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李力, 张蓬勃, 戴竹君, 周文君, 陆晓波. 利用微波辐射计对南京2013年12月霾天大气温湿结构的探测分析[J]. 气候与环境研究, 2016, 21(1): 8-16. DOI: 10.3878/j.issn.1006-9585.2015.15002
引用本文: 李力, 张蓬勃, 戴竹君, 周文君, 陆晓波. 利用微波辐射计对南京2013年12月霾天大气温湿结构的探测分析[J]. 气候与环境研究, 2016, 21(1): 8-16. DOI: 10.3878/j.issn.1006-9585.2015.15002
LI Li, ZHANG Pengbo, DAI Zhujun, ZHOU Wenjun, LU Xiaobo. Using Microwave Radiometer Data to Detect and Analyze the Atmospheric Temperature and Moisture Structure of the Haze Weather of Nanjing in December 2013[J]. Climatic and Environmental Research, 2016, 21(1): 8-16. DOI: 10.3878/j.issn.1006-9585.2015.15002
Citation: LI Li, ZHANG Pengbo, DAI Zhujun, ZHOU Wenjun, LU Xiaobo. Using Microwave Radiometer Data to Detect and Analyze the Atmospheric Temperature and Moisture Structure of the Haze Weather of Nanjing in December 2013[J]. Climatic and Environmental Research, 2016, 21(1): 8-16. DOI: 10.3878/j.issn.1006-9585.2015.15002

利用微波辐射计对南京2013年12月霾天大气温湿结构的探测分析

Using Microwave Radiometer Data to Detect and Analyze the Atmospheric Temperature and Moisture Structure of the Haze Weather of Nanjing in December 2013

  • 摘要: 利用高时间分辨率的微波辐射计数据分析南京逆温层结构与雾霾天气的关系。首先将南京MP-3000A型地基微波辐射计2013年12月的数据与常规探空资料的温度和相对湿度进行对比,以确定微波辐射计数据的可用性,结果表明:微波辐射计反演的气温与常规探空资料十分接近,而相对湿度的效果则差了很多。再利用微波辐射计对南京市2013年12月的霾天气过程进行分析,发现在受秸秆焚烧的影响阶段(12月1~9日),污染物浓度与逆温层没有明显的相关;在没有秸秆焚烧影响阶段(12月10~31日),污染物浓度变化与逆温层厚度、强度呈显著的滞后正相关,和底高有显著的滞后负相关;定量化分析表明重度污染和中度污染对应的逆温层阈值一致,轻度污染对应的逆温层阈值明显较小。

     

    Abstract: Using microwave radiometer data, which has a high temporal resolution, to analyze the relationship between the structure of the inversion layer and haze in Nanjing. First, in order to confirm the availability of microwave radiometer data, we compare the temperature and relative humidity data of the MP-3000A ground-based microwave radiometer in December 2013 with that of sounding data. The results show the temperature based on the microwave radiometer to be very close to that of the sounding, but their relative humidity values to differ greatly. Analyzing the haze in December 2013 with the data of the microwave radiometer, it is found that, due to the impact of straw burning (1-9 December), there is no significant correlation between pollutants and the inversion layer. However, in periods of no straw burning (10-31 December), there is a significant positive lag correlation between pollutant variation and the thickness and strength of the inversion layer, and a negative lag correlation between pollutants and the height of the bottom of the inversion layer. Through quantitative analysis, we reveal that the thresholds of inversion layers corresponding to heavy pollution are the same as with moderate pollution, while the thresholds of inversion layers corresponding to light pollution are weaker.

     

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