时间变化的过器在稳定的条件下在山区地形上的时间性能
Manuela Lehner1, Mathias W Rotach1
1Department of Atmospheric and Cryospheric Sciences, University of Innsbruck, Innrain 52f, 6020 Innsbruck, Austria.
概括
研究人员分析了-共变率数据,以找到最好的过时间来分离动荡和非动荡运动. 恒定的过时间为2-3分钟,有效地去除非流运动,同时保留流数据.
科学领域:
- 大气科学 大气科学
- 流研究 流研究
- 边界层 气象学 边界层
背景情况:
- 埃迪共变技术对于测量流是非常重要的.
- 区分动荡和非动荡运动对于准确的流量计算至关重要.
- 之前的研究使用了不同的过时间,结果不一致.
研究的目的:
- 确定最佳的间隙尺度,以分离动荡和非动荡的运动.
- 评估时间变化与恒定波器时间的性能.
- 研究大气稳定性和风速对波器时间选择的影响.
主要方法:
- 在稳定的条件下,分析了来自五个奥地利站的旋共变率数据.
- 应用福里埃分析和多分辨率流量分解来计算 (共同) 光谱.
- 间隙尺度,平均风速和稳定性参数 (z/L) 之间的相关性分析.
主要成果:
- 在间隙尺度,平均风速和稳定性参数 (z/L) 之间发现了相关性.
- 时间变化的过时间和2到3分钟的恒定过时间都有效地将流动与非流动分开.
- 过器时间对流统计数据的影响因参数和位置而异,影响水平组件和流量超过垂直风变异.
结论:
- 建议在Inn Valley分离动荡和非动荡运动时保持2-3分钟的恒定过时间.
- 时间变化的过时间虽然在理论上是合理的,但在本研究中与精心挑选的恒定过时间相比没有显著的优势.
- 这些发现为处理-共变量数据提供了实际指导,以改进流测量.
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