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CEDAR: Ground-Based Optical Imaging of Sporadic Sodium Clouds Near the Summer Mesopause, Using Resonantly Scattered Sunlight

CEDAR：利用共振散射阳光对夏季中层顶附近的零星钠云进行地基光学成像

基本信息

批准号：
0122995
负责人：
Richard Collins
金额：
$ 18.15万
依托单位：
University of Alaska Fairbanks Campus
依托单位国家：
美国
项目类别：
Continuing Grant
财政年份：
2002
资助国家：
美国
起止时间：
2002-02-15 至 2005-08-31
项目状态：
已结题

来源：
https://www.nsf.gov/awardsearch/showAward?AWD_ID=0122995&HistoricalAwards=false
关键词：
CEDAR Ground Based Optical Imaging

项目摘要

The investigators will develop a new method to obtain two-dimensional images of sporadic clouds of mesospheric sodium. These images will be constructed by combining data from a sodium lidar and an optical spectrometer obtained during arctic summer months. The project involves minor modifications to existing instruments at Poker Flat, Alaska, and the development of analysis and calibration software to perform the two-dimensional imaging with high reliability. The mesopause region hosts persistent layers of neutral and ionized metallic atoms that are replenished by the ablation of meteors. These metal layers can be used as tracers of the thermal, chemical, and dynamical conditions near the mesopause. Although the altitude distribution of these layers have been studied using various techniques, the horizontal structure of the layers remains unknown. This investigation aims to observe the two-dimensional structure of metallic layers using the sun to illuminate sodium atoms, and sensitive instrumentation to detect the scattered sunlight. The simultaneous lidar measurements will provide information about the altitude distribution of the layers. Various models have shown that the temperature structure in the mesopause may be a sensitive indicator of global change. Understanding the distribution of sporadic layers in the mesosphere is important in studying processes that heat and cool the middle atmosphere.

研究人员将开发一种新的方法来获得中间层钠散发性云的二维图像。这些图像将通过结合在北极夏季获得的钠激光雷达和光谱仪的数据来构建。该项目涉及对阿拉斯加Poker Flat现有仪器进行微小修改，并开发分析和校准软件，以高可靠性执行二维成像。中间层顶区域拥有中性和电离金属原子的持久层，这些金属原子通过流星的消融得到补充。这些金属层可以用作中层顶附近热、化学和动力条件的示踪剂。尽管已经使用各种技术研究了这些层的高度分布，但这些层的水平结构仍然未知。本研究旨在利用太阳照射钠原子来观察金属层的二维结构，并利用灵敏的仪器来探测散射的阳光。同时进行的激光雷达测量将提供有关各层高度分布的信息。各种模式表明，中层顶的温度结构可能是全球变化的一个敏感指标。了解中间层中零星层的分布对于研究中间大气的冷热过程是很重要的。