Coherent Doppler Lidar Deployment and Data Analysis for Terrain-induced Rotor EXperiment (T-REX)
Coherent Doppler Lidar Deployment and Data Analysis for Terrain-induced Rotor EXperiment (T-REX)
批准号:
0522324
负责人:
Ronald Calhoun
金额:
$0.0万
依托单位:
依托单位国家:
美国
项目类别:
Continuing Grant
财政年份:
2005
资助国家:
美国
项目状态:
已结题
起止时间:
2005-12-15 至 2010-11-30
中文摘要
遥感仪器和数值模拟的进步现在使人们能够更全面地探测和分析与大气转子有关的三维流体动力学细节。首席调查员(PI)将参加一项实地实验(地形诱导旋翼实验;T-REX),该实验旨在于2006年3月至4月在加利福尼亚州欧文斯山谷调查大气旋翼。亚利桑那州立大学将部署其相干多普勒激光雷达,这是一个地面能量预算站,并对收集的数据进行实验后分析。对于分析,PI将侧重于涡旋结构及其动力学。PI将利用几种形式从激光雷达数据中提取信息,包括双多普勒分析和四维变分数据同化。这项研究的学术价值源于以下激励科学的问题:(1)大型旋翼的物理尺寸、强度和下游稳定性的范围是什么?(2)对波状边界上的流动的模拟表明,剪切层在山丘背风处分离,并可能卷曲成向下游平流的强涡量区。是否有证据表明这种(未被困住的)涡流向下游大气喷射?它们在什么条件下可能存在?它们的大小是否足以对飞机构成危险?(3)在山地大气旋翼的模拟中发现了次旋翼。如果他们存在,他们能有多强,他们位于哪里?这样的漩涡是如何演变的,它们的命运是什么?侧向速度波动对副旋翼发展(涡旋拉伸)有多重要?(4)对实验室流动中波浪面上的流动的模拟也显示出长的流向涡旋,这似乎与Goertler不稳定性有关。通常情况下,颗粒上升沿流向的“线”发生--这与涡流与下游方向对齐的可能性一致。有证据表明这种旋涡存在吗?它们在气溶胶进入旋翼区域的过程中有多重要?(5)表面通量的变化是否显著影响旋翼的大小和强度?该项目的更广泛影响是因为它对改善航空安全和了解与旋翼相关的气溶胶放样具有重要意义。相干多普勒激光雷达数据的获取也将有利于其他T-REX研究人员。在教育方面,亚利桑那州立大学的激光雷达已被证明是本科生和研究生的优秀教学工具。由于这种类型的激光雷达经过了广泛的工程开发,在操作程序上相对容易获得。其次,在以往的实验中,其动态、可视化的实时输出引起了学生的极大热情。
英文摘要
Advances in remote sensing instruments and numerical simulations now allow more comprehensive probing and analysis of three-dimensional fluid dynamical details associated with atmospheric rotors. The Principal Investigator (PI) will participate in a field experiment (Terrain induced Rotor Experiment; T-REX) designed to investigate atmospheric rotors in Owens Valley, California, during March and April of 2006. Arizona State University will deploy its coherent Doppler lidar, a ground-based surface energy budget station, and perform post-experiment analysis of collected data. For the analysis, the PI will focus on vortical structures and their dynamics. The PI will utilize several forms of extraction of information from the lidar data, including dual-Doppler analyses, and four dimensional variational data assimilation. The intellectual merit of the research is due to the following motivating scientific questions: (1) What are the ranges of physical size, strength, and downstream stabilities of large rotors? (2) Simulations of flows over wavy boundaries indicate that shear layers become detached over the lee of the hills and may roll-up into strong regions of vorticity that advect downstream. Is there evidence for such ejection of (non-trapped) vortices into the downstream atmosphere? Under what conditions are they likely to exist, and are their magnitudes large enough to pose a hazard to aircraft? (3) Sub-rotors have been found in simulations of mountain-induced atmospheric rotors. If they exist, how strong can they be, and where are they located? How do such vortices evolve and what is their fate? How important are lateral velocity fluctuations in the development of sub-rotors (vortex stretching)? (4) Simulations of flows over wavy surfaces in laboratory flows also show evidence of long, streamwise vortices, which appear to be related to Goertler instability. Frequently, particulate lifting occurs in streamwise "lines" - consistent with the possibility of vortices aligned with the downstream direction. Is there evidence that such vortices exist and how important are they in the lofting of aerosols into the rotor domain? (5) Do variations in surface fluxes significantly affect the size and strength of rotors? The project's broader impacts are due to its significance for improving aviation safety and understanding aerosol lofting associated with rotors. The acquisition of coherent Doppler lidar data also will be beneficial to other T-REX investigators. Educationally, the Arizona State University lidar has proven to be an excellent teaching tool for undergraduate and graduate students. Because this type of lidar has gone through extensive engineering development, it is relatively accessible, in terms of operational procedures. Secondly, in prior experiments, its dynamic and visual real-time output has generated much student enthusiasm.
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Collaborative Research: Observing and Modeling Downslope-windstorm-type Flow in a Small-scale Crater Induced by Larger-scale Katabatic Winds
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批准号:1160737
-
项目类别:Standard Grant
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资助金额:$15.46万
-
财政年份:2012
-
负责人:Ronald Calhoun
-
依托单位:
EAGER: Collaborative Analysis of Doppler Lidar Data from Canopy Horizontal Array Turbulence Study (CHATS)
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批准号:1230055
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项目类别:Standard Grant
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资助金额:$3.15万
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财政年份:2012
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负责人:Ronald Calhoun
-
依托单位:
Collaborative Research: Data Assimilation of Dual Doppler Lidar Observations of the Urban Boundary Layer
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批准号:0352185
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项目类别:Continuing Grant
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资助金额:$10.15万
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财政年份:2004
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负责人:Ronald Calhoun
-
依托单位:
国内基金
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