Abstract. Aerosols are complex compounds that greatly affect the global radiation
balance and climate system and even human health; in addition, aerosols are
currently a large source of uncertainty in the numerical simulation process.
The arid and semi-arid areas have fragile ecosystems with abundant dust but
lack related high-accuracy aerosol data. To solve these problems, we use the
bagging trees ensemble model, based on 1 km aerosol optical depth (AOD) data
and multiple environmental covariates, to produce a monthly
advanced-performance, full-coverage, and high-resolution (250 m) AOD product
(named FEC AOD, fusing environmental covariates AOD) covering the arid and
semi-arid areas. Then, based on the FEC AOD products, we analyzed the
spatiotemporal AOD pattern and further discussed the interpretation of
environmental covariates to AOD. The results show that the bagging trees
ensemble model has a good performance, with its verification
R2 values always remaining at 0.90 and the R2 being 0.79 for FEC AOD
compared with AERONET AOD product. The high-AOD areas are located in the
Taklimakan Desert and on the Loess Plateau, and the low-AOD areas are
concentrated in southern Qinghai province. The higher the AOD, the
stronger the interannual variability. Interestingly, the AOD reflected a
dramatic decrease on the Loess Plateau and an evident increase in the
south-eastern Taklimakan Desert, while the southern Qinghai province AODs
showed almost no significant change between 2000 and 2019. The annual
variation characteristics show that the AOD was largest in spring (0.267±0.200) and smallest in autumn (0.147±0.089); the annual AOD
variation pattern showed different features, with two peaks in March and
August over Gansu province but only one peak in April in other
provinces/autonomous regions. Farmlands and construction lands have high AOD
levels compared to other land cover types. Meteorological factors
demonstrate the maximum interpretation ability of the AODs on all set
temporal scales, followed by the terrain factors, while surface properties
have the smallest explanatory abilities; the corresponding average
contributions are 77.1 %, 59.1 %, and 50.4 %, respectively. The
capability of the environmental covariates to explain the AOD varies
seasonally in the following sequence: winter (86.6 %) > autumn
(80.8 %) > spring (79.9 %) > summer (72.5 %). In
this research, we provide a pathbreaking high spatial resolution (250 m)
and long time series (2000–2019) FEC AOD dataset covering arid and semi-arid
regions to support atmospheric and related studies in northwest China; the
full dataset is available at https://doi.org/10.5281/zenodo.5727119 (Chen et
al., 2021b).