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从模拟甲循环的图坦的极地甲积累和暴雨
T Schneider1, S D B Graves, E L Schaller
1California Institute of Technology, Pasadena, California 91125, USA. tapio@caltech.edu
Nature
|January 7, 2012
概括
泰坦的甲循环反映了地球的水循环,极地甲湖主要在北方形成. 一个新的模型解释了这一点,预测北极云和湖泊水位的上升很快就会发生.
科学领域:
- 行星科学 行星科学
- 大气科学 大气科学
- 气候学 气候学 气候学
背景情况:
- 泰坦表现出类似于地球水循环的甲循环,有极地湖泊,赤道干旱和独特的云层模式.
- 以前的模型无法解释偏好的北极湖泊分布,低度暴雨的起源和南半球云集群.
研究的目的:
- 研究泰坦独特的甲分布背后的机制,包括极地湖的形成和区域降水模式.
- 开发一个模型,使泰坦甲循环的观察特征与大气和表面动态相协调.
主要方法:
- 使用三维大气模型与动态表面甲储相结合的模拟.
- 在泰坦的度范围内分析甲运输,冷,降水和蒸发过程.
主要成果:
- 甲被冷,在极地积累,特别是北方,因为北方的夏季更长,更.
- 极地降水是通过缓慢的甲运输和蒸发向中度平衡的.
- 低度的罕见,强烈的赤道风暴会产生河流特征,云层主要在夏季半球的中高度形成.
结论:
- 该模型成功地解释了泰坦观察到的甲循环特征,包括偏好的北极湖泊形成和区域降水.
- 北极云预计将在地球两年内形成,湖水位将在15年内上升.
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