Economic globalization and concomitant growth in international trade since the late 1990s have profoundly reorganized global production activities and related CO2 emissions. Here we show trade among developing nations (i.e., South–South trade) has more than doubled between 2004 and 2011, which reflects a new phase of globalization. Some production activities are relocating from China and India to other developing countries, particularly raw materials and intermediate goods production in energy-intensive sectors. In turn, the growth of CO2 emissions embodied in Chinese exports has slowed or reversed, while the emissions embodied in exports from less-developed regions such as Vietnam and Bangladesh have surged. Although China’s emissions may be peaking, ever more complex supply chains are distributing energy-intensive industries and their CO2 emissions throughout the global South. This trend may seriously undermine international efforts to reduce global emissions that increasingly rely on rallying voluntary contributions of more, smaller, and less-developed nations.
Abstract. Total gaseous mercury (TGM) concentrations were continuously measured at Nam
Co Station, a remote high-altitude site (4730 m a.s.l.), on the inland
Tibetan Plateau, China, from January 2012 to October 2014 using a Tekran
2537B instrument. The mean concentration of TGM during the entire monitoring
period was 1.33±0.24 ng m−3 (mean ± standard deviation),
ranking it as the lowest value among all continuous TGM measurements reported
in China; it was also lower than most of sites in the Northern Hemisphere.
This indicated the pristine atmospheric environment on the inland Tibetan
Plateau. Long-term TGM at the Nam Co Station exhibited a slight decrease
especially for summer seasons. The seasonal variation of TGM was
characterized by higher concentrations during warm seasons and lower
concentrations during cold seasons, decreasing in the following order: summer
(1.50±0.20 ng m−3) > spring
(1.28±0.20 ng m−3) > autumn
(1.22±0.17 ng m−3) > winter (1.14±0.18 ng m−3).
Diurnal variations of TGM exhibited uniform patterns in different seasons:
the daily maximum was reached in the morning (around 2–4 h after sunrise),
followed by a decrease until sunset and a subsequent buildup at night,
especially in the summer and the spring. Regional surface reemission and
vertical mixing were two major contributors to the temporal variations of TGM
while long-range transported atmospheric mercury promoted elevated TGM during
warm seasons. Results of multiple linear regression (MLR) revealed that
humidity and temperature were the principal covariates of TGM. Potential
source contribution function (PSCF) and FLEXible PARTicle dispersion model
(WRF-FLEXPART) results indicated that the likely high potential source
regions of TGM to Nam Co were central and eastern areas of the Indo-Gangetic
Plain (IGP) during the measurement period with high biomass burning and
anthropogenic emissions. The seasonality of TGM at Nam Co was in phase with
the Indian monsoon index, implying the Indian summer monsoon as an important
driver for the transboundary transport of air pollution onto the inland
Tibetan Plateau. Our results provided an atmospheric mercury baseline on the
remote inland Tibetan Plateau and serve as new constraint for the assessment
of Asian mercury emission and pollution.
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