2021
DOI: 10.1016/j.rse.2020.112221
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A High-Precision Aerosol Retrieval Algorithm (HiPARA) for Advanced Himawari Imager (AHI) data: Development and verification

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Cited by 78 publications
(19 citation statements)
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“…Commonly, the aerosol radiative feedback and properties are studied using observational in-situ and satellite data [28][29][30] as well as atmospheric dispersion models [31,32]. The usage of atmospheric dispersion models allows a separation of local and LTD components of air pollutants but has rarely been conducted on bioaerosols (pollen).…”
Section: Introductionmentioning
confidence: 99%
“…Commonly, the aerosol radiative feedback and properties are studied using observational in-situ and satellite data [28][29][30] as well as atmospheric dispersion models [31,32]. The usage of atmospheric dispersion models allows a separation of local and LTD components of air pollutants but has rarely been conducted on bioaerosols (pollen).…”
Section: Introductionmentioning
confidence: 99%
“…With the comparison between Himawari-8 IBAA and other AHI algorithms in previous papers, such as different improved DT algorithms (R = 0.86 and RMSE = 0.12 in [21], 2018; R = 0.9 and RMSE = 0.15 in [22]; R > 0.8 in [23]), an improved time-series algorithm (R > 0.8 and RMSE < 0.2 in [59]), the OE method (R = 0.88, RMSE = 0.17 and 69.9% of retrievals falling within EE = ±(0.05 + 0.2 × AOD AERONET ) in [24]), and the monthly spectral base reflectance ratio library method (R = 0.939, RMSE = 0.113 and 82.5% of retrievals falling within EE = ±(0.05 + 0.2 × AOD AERONET in [25]), the IBAA algorithm has certain precision and a simple process. Due to different time range and regions and different ground-based station observation selected for algorithm validation applied in the above papers, there are great uncertainties in such comparisons.…”
Section: Discussionmentioning
confidence: 99%
“…R is the correlation coefficient and RMSE is the root-mean-square error, MD is the mean difference and represents the average value of all AERONET-matched AOD minus AHI AOD. EE is the expected error of ±(0.05 + 0.2 × AOD AERONET ) according to other studies [24,25]. WEE is the percentage of points falling within the EE envelope and UpEE and LowEE are above and below EE envelope.…”
mentioning
confidence: 95%
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“…Limited to point locations, ground-based instruments can only support research at the local scale. Satellite sensors such as Moderate Resolution Imaging Spectroradiometer (MODIS), Advanced Himawari Imager (AHI), Ozone Monitoring Instrument (OMI), and Multi-angle Imaging Spectroradiometer (MISR) can provide continuous spatial aerosol property observations, which greatly aid the research of the aerosol effect on the global atmospheric environment and air quality, especially in areas with heavy aerosol loads (e.g., the Indo-Gangetic Plains [IGP] and the North China Plain [NCP]) [13][14][15][16][17][18][19]. However, there are evident differences in the accuracy and applicability of each satellite aerosol product owing to the different retrieval algorithms and spatiotemporal resolutions.…”
Section: Introductionmentioning
confidence: 99%