒素同位体 (CS-δ15N) を利用した.
- ETNPからの80年連続のCS-δ15を分析した.
主要な成果:
- ETNPの脱窒化と酸素欠乏における10年間の有意な変動が観察された.
- パシフィック・デカダル・ヴァリアビリティの冷たい段階でピークに達した.
- これらの段階でのより強い上流は,生産性と酸素需要を増加させる可能性が高い.
結論:
- デカダルの変動,特に太平洋のデカダルの変動は,ETNP ODZのダイナミクスを強く影響する.
- 過去の長期ODZの傾向評価は,十年振動によってバイアスされている可能性があります.
- 将来のODZの進化は,地球温暖化と10年間の気候パターンの相互作用に依存しています.
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