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A method for retrieving the cumulus entrainment rate from ground based observations.

机译:一种从地面观测中检索积云夹带率的方法。

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摘要

The entrainment of drier environmental air into cumulus clouds affects the impact that these clouds have on the environment by modifying their radiative, microphysical, and thermodynamic characteristics. Entrainment is a difficult parameter to observe directly, and heretofore has been obtained from occasional aircraft penetrations.;To increase the number of cumulus entrainment rate observations under a wide range of atmospheric conditions, an algorithm for retrieving the cumulus entrainment rate from ground-based remote sensing observations has been developed. This algorithm, called the Entrainment Rate In Cumulus Algorithm (ERICA), uses the suite of instruments at the Southern Great Plains (SGP) site of the United States Department of Energy's Atmospheric Radiation Measurement (ARM) Climate Research Facility as inputs into a Gauss-Newton optimal estimation scheme. The forward model in this algorithm is the Explicit Mixing Parcel Model (EMPM), a cloud parcel model that treats entrainment as a series of discrete mixing events. Output from EMPM is used to calculate quantities that can be observed from the surface, including effective radius and liquid water path. The entrainment rate in EMPM is adjusted iteratively until the modeled output converges to the observations. Sensitivity testing and error and information content analysis show that ERICA is a robust method for obtaining accurate estimates of entrainment rate without the drawbacks of aircraft observations.;Results from a three-month trial of ERICA show significant variability of the entrainment rate of clouds in a single day and from one day to the next. The mean value from this analysis corresponds well with prior knowledge of the entrainment rate.
机译:干燥的环境空气夹带积云,通过改变其辐射,微物理和热力学特性,影响这些云对环境的影响。夹带是一个很难直接观测的参数,迄今为止已经从飞机的偶尔穿透中获得。为了增加大范围大气条件下积云夹带率观测值的数量,一种从地面远程获取积云夹带率的算法传感观测已经发展。该算法称为累积积水率算法(ERICA),它使用美国能源部大气辐射测量(ARM)气候研究设施的南部大平原(SGP)站点上的一套仪器作为高斯-牛顿最优估计方案。此算法中的正向模型是显式混合包裹模型(EMPM),这是一种将包裹作为一系列离散混合事件处理的云包裹模型。 EMPM的输出用于计算可以从表面观察到的数量,包括有效半径和液体水路径。迭代调整EMPM中的夹带率,直到模型输出收敛到观测值为止。敏感性测试以及错误和信息内容分析表明,ERICA是一种获取夹带率的准确估计值的可靠方法,而没有飞机观测的缺点。ERICA为期三个月的试验结果表明,云层中夹带率的显着变化。一天,从一天到第二天。该分析的平均值与先前的夹带率知识非常吻合。

著录项

  • 作者

    Wagner, Timothy J.;

  • 作者单位

    The University of Wisconsin - Madison.;

  • 授予单位 The University of Wisconsin - Madison.;
  • 学科 Atmospheric Sciences.;Remote Sensing.
  • 学位 Ph.D.
  • 年度 2011
  • 页码 108 p.
  • 总页数 108
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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