Experimental and Numerical Investigations of Spectral Broadening and the Onset of Precipitation in Warm Rain In Cumulus over the Ocean (RICO) Cumuli

海洋上空积云 (RICO) 的光谱展宽和暖雨降水开始的实验和数值研究

• 批准号: 0342486
• 负责人: Bradley Baker
• 金额: $ 31.13万
• 依托单位: SPEC, Inc.
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2004
• 资助国家: 美国
• 起止时间: 2004-03-15 至 2007-02-28
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0342486&HistoricalAwards=false
• 关键词: Experimental; Numerical; Investigations; Spectral; Broadening

The "Rain in Cumulus over the Oceans" experiment will be a multi-investigator study of warm rain formation and the nature of trade wind Cumulus clouds. One hypothesis being investigated in that experiment is that turbulent air motions in clouds increase the collision rates among cloud droplets and so accelerate the formation of rain. These investigators will participate in that study by contributing measurements of the spatial inhomogeneities in droplet locations in the clouds. Using those measurements, they will evaluate the possibility that such inhomogeneities lead to faster rain formation than would be present without turbulence. Unique instruments will include a new "2D-S" (Two-Dimensional Stereo) imaging probe, an updated version of a cloud particle imager that can provide information on the spatial distribution of hydrometeors with fine resolution, and an instrument that measures the location of each droplet encountered with high resolution. These instruments promise to provide reliable measurements of quantities previously difficult to measure from aircraft, including the drizzle size range and the clustering of droplets. If they are shown to be reliable, they have the potential to contribute to many future studies of microphysical processes in clouds. The 2D-S probe in particular could make a major contribution to research objectives of all RICO investigators if it provides good documentation of the 30-200 micrometer droplet size range because this is of crucial importance to the project objectives and is poorly measured by standard instruments. The instrumentation development and testing that will occur as part of this project may benefit future measurement programs as well. Analysis efforts in subsequent years will include collaboration with modelers to represent microphysical processes in clouds in ways that are consistent with the observed characteristics.

“海洋上积云中的雨”实验将是一个多研究者对暖雨形成和信风积云性质的研究。实验中正在研究的一个假设是，云中的湍流空气运动增加了云滴之间的碰撞率，从而加速了雨的形成。这些研究人员将通过测量云中液滴位置的空间不均匀性来参与这项研究。利用这些测量结果，他们将评估这种不均匀性是否会导致比没有湍流时更快的降雨形成。独特的仪器将包括一个新的“2D-S”（二维立体）成像探头，一个更新版本的云粒子成像仪，可以提供水成物的空间分布信息，分辨率很高，还有一个仪器，可以测量遇到的每个液滴的位置，分辨率很高。这些仪器有望提供以前难以从飞机上测量的数量的可靠测量，包括毛毛雨的大小范围和液滴的聚集。如果它们被证明是可靠的，它们就有可能对云中的微物理过程的许多未来研究作出贡献。特别是2D-S探针，如果它提供30-200微米液滴尺寸范围的良好文档，则可以为所有RICO研究者的研究目标做出重大贡献，因为这对项目目标至关重要，并且很难用标准仪器测量。仪器的开发和测试将作为这个项目的一部分，也可能有利于未来的测量计划。随后几年的分析工作将包括与建模者合作，以符合观测特征的方式表示云中的微物理过程。