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Study on aerosol optical depth retrieval over land from Himawari-8 data based on dark target method

  • role： First author第一作者
  • Affiliation：

    School of Surveying and Land Information Engineering, Henan Polytechnic University, Jiaozuo 454003, China

    State Environmental Protection Key Laboratory of Satellite Remote Sensing, Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences, Beijing 100101, China

  • Email：geby2015@163.com
  • Introduction：葛邦宇(1989—　)，男，硕士研究生，研究方向为气溶胶卫星遥感反演。E-mail：geby2015@163.com
Bangyu GE12,  
  • role： Corresponding author通信作者
  • Affiliation：

    School of Surveying and Land Information Engineering, Henan Polytechnic University, Jiaozuo 454003, China

  • Email：leiku.yang@foxmail.com
  • Introduction：杨磊库(1980—　)，男，副教授，研究方向为气溶胶卫星遥感反演。E-mail：leiku.yang@foxmail.com
Leiku YANG1*,  
  • Affiliation：

    State Environmental Protection Key Laboratory of Satellite Remote Sensing, Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences, Beijing 100101, China

Xingfeng CHEN2,  
  • Affiliation：

    State Environmental Protection Key Laboratory of Satellite Remote Sensing, Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences, Beijing 100101, China

Zhengqiang LI2,  
  • Affiliation：

    College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China

Xiaodong MEI3,  
  • Affiliation：

    China Centre for Resources Satellite Data and Application, Beijing 100094, China

Li LIU4

résumé

Himawari-8 (H8), as a new generation of geostationary meteorological satellites that observes full-disk images (images of the Earth as seen from the satellite) per 10 min, was launched by Japan Meteorological Agency to investigate aerosol characteristics. The Advanced Himawari Imager (AHI) onboard Himawari-8 has similar spectral bands with Moderate Resolution Imaging Spectroradiometer (MODIS). This study applies the Dark Target (DT) method for Aerosol Optical Depth (AOD) retrieval from AHI data. The atmospheric effect is established for the AHI data over AErosol RObotic NETwork sites. The ratio of surface reflectance between the shortwave infrared and visible bands is then obtained. This ratio serves as a priori knowledge for the surface reflectance estimation in the atmosphere-surface coupling model. Assuming that the aerosol type is continental, we build a look-up table through the radiative transfer model. With the retrieval algorithm, the AOD is determined in the case of a minimum difference between simulated apparent reflectance and satellite observations. The algorithm was used to retrieve AOD over the Beijing-Tianjing-Hebei area of China in May 2016. H8 AOD products were compared with MODIS products, and the results revealed a good spatial coincidence, with the correlation coefficientR being 0.852. The H8 AOD products were validated with AERONET observations, and they showed good linear relations, with the correlation coefficient R2 being better than 0.88. The high temporal resolution products were used to analyze aerosol spatial distribution and diurnal variation in the Beijing-Tianjin-Hebei region. Results show that H8 AOD retrieval based on the DT method has certain feasibility and potential. AOD products can express the high temporal variation of aerosol and are thus potentially useful in atmospheric environmental pollution monitoring.

mots-clés

Himawari-8;dark target method;surface reflectance;aerosol optical depth;Beijing-Tianjin-Hebei area

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