大气与环境光学学报 ›› 2021, Vol. 16 ›› Issue (5): 404-414.

• 大气光学 • 上一篇    下一篇

全天空红外云探测在航空气象中的应用

王本革1, 杨 明1∗, 凌新锋2, 吴佳玲3   

  1. 1 中国民用航空华东地区空中交通管理局安徽分局, 安徽 合肥 230001; 2 寿县气象局, 安徽 淮南 232000; 3 中国科学院合肥物质科学研究院安徽光学精密机械研究所光电子技术研究中心, 安徽 合肥 230031
  • 收稿日期:2020-09-30 修回日期:2021-08-26 出版日期:2021-09-28 发布日期:2021-09-28
  • 通讯作者: E-mail: yangriyue@126.com E-mail:E-mail: yangriyue@126.com
  • 作者简介:王本革 (1967 - ), 安徽合肥人, 工程师, 主要从事航空气象探测和信息化技术研究。 E-mail: 13866107557@139.com
  • 基金资助:
    Supported by Major Scientific and Technological Projects in Anhui Province (安徽省科技重大专项, 18030901013), Key Research and Development Projects in Anhui Province and Science and Technology (安徽省重点研究和开发计划项目, 201904b11020031), Project of Anhui Air Traffic Control Branch of Civil Aviation (民航安徽空管分局科技项目, F2019-04)

Application of All-Sky Infrared Cloud Observation in Aviation Meteorology

WANG Benge1, YANG Ming1∗, LING Xinfeng2, WU Jialing3   

  1. 1 Anhui Branch of East China Air Traffic Administration of Civil Aviation of China, Hefei 230001, China; 2 Shouxian Meteorological Bureau, Huainan 232000, China; 3 Opto-Electronics Technology Research Centre, Anhui Institute of Optics and Fine Mechanics, HFIPS, Chinese Academy of Sciences, Hefei 230031, China
  • Received:2020-09-30 Revised:2021-08-26 Published:2021-09-28 Online:2021-09-28

摘要: 利用合肥新桥机场温湿度、云高、能见度以及全天空云图仪数据资料, 分析了 2019 年 7 月至 2020 年 4 月机 场上空各类云的红外特征以及云、雾演变规律。结果表明: (1) 在云判别上, 云底高度越高, 红外云图上表现亮度越暗, 反之亦然。且不同类型的云具有各自独有的红外特征。 (2) 不同高度的波状云最大云块平均最短直径表现为层积云云 块是高积云的 2∼4 倍, 高积云是卷积云的 2∼4 倍。碎层云主要呈现出团状, 具有蓬松棉花状结构; 而碎雨云相对破碎, 一般为烟带状或散片状。 (3) 云与雾有明确的转化过程。辐射雾一般发生在云层刚散开期间, 天空至少一半为晴空的 时段, 且雾逐步抬升为云, 并持续消散。当天空形成不均匀缺口, 表明雾开始消散, 其可作为能见度迅速回升的一个重 要指标。非对流降水云层演变呈现出云高由高到低, 云层由分散纹理状变为均匀层状, 降水前期均会出现“均匀层状”, 地面相对湿度呈现出陡增现象。

关键词: 红外探测, 航空气象, 云图识别, 云演变

Abstract: Based on the data of temperature, humidity, cloud height, visibility and all-sky view imaging from the automatic meteorological system of Hefei Xinqiao Airport, China, the infrared characteristics of all kinds of clouds as well as the evolution of clouds and fog over the airport from July 2019 to April 2020, are analyzed. The results show that: (1) the higher the cloud bottom height is, the lower the temperature is, which means that the higher clouds have the weaker thermal radiation resulting in the darker infrared cloud image, and vice versa. And different types of clouds have their own unique infrared characteristics. (2) As for the average shortest diameter of the largest cloud block of wave clouds at various heights, that of stratocumulus is 2–4 times that of altocumulus, and that of altocumulus is 2–4 times that of cirrocumulus. Generally, fractostratus shows fluffy-cotton alike structures, while fractonimbus are usually in the form of smoke band or scattered sheet. (3) There is a clear transformation process between cloud and fog. Radiation fog generally occurs during the period when clouds just disperse and at least half of the sky is clear, and the fog gradually rises to clouds and continues to dissipate. When a breach is formed in the sky, it indicates that the fog begins to dissipate, which can be used as an important indicator for the rapid recovery of visibility. The evolution of the non-convective precipitation cloud layer shows that the cloud base height changes from high to low, and the cloud layer changes from dispersed texture to uniform layer at the same time. The uniform cloud layer always appears in the early stage of the precipitation, and the relative humidity of ground presents a sharp increase.

Key words: infrared detection, aviation meteorology, cloud image recognition, cloud evolution

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