2019
DOI: 10.1016/j.atmosenv.2019.02.026
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Assessing the impact of Chinese FY-3/MERSI AOD data assimilation on air quality forecasts: Sand dust events in northeast China

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Cited by 16 publications
(4 citation statements)
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“…Although the DA of AOP products has been carried out in many previous studies, such bias inconsistency is seldom noticed because many similar works only validate their results against the same kind of AOP observations assimilated. When validated against the surface PM observation, the Table 4 Similar to Table 2 Journal of Geophysical Research: Atmospheres results of some works (Bao et al, 2019;Mathur, 2008;Schwartz et al, 2012) achieve an overall improvement (although similar overestimations after DA could be found sometimes) because their natural run already underestimates the surface PM concentration in total, which is similar to what occurred in the November case. Mangold et al (2011) and Liu et al (2011) were the first to note this problem.…”
Section: Cause Of the Bias Inconsistencymentioning
confidence: 54%
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“…Although the DA of AOP products has been carried out in many previous studies, such bias inconsistency is seldom noticed because many similar works only validate their results against the same kind of AOP observations assimilated. When validated against the surface PM observation, the Table 4 Similar to Table 2 Journal of Geophysical Research: Atmospheres results of some works (Bao et al, 2019;Mathur, 2008;Schwartz et al, 2012) achieve an overall improvement (although similar overestimations after DA could be found sometimes) because their natural run already underestimates the surface PM concentration in total, which is similar to what occurred in the November case. Mangold et al (2011) and Liu et al (2011) were the first to note this problem.…”
Section: Cause Of the Bias Inconsistencymentioning
confidence: 54%
“…They are usually in the form of the mixing ratio of particle mass (PM) with diameters of less than 10 μm (PM 10 ) (Jiang et al, 2013) and 2.5 μm (PM 2.5 ) (Werner et al, 2019) or the mass concentrations of specific aerosol species (Henze et al, 2009;Li et al, 2013), which mostly originate from surface monitoring sites and sometimes from aircrafts. The other category is aerosol optical properties (AOP), which usually include the aerosol optical depth (AOD) (Bao et al, 2019;Dai et al, 2014;Dai et al, 2019;Rubin et al, 2017;Saide et al, 2014), vertical profile of aerosol extinction coefficient (AEXT) (Uno et al, 2008;Zhang et al, 2011) and backscattering coefficient (Kahnert, 2008;Sekiyama et al, 2010). These observations can be obtained from spaceborne instruments such as the Moderate Resolution Imaging Spectroradiometer (MODIS) and Cloud-Aerosol Lidar with Orthogonal Polarization or from surface-based instruments such as sun photometers from the Aerosol Robotic Network (AERONET) and ground-based lidar.…”
Section: Introductionmentioning
confidence: 99%
“…For most regions in Western China, surface observation stations are still sparse. In addition, some studies also certified the importance of assimilation of the initial aerosol vertical profile (Bao et al, 2019;Ha et al, 2020;Jiang et al, 2013;. Thus, the development of satellite AOD, Lidar, and other multisource DA methods is necessary in the future.…”
Section: Conclusion and Discussionmentioning
confidence: 99%
“…Aerosol density is necessitated to compute aerosol optical parameters in the AOD forward operator and construct our tangent linear operator. The Supplement also shows the aerosol density (Table S2) that follows the data in Barnard et al (2010).…”
Section: Aerosol Complex Refractive Indexes In Gsimentioning
confidence: 99%