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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Evaluation of a new cloud droplet activation parameterization with in situ data from CRYSTAL-FACE and CSTRIPE
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Evaluation of a new cloud droplet activation parameterization with in situ data from CRYSTAL-FACE and CSTRIPE

机译:评估一个新的云滴激活与现场数据参数化晶面和CSTRIPE

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摘要

The accuracy of the 2003 prognostic, physically based aerosol activation parameterization of A. Nenes and J. H. Seinfeld (NS) with modifications introduced by C. Fountoukis and A. Nenes in 2005 (modified NS) is evaluated against extensive microphysical data sets collected on board the Center for Interdisciplinary Remotely Piloted Aircraft Studies (CIRPAS) Twin Otter aircraft for cumuliform and stratiform clouds of marine and continental origin. The cumuliform cloud data were collected during NASA's Cirrus Regional Study of Tropical Anvils and Cirrus Layers–Florida Area Cirrus Experiment (CRYSTAL-FACE, Key West, Florida, July 2002), while the stratiform cloud data were gathered during Coastal Stratocumulus Imposed Perturbation Experiment (CSTRIPE, Monterey, California, July 2003). In situ data sets of aerosol size distribution, chemical composition, and updraft velocities are used as input for the NS parameterization, and the evaluation is carried out by comparing predicted cloud droplet number concentrations (CDNC) with observations. This is the first known study in which a prognostic cloud droplet activation parameterization has been evaluated against a wide range of observations. On average, predicted droplet concentration in adiabatic regions is within ~20% of observations at the base of cumuliform clouds and ~30% of observations at different altitudes throughout the stratiform clouds, all within experimental uncertainty. Furthermore, CDNC is well parameterized using either a single mean updraft velocity or by weighting droplet nucleation rates with a Gaussian probability density function of w. This study suggests that for nonprecipitating warm clouds of variable microphysics, aerosol composition, and size distribution the modified NS parameterization can accurately predict cloud droplet activation and can be successfully implemented for describing the aerosol activation process in global climate models.
机译:2003年预后的准确性,身体基于气溶胶激活的参数化。nene和j·h·宋飞(NS)的修改在2005年引入了c . Fountoukis和a . nene(修改NS)是对广泛的评估微观物理学的数据集收集上跨学科中心遥控飞机的研究(CIRPAS)双獭飞机积云状的和层状云的海洋起源大陆。收集在美国宇航局的卷云区域研究热带铁砧和卷云Layers-Florida区卷实验(晶面,基韦斯特,佛罗里达州,2002年7月),层状云数据聚集在沿海施加扰动层积云加州蒙特利实验(CSTRIPE, 7月2003)。分布、化学成分和上升气流速度作为输入使用NS进行参数化,评价通过比较预测云滴数浓度(CDNC)与观察。第一个研究的预后云液滴激活参数化广泛的观测值。平均而言,预测液滴浓度绝热区域内~ 20%的观察底部的积云状的云和~ 30%观察在不同的海拔层状云,所有的实验不确定性。参数化使用单个意味着上升气流速度或加权液滴成核率的高斯概率密度函数nonprecipitating w。这项研究表明温暖的变量云粒子物理学,气溶胶修改后的成分,和大小分布NS云参数化可以准确预测液滴激活,可以成功实现用于描述气溶胶激活在全球气候模型的过程。

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