TY - JOUR
T1 - Estimation of CH4 emissions from the East Siberian Arctic Shelf based on atmospheric observations aboard the R/V Mirai during fall cruises from 2012 to 2017
AU - Tohjima, Yasunori
AU - Zeng, Jiye
AU - Shirai, Tomoko
AU - Niwa, Yosuke
AU - Ishidoya, Shigeyuki
AU - Taketani, Fumikazu
AU - Sasano, Daisuke
AU - Kosugi, Naohiro
AU - Kameyama, Sohiko
AU - Takashima, Hisahiro
AU - Nara, Hideki
AU - Morimoto, Shinji
N1 - Funding Information:
This study was financially supported by the GRENE Arctic Climate Change Research Project and Arctic Challenge for Sustainability (ArCS) Project from the Ministry of Education, Culture, Sports, Science, and Technology (MEXT) in Japan . The CH 4 inverse analysis of NICAM-TM 4D-Var was conducted under the project of the Environment Research and Technology Development Fund ( 2–1701 ) of the Ministry of the Environment, Japan .
Funding Information:
To investigate the present state of the Arctic environment and climate, observational cruises aboard the R/V Mirai were conducted every year from 2012 to 2015 as a part of the GRENE (Green Network of Excellence) Arctic Climate Change Research Project and during 2016–2018 as a part of the ArCS (Arctic Challenge for Sustainability) Arctic Region Research Project, both funded by the Ministry of Education, Culture, Sports, Science and Technology-Japan (MEXT). In general, more than 20 days of the entire observational duration of 40–50 days were allocated for the cruises in the Arctic Ocean centered on September, except the cruise in 2018 (cruise ID: MR18-05C), which was conducted mostly in November. The cruise routes of the R/V Mirai in the Arctic Ocean were limited to the area between 182.5°E and 209°E (177.5°W and 151°W) and south of 76.5°N, including the Bering Strait, the Chukchi Sea, and the Beaufort Sea (see Fig. 1 . The individual cruise routes are shown in Fig. A1 in Appendix A ). The cruise IDs, the observation periods, the research areas, and the range of the observed CH 4 variations are summarized in Table 1 . Note that hereinafter we use the first four characters of the cruise ID (e.g., MR12) to designate the individual cruise.
Publisher Copyright:
© 2020 The Authors
PY - 2021/3
Y1 - 2021/3
N2 - Atmospheric CH4 mole fractions were observed aboard the R/V Mirai sailing in waters off Alaska in the Arctic Ocean in September 2012–2017 to investigate the CH4 emissions from the surrounding region, especially from the East Siberian Arctic Shelf (ESAS). The synoptic-scale increases of CH4 were compared with simulated increases based on a Lagrangian Particle Dispersion Model and monthly CH4 flux maps determined by a global atmospheric inversion system. There were good agreements between the observed and simulated CH4 increases, suggesting the validity of CH4 fluxes from the surrounding areas of the cruise experiments. The CH4 emissions from the ESAS in September were further optimized in order to minimize the root mean square of the differences between the observed and simulated CH4 increases. The average (±1σ) of the resulting emission rates was 0.58 ± 0.47 TgCH4 yr−1, which was much smaller than previously reported estimates. The individual optimized CH4 emissions varied from −0.1 ± 0.3 to 1.3 ± 0.4 TgCH4 yr−1, showing a positive correlation with the sea surface temperature and a negative correlation with the ice concentration of the ESAS area in September. These results suggest a possible enhancement of the CH4 emissions from the ESAS in a warmer future.
AB - Atmospheric CH4 mole fractions were observed aboard the R/V Mirai sailing in waters off Alaska in the Arctic Ocean in September 2012–2017 to investigate the CH4 emissions from the surrounding region, especially from the East Siberian Arctic Shelf (ESAS). The synoptic-scale increases of CH4 were compared with simulated increases based on a Lagrangian Particle Dispersion Model and monthly CH4 flux maps determined by a global atmospheric inversion system. There were good agreements between the observed and simulated CH4 increases, suggesting the validity of CH4 fluxes from the surrounding areas of the cruise experiments. The CH4 emissions from the ESAS in September were further optimized in order to minimize the root mean square of the differences between the observed and simulated CH4 increases. The average (±1σ) of the resulting emission rates was 0.58 ± 0.47 TgCH4 yr−1, which was much smaller than previously reported estimates. The individual optimized CH4 emissions varied from −0.1 ± 0.3 to 1.3 ± 0.4 TgCH4 yr−1, showing a positive correlation with the sea surface temperature and a negative correlation with the ice concentration of the ESAS area in September. These results suggest a possible enhancement of the CH4 emissions from the ESAS in a warmer future.
KW - Atmospheric CH
KW - Cavity ring-down spectroscopy (CRDS)
KW - East Siberian Arctic Shelf (ESAS)
KW - Shipboard measurement
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U2 - 10.1016/j.polar.2020.100571
DO - 10.1016/j.polar.2020.100571
M3 - Article
AN - SCOPUS:85090301742
SN - 1873-9652
VL - 27
JO - Polar Science
JF - Polar Science
M1 - 100571
ER -