Validation of JAXA Himawari-8 Aerosol Optical Depth Products over China with AERONET and CARSNET Observations
- 1China Meteorological Administration, National Satellite Meteorological Center, beijing, China (gaoling@cma.gov.cn)
- 2Laboratory for Climate and Ocean-Atmosphere Studies, Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing , China(ccli@pku.edu.cn)
- 3Cooperative Institute for Meteorological Satellite Studies, University of Wisconsin–Madison, Madison, WI , USA(Jun.Li@ssec.wisc.edu)
- 4Chinese Academy of Meteorological Sciences, China Meteorological Administration, Beijing , China(chehz@camscma.cn)
The performance of JAXA Himawari-8 Advanced Himawari Imager (AHI) aerosol optical depth (AOD) products over China is evaluated with ground-based AErosol RObotic NETwork (AERONET) and Sun-Sky Radiometer Observation Network (CARSNET) observations as well as the Moderate Resolution Imaging Spectroradiometer (MODIS) AOD products. Considering the quality and quantity of valid data, the study was limited to AOD products from AHI with a Quality Assurance Flag (QA_Flag) of “good” and “very good.” The spatial distribution of the AHI AOD product is similar to that of the MODIS AOD product. The AOD correlation between AHI and MODIS is better in the morning than in the afternoon after March, however, using MODIS AOD as a reference resulted in underestimation in the morning and overestimation in the afternoon. The bias is also larger in spring and autumn than in summer and winter. Validation with sun-photometer observations indicates good correlation between AHI AOD and ground-based observations with correlation coefficients larger than 0.75 (N>1000) when barren and sparsely vegetated surfaces are excluded. At 02:30 UTC, 53% of the collocated AHI AOD observations fall in the expected error (EE) range and at 5:30 UTC, 59.3% fall above the EE. The AHI AOD overestimation was apparent at the Northern China stations in April and after October, whereas the underestimation was apparent in southern China throughout the year. The temporal variations of AHI and AERONET AOD also show that the overestimation occurred in the afternoon and underestimation occurred in the morning.
The assumption that the solar geometries were nearly identical and the surface reflectance unchanged for a month causes the surface reflectance underestimation and leads to the AOD overestimation for barren surfaces in autumn and winter. Because background aerosols were neglected, the surface reflectance was overestimated, leading to AOD underestimation in vegetated surfaces.
Overall, the JAXA AOD provides a reliable and high temporal resolution aerosol product for environmental and climate research and the aerosol retrieval algorithm requires improvement.
How to cite: Gao, L., Li, C., Chen, L., Li, J., and Che, H.: Validation of JAXA Himawari-8 Aerosol Optical Depth Products over China with AERONET and CARSNET Observations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18695, https://doi.org/10.5194/egusphere-egu2020-18695, 2020
