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Updated: Jun 14, 2025

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在阿尔卑斯山突拉的流运输中转移效率和组织
Laura Mack1, Terje Koren Berntsen1, Nikki Vercauteren2
1Department of Geosciences, University of Oslo, Blindern, P.O. 1022, 0315 Oslo, Norway.
概括
动荡的流动驱动大气交换,但Monin-Obukhov相似性理论 (MOST) 与异质的表面作斗争. 这项研究揭示了连贯结构显著影响流运输,需要新的模型参数化.
科学领域:
- 大气科学 大气科学
- 地质物理学 地质物理学
- 环境科学 环境科学
背景情况:
- 流是大气层和地表之间动量,热量和微量气体交换的关键.
- 莫宁-奥布霍夫相似性理论 (MOST) 是参数化乱混合的标准,但假定稳定,均的条件.
研究的目的:
- 研究MOST在异质高山环境中的有效性.
- 分析流运输机制和连贯结构.
- 改进数值天气预报和气候模型的参数化.
主要方法:
- 从一个异质的阿尔卑斯山谷站点利用了四年的-协变度测量.
- 应用了对动量流量的象限分析来研究连贯结构.
- 导出了一个"组织比率" (OR) 来量化有组织与无组织的乱结构的平衡.
主要成果:
- 在占主导地位的风力部门中确定了具有不同异构和亚介质尺度运动贡献的双模流量足迹.
- 证明通过组织比率量化的连贯结构显著影响转移效率,并解释了MOST扩展函数中的分散.
- 发现转移效率与组织比率之间存在可逆关系.
结论:
- 连贯的结构在异质的原环境中的流运输中发挥着关键作用.
- 由于连贯结构的影响,现有的MOST参数化对于复杂的地形是不够的.
- 组织比为理解和潜在地改进流式运输模型提供了一个新的指标.
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