TY - JOUR
T1 - Emissions from the oil and gas sectors, coal mining and ruminant farming drive methane growth over the past three decades
AU - Chandra, Naveen
AU - Patra, Prabir K.
AU - Bisht, Jagat S.H.
AU - Ito, Akihiko
AU - Umezawa, Taku
AU - Saigusa, Nobuko
AU - Morimoto, Shinji
AU - Aoki, Shuji
AU - Janssens-Maenhout, Greet
AU - Fujita, Ryo
AU - Takigawa, Masayuki
AU - Watanabe, Shingo
AU - Saitoh, Naoko
AU - Canadell, Josep G.
N1 - Funding Information:
This research was conducted by the Environment Research and Technology Development Fund of the Environmental Restoration and Conservation Agency of Japan (JPMEERF20172001 and JPMEERF2018 2002); Arctic Challenge for Sustainability Project grant (JPMXD1300000000); Arctic Challenge for Sustainability II grant (JPMXD1420318865). We thank E. Dlugokencky (and colleagues at the NOAA and cooperative institutions) for providing methane data and initial discussions and B. Vaughn, J. White, and A. Rice for providing δ 13C-CH4 data.
Publisher Copyright:
© The Author(s) 2021.
PY - 2021
Y1 - 2021
N2 - Methane (CH4) is an important greenhouse gas and plays a significant role in tropospheric and stratospheric chemistry. Despite the relevance of methane (CH4) in human-induced climate change and air pollution chemistry, there is no scientific consensus on the causes of changes in its growth rates and variability over the past three decades. We use a well-validated chemistry-transport model for simulating CH4 concentration and estimation of regional CH4 emissions by inverse modeling during 1988-2016. The control simulations are conducted using seasonally varying hydroxyl (OH) concentrations and assumed no interannual variability. Using inverse modeling of atmospheric observations, emission inventories, a wetland model, and a δ 13C-CH4 box model, we show that reductions in emissions from Europe and Russia since 1988, particularly from oil-gas exploitation and enteric fermentation, led to decreased CH4 growth rates in the 1990s. This period was followed by a quasi-stationary state of CH4 in the atmosphere during the early 2000s. CH4 resumed growth from 2007, which we attribute to increases in emissions from coal mining mainly in China and the intensification of ruminant farming in tropical regions. A sensitivity simulation using interannually varying OH shows that regional emission estimates by inversion are unaffected for the mid- and high latitude areas. We show that meridional shift in CH4 emissions toward the lower latitudes and the increase in CH4 loss by hydroxyl (OH) over the tropics finely balance out, keeping the CH4 gradients between the southern hemispheric tropical and polar sites relatively unchanged during 1988-2016. The latitudinal emissions shift is confirmed using the global distributions of the total column CH4 observations via satellite remote sensing. During our analysis period, there is no evidence of emission enhancement due to climate warming, including the boreal regions. These findings highlight key sectors for effective emission reduction strategies toward climate change mitigation.
AB - Methane (CH4) is an important greenhouse gas and plays a significant role in tropospheric and stratospheric chemistry. Despite the relevance of methane (CH4) in human-induced climate change and air pollution chemistry, there is no scientific consensus on the causes of changes in its growth rates and variability over the past three decades. We use a well-validated chemistry-transport model for simulating CH4 concentration and estimation of regional CH4 emissions by inverse modeling during 1988-2016. The control simulations are conducted using seasonally varying hydroxyl (OH) concentrations and assumed no interannual variability. Using inverse modeling of atmospheric observations, emission inventories, a wetland model, and a δ 13C-CH4 box model, we show that reductions in emissions from Europe and Russia since 1988, particularly from oil-gas exploitation and enteric fermentation, led to decreased CH4 growth rates in the 1990s. This period was followed by a quasi-stationary state of CH4 in the atmosphere during the early 2000s. CH4 resumed growth from 2007, which we attribute to increases in emissions from coal mining mainly in China and the intensification of ruminant farming in tropical regions. A sensitivity simulation using interannually varying OH shows that regional emission estimates by inversion are unaffected for the mid- and high latitude areas. We show that meridional shift in CH4 emissions toward the lower latitudes and the increase in CH4 loss by hydroxyl (OH) over the tropics finely balance out, keeping the CH4 gradients between the southern hemispheric tropical and polar sites relatively unchanged during 1988-2016. The latitudinal emissions shift is confirmed using the global distributions of the total column CH4 observations via satellite remote sensing. During our analysis period, there is no evidence of emission enhancement due to climate warming, including the boreal regions. These findings highlight key sectors for effective emission reduction strategies toward climate change mitigation.
KW - Atmospheric chemistry-transport model
KW - Greenhouse gases
KW - Inversion model
KW - Methane (CH)
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U2 - 10.2151/jmsj.2021-015
DO - 10.2151/jmsj.2021-015
M3 - Article
AN - SCOPUS:85099630022
SN - 0026-1165
VL - 99
SP - 309
EP - 337
JO - Journal of the Meteorological Society of Japan
JF - Journal of the Meteorological Society of Japan
IS - 2
ER -