Spatial and temporal changes in SO2 regimes over China in the recent decade and the driving mechanism
Spatial and temporal changes in SO2 regimes over China in the recent decade and the driving mechanism
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近十年中国SO2格局时空变化及驱动机制
DOI:
10.5194/acp-18-18063-2018
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发表时间:
2018-12
影响因子:
6.3
通讯作者:
Van Roozendael Michel
中科院分区:
文献类型:
--
作者:
Wang Ting;Wang Pucai;Theys Nicolas;Tong Dan;Hendrick Francois;Zhang Qiang;Van Roozendael Michel
. The spatial and temporal changes in SO2 regimes over China during 2005 to 2016 and their associated
driving mechanism are investigated based on a state-of-the-art retrieval
dataset. Climatological SO2 exhibits pronounced seasonal and
regional variations, with higher loadings in wintertime and two prominent
maxima centered in the North China Plain and the Cheng-Yu District. In the
last decade, overall SO2 decreasing trends have been reported
nationwide, with spatially varying downward rates according to a general rule
– the higher the SO2 loading, the more significant the decrease.
However, such decline is in fact not monotonic, but instead four distinct
temporal regimes can be identified by empirical orthogonal function analysis.
After an initial rise at the beginning, SO2 in China undergoes two
sharp drops in the periods 2007–2008 and 2014–2016, amid which 5-year
moderate rebounding is sustained. Despite spatially coherent behaviors,
different mechanisms are tied to North China and South China. In North China,
the same four regimes are detected in the time series of emission that is
expected to drive the regime of atmospheric SO2, with a percentage
of explained variance amounting to 81 %. Out of total emission, those from
the industrial sector dominate SO2 variation throughout the whole
period, while the role of household emission remains uncertain. In contrast
to North China, SO2 emissions in South China exhibit a continuous
descending tendency, due to the coordinated cuts of industrial and household
emissions. As a result, the role of emissions only makes up about 45 % of
the SO2 variation, primarily owing to the decoupled pathways of
emission and atmospheric content during 2009 to 2013 when the emissions
continue to decline but atmospheric content witnesses a rebound. Unfavorable
meteorological conditions, including deficient precipitation, weaker wind
speed and increased static stability, outweigh the effect of decreasing
emissions and thus give rise to the rebound of SO2 during 2009
to 2013.
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影响因子:
3.8
作者:
Yan Zhang;Can Li;N. Krotkov;J. Joiner;V. Fioletov;C. McLinden
通讯作者:
Yan Zhang;Can Li;N. Krotkov;J. Joiner;V. Fioletov;C. McLinden
影响因子:
--
作者:
M. Rix;P. Valks;N. Hao;D. Loyola;H. Schlager;H. Huntrieser;J. Flemming;U. Koehler;U. Schumann;A. Inness
通讯作者:
M. Rix;P. Valks;N. Hao;D. Loyola;H. Schlager;H. Huntrieser;J. Flemming;U. Koehler;U. Schumann;A. Inness
DOI:
--
发表时间:
2009
期刊:
Climatic and Environmental Research
影响因子:
--
作者:
Xiao-yan Meng
通讯作者:
Xiao-yan Meng
影响因子:
4.4
作者:
Theys, N.;De Smedt, I.;Van Roozendael, M.
通讯作者:
Van Roozendael, M.
DOI:
10.1007/978-981-10-5657-4_2
发表时间:
2017-01-01
期刊:
AMBIENT AIR POLLUTION AND HEALTH IMPACT IN CHINA
影响因子:
--
作者:
Ren, Lihong;Yang, Wen;Bai, Zhipeng
通讯作者:
Bai, Zhipeng