過去2万年にわたる中央アフリカ水文学の気候制御
Enno Schefuss1, Stefan Schouten, Ralph R Schneider
1DFG-Research Center Ocean Margins (RCOM) at the University of Bremen, Klagenfurter Strasse, 28359 Bremen, Germany. eschefuss@whoi.edu
Nature
|October 14, 2005
まとめ
過去2万年にわたる中央アフリカの降雨は,主に南大西洋の海面温度差によって引き起こされました. 海洋循環の変化は,この地域への水分輸送に大きな影響を与えました.
科学分野:
- 古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは
- 水文学 水文学とは
- 海洋学 海洋学 海洋学
背景:
- アフリカの水文学的変化は地域的にも時間的にも多様で,モンスーンによる降雨や海面温度異常などの要因の影響を受けます.
- 北アフリカと南アフリカにおける過去の降雨の変化は,プレセッショナル・インソレーションと関連しているが,熱帯北アフリカの変化は北大西洋の海面温度と相関している.
- 赤道アフリカにおける大規模な水文学的変化とその要因を理解することは,依然として課題です.
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