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Evolution of Staircase Structures in Diffusive Convection
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熱帯間の収束地帯の移動と動態
Tapio Schneider1, Tobias Bischoff1, Gerald H Haug2
11] California Institute of Technology, Pasadena, California 91125, USA [2] Department of Earth Sciences, ETH Zürich, 8092 Zürich, Switzerland.
Nature
|September 5, 2014
まとめ
熱帯間の収束地帯 (ITCZ) は,地球の最も激しい降雨が発生する場所であり,北半球の温暖化のために主として赤道から北に位置しています. その位置は,大気中のエネルギーバランスの影響を受け,季節的に,また長期にわたって変化します.
科学分野:
- 地球の降雨パターンと気候の動態に焦点を当てた気候学と大気科学.
背景:
- 熱帯間の収束地帯 (ITCZ) は,通常赤道近くに位置する,激しい降雨と曇りの地球規模の帯域です.
- その平均位置は赤道から北に観測され,大洋の熱伝導によって引き起こされる半球の温度差の影響を受けます.
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