Spatial and seasonal variations of aerosols over China from two decades of multi-satellite observations – Part 2: AOD time series for 1995–2017 combined from ATSR ADV and MODIS C6.1 and AOD tendency estimations
Authors: Sogacheva Larisa , Rodriguez Edith , Kolmonen Pekka , Virtanen Timo H. , Saponaro Giulia , de Leeuw Gerrit , Georgoulias Aristeidis K. , Alexandri Georgia , Kourtidis Konstantinos , van der A Ronald J. 
Published: November 2018

Abstract. Understanding long-term variations in aerosol loading is
essential for evaluating the health and climate effects of airborne
particulates as well as the effectiveness of pollution control policies.
The expected satellite lifetime is about 10 to 15 years. Therefore, to study the
variations of atmospheric constituents over longer periods information
from different satellites must be utilized. Here we introduce a method to construct a combined annual and seasonal long
time series of AOD at 550 nm using the Along-Track Scanning Radiometers
(ATSR: ATSR-2 and AATSR combined) and the MODerate resolution Imaging
Spectroradiometer on Terra (MODIS/Terra), which together cover the 1995–2017 period. The
long-term (1995–2017) combined AOD time series are presented for all of
mainland China, for southeastern (SE) China and for 10 selected regions in
China. Linear regression was applied to the combined AOD time series
constructed for individual L3 (1∘ × 1∘) pixels to
estimate the AOD tendencies for two periods: 1995–2006 (P1) and 2011–2017
(P2), with respect to the changes in the emission reduction policies in China. During P1, the annually averaged AOD increased by 0.006 (or 2 % of the
AOD averaged over the corresponding period) per year across all of mainland
China, reflecting increasing emissions due to rapid economic development. In
SE China, the annual AOD positive tendency in 1995–2006 was 0.014 (3 %)
per year, reaching maxima (0.020, or 4 %, per year) in Shanghai and the
Pearl River Delta regions. After 2011, during P2, AOD tendencies reversed
across most of China with the annually averaged AOD decreasing by −0.015 (−6 %)
per year in response to the effective reduction of the anthropogenic emissions of
primary aerosols, SO2 and NOx. The strongest AOD decreases were observed
in the Chengdu (−0.045, or −8 %, per year) and Zhengzhou (−0.046, or
−9 %, per year) areas, while over the North China Plain and coastal areas
the AOD decrease was lower than −0.03 (approximately −6 %) per year. In
the less populated areas the AOD decrease was small. The AOD tendency varied by both season and region. The increase in the
annually averaged AOD during P1 was mainly due to an increase in summer and
autumn in SE China (0.020, or 4 %, and 0.016, or 4 %, per year,
respectively), while during winter and spring the AOD actually decreased
over most of China. The AOD negative tendencies during the
2011–2017 period were larger in summer than in other seasons over the whole of China
(ca. −0.021, or −7 %, per year) and over SE China (ca. −0.048, or −9 %, per year). The long-term AOD variations presented here show a gradual decrease in the
AOD after 2011 with an average reduction of 30 %–50 % between 2011 and
2017. The effect is more visible in the highly populated and industrialized
regions in SE China, as expected.