课题基金 / 基金详情

Observations and Modeling of Orographic Cumulus Development Using Data Collected During CuPIDO 2006

Observations and Modeling of Orographic Cumulus Development Using Data Collected During CuPIDO 2006
使用 CuPIDO 2006 期间收集的数据进行地形积云发展的观测和建模
批准号:
0809214
负责人:
Joseph Zehnder
金额:
$27.17万
依托单位:
依托单位国家:
美国
项目类别:
Continuing Grant
财政年份:
2007
资助国家:
美国
项目状态:
已结题
起止时间:
2007-10-01 至 2011-01-31

项目摘要

项目成果

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中文摘要
翻译
在以前国家科学基金会的支持下,PI进行了积云摄影测量、现场和多普勒观测(CUPIDO)的实地阶段,并对收集的数据进行了初步分析。项目期间使用的观测资产包括数码相机、自动地面中网站、基于GPS的气球探测系统和配备95 GHz机载多普勒雷达的怀俄明州国王航空研究飞机。Cupido所依据的基本假设是,地形对流的开始是由于山脉上的边界层和局地地面热通量的汇合,导致局地边界层加深到自由对流的水平,随后对流和雷暴的发展是由积云和环境的相互作用控制的。特别是,人们认为,通过浅对流的作用使廓线增湿和/或稳定层被移除,为深层对流提供了有利的环境。干燥空气对热量的侵蚀在沙漠西南部可能更为明显,但作为组织对流的一种手段,对流对环境的调节可能总体上是重要的。在这项研究中,首席调查员将改进和自动化分割和立体分析技术,并利用这些技术分析在丘比多期间收集的数据。文中将描述地面强迫、中尺度上坡流的开始、对流的触发和随后的深对流发展。通过结合现场、多普勒和摄影测量数据以及云解析模型的模拟,将提供对流单体结构和周围环境演变的详细发展情况。知识价值:目标是通过研究积云夹带/剥离的机制、从浅对流向深对流转变的时间以及不同切变、稳定性和湿度廓线下积云与环境的相互作用,来扩大对积云发展的基本方面的理解。通过自动从图像中提取定量信息,首席调查员将能够处理大量案件,并扩展和推广以前关于这一主题的工作结果。特别是,他将专注于提炼由实验室模拟和高分辨率数值模拟产生的经典概念模型。更广泛的影响:除了扩大对积云对流基本原理的理解外,这些信息将对西南沙漠的业务预报员有用。高耸地形上对流边界层的演变在很大程度上还没有被探索。对不同环境条件下对流发展的汇编将使预报员能够将山谷中的条件与触发风暴的地区的条件联系起来。在本项目期间收集的数据将有助于设计和调整云参数,用于数值天气预报、中层和云解析过程模式研究以及大尺度大气环流和气候模式。该项目还依赖于各学科之间的协同作用,因为计算机科学和图像处理是分析的基本部分。
英文摘要
Under prior NSF support, the PI conducted the field phase of the Cumulus Photogrammetric, In-situ and Doppler Observations (CuPIDO) and performed preliminary analysis of the collected data. Observational assets employed during the project included digital cameras, automated surface mesonet stations, GPS based balloon sounding systems and the Wyoming King Air research aircraft with 95 GHz airborne Doppler radar. The fundamental hypotheses around which CuPIDO is based are that the onset of orographic convection results from the convergence of boundary layer over the mountain and local surface heat fluxes, leading to local boundary-layer deepening to the level of free convection and that subsequent development of the convection and thunderstorm development is governed by mutual interaction of cumulus and the environment. In particular, it is believed that moistening of the profile and/or that removal of stable layers though the action of shallow convection provides a favorable environment for deep convection. The erosion of thermals by dry air may be more pronounced in the desert southwest, but the conditioning of the environment by convection as a means of organizing convection may be important in general. In this research, the Principal Investigator will refine and automate segmentation and stereo analysis techniques and utilize these to analyze data collected during CuPIDO. A description of the surface forcing, onset of the mesoscale upslope flow, triggering of the convection and subsequent development of deep convection will be obtained. Detailed development of the structure of convective cells and the evolution of the surrounding environment will be provided through the combination of in-situ, Doppler and photogrammetric data along with simulations from a cloud resolving model. Intellectual Merit: The goal is to extend understanding of fundamental aspects of cumulus development by examining the mechanics of cumulus entrainment/detrainment, timing of the transition from shallow to deep convection and interaction of cumulus with the environment under varying shear, stability and moisture profiles. By extracting quantitative information from the images automatically, the Principal Investigator will be able to process large numbers of cases and extend and generalize the results of previous work on this subject. In particular, he will focus on refining classical conceptual models resulting from laboratory analogs and those emerging from high resolution numerical simulations. Broader Impact: In addition to extending understanding of the fundamentals of cumulus convection, this information will be of use to operational forecasters in the desert southwest. The evolution of the convective boundary layer over the elevated terrain is largely unexplored. A compilation of convective development under different environmental conditions will allow forecasters to relate conditions in the valley to those in the regions where the storms are triggered. The data collected during this project will be useful in designing and tuning cloud parameterizations for numerical weather prediction, meso- and cloud resolving process model studies and large-scale, general circulation and climate models. This project also relies on a synergy between disciplines, as computer science and image processing are essential parts of the analysis.
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Observations and Modeling of Orographic Cumulus Development Using Data Collected During CuPIDO 2006
  • 批准号:
    0638788
  • 项目类别:
    Continuing Grant
  • 资助金额:
    $35.78万
  • 财政年份:
    2007
  • 负责人:
    Joseph Zehnder
  • 依托单位:
Observations and Modeling of Orographic Cumulus Development Using Digital Imaging and Data Cataloguing
  • 批准号:
    0352988
  • 项目类别:
    Continuing Grant
  • 资助金额:
    $0.0万
  • 财政年份:
    2004
  • 负责人:
    Joseph Zehnder
  • 依托单位:
Collaborative Research: Structure and Evolution of the East Pacific Intertropical Convergence Zone under the Influence of Easterly Waves & the Madden-Julian Oscillation in EPIC
  • 批准号:
    0104234
  • 项目类别:
    Standard Grant
  • 资助金额:
    $3.05万
  • 财政年份:
    2001
  • 负责人:
    Joseph Zehnder
  • 依托单位:
Orographically Triggered Tropical Cyclones in the Eastern North Pacific
  • 批准号:
    0196313
  • 项目类别:
    Continuing Grant
  • 资助金额:
    $13.91万
  • 财政年份:
    2001
  • 负责人:
    Joseph Zehnder
  • 依托单位:
国内基金
海外基金
Galaxy Analytical Modeling Evolution (GAME) and cosmological hydrodynamic simulations.
  • 批准号:
  • 项目类别:
    省市级项目
  • 资助金额:
    10.0万元
  • 批准年份:
    2025
  • 负责人:
    Antonios Katsianis
  • 依托单位: