Near-real-time estimation of fossil fuel CO2 emissions from China based on atmospheric observations on Hateruma and Yonaguni Islands, Japan

Abstract We developed a near-real-time estimation method for temporal changes in fossil fuel CO2 (FFCO2) emissions from China for 3 months [January, February, March (JFM)] based on atmospheric CO2 and CH4 observations on Hateruma Island (HAT, 24.06° N, 123.81° E) and Yonaguni Island (YON, 24.47° N,...

Full description

Bibliographic Details
Main Authors: Yasunori Tohjima, Yosuke Niwa, Prabir K. Patra, Hitoshi Mukai, Toshinobu Machida, Motoki Sasakawa, Kazuhiro Tsuboi, Kazuyuki Saito, Akihiko Ito
Format: Article
Language:English
Published: SpringerOpen 2023-03-01
Series:Progress in Earth and Planetary Science
Subjects:
Online Access:https://doi.org/10.1186/s40645-023-00542-6
_version_ 1797863210193256448
author Yasunori Tohjima
Yosuke Niwa
Prabir K. Patra
Hitoshi Mukai
Toshinobu Machida
Motoki Sasakawa
Kazuhiro Tsuboi
Kazuyuki Saito
Akihiko Ito
author_facet Yasunori Tohjima
Yosuke Niwa
Prabir K. Patra
Hitoshi Mukai
Toshinobu Machida
Motoki Sasakawa
Kazuhiro Tsuboi
Kazuyuki Saito
Akihiko Ito
author_sort Yasunori Tohjima
collection DOAJ
description Abstract We developed a near-real-time estimation method for temporal changes in fossil fuel CO2 (FFCO2) emissions from China for 3 months [January, February, March (JFM)] based on atmospheric CO2 and CH4 observations on Hateruma Island (HAT, 24.06° N, 123.81° E) and Yonaguni Island (YON, 24.47° N, 123.01° E), Japan. These two remote islands are in the downwind region of continental East Asia during winter because of the East Asian monsoon. Previous studies have revealed that monthly averages of synoptic-scale variability ratios of atmospheric CO2 and CH4 (ΔCO2/ΔCH4) observed at HAT and YON in JFM are sensitive to changes in continental emissions. From the analysis based on an atmospheric transport model with all components of CO2 and CH4 fluxes, we found that the ΔCO2/ΔCH4 ratio was linearly related to the FFCO2/CH4 emission ratio in China because calculating the variability ratio canceled out the transport influences. Using the simulated linear relationship, we converted the observed ΔCO2/ΔCH4 ratios into FFCO2/CH4 emission ratios in China. The change rates of the emission ratios for 2020–2022 were calculated relative to those for the preceding 9-year period (2011–2019), during which relatively stable ΔCO2/ΔCH4 ratios were observed. These changes in the emission ratios can be read as FFCO2 emission changes under the assumption of no interannual variations in CH4 emissions and biospheric CO2 fluxes for JFM. The resulting average changes in the FFCO2 emissions in January, February, and March 2020 were 17 ± 8%, − 36 ± 7%, and − 12 ± 8%, respectively, (− 10 ± 9% for JFM overall) relative to 2011–2019. These results were generally consistent with previous estimates. The emission changes for January, February, and March were 18 ± 8%, − 2 ± 10%, and 29 ± 12%, respectively, in 2021 (15 ± 10% for JFM overall) and 20 ± 9%, − 3 ± 10%, and − 10 ± 9%, respectively, in 2022 (2 ± 9% for JFM overall). These results suggest that the FFCO2 emissions from China rebounded to the normal level or set a new high record in early 2021 after a reduction during the COVID-19 lockdown. In addition, the estimated reduction in March 2022 might be attributed to the influence of a new wave of COVID-19 infections in Shanghai.
first_indexed 2024-04-09T22:33:01Z
format Article
id doaj.art-924148883c2f431fbcf788304e8ad703
institution Directory Open Access Journal
issn 2197-4284
language English
last_indexed 2024-04-09T22:33:01Z
publishDate 2023-03-01
publisher SpringerOpen
record_format Article
series Progress in Earth and Planetary Science
spelling doaj.art-924148883c2f431fbcf788304e8ad7032023-03-22T12:40:49ZengSpringerOpenProgress in Earth and Planetary Science2197-42842023-03-0110111410.1186/s40645-023-00542-6Near-real-time estimation of fossil fuel CO2 emissions from China based on atmospheric observations on Hateruma and Yonaguni Islands, JapanYasunori Tohjima0Yosuke Niwa1Prabir K. Patra2Hitoshi Mukai3Toshinobu Machida4Motoki Sasakawa5Kazuhiro Tsuboi6Kazuyuki Saito7Akihiko Ito8National Institute for Environmental Studies (NIES)National Institute for Environmental Studies (NIES)Japan Agency for Marine-Earth Science and Technology (JAMSTEC)National Institute for Environmental Studies (NIES)National Institute for Environmental Studies (NIES)National Institute for Environmental Studies (NIES)Meteorological Research Institute (MRI)Japan Meteorological Agency (JMA)National Institute for Environmental Studies (NIES)Abstract We developed a near-real-time estimation method for temporal changes in fossil fuel CO2 (FFCO2) emissions from China for 3 months [January, February, March (JFM)] based on atmospheric CO2 and CH4 observations on Hateruma Island (HAT, 24.06° N, 123.81° E) and Yonaguni Island (YON, 24.47° N, 123.01° E), Japan. These two remote islands are in the downwind region of continental East Asia during winter because of the East Asian monsoon. Previous studies have revealed that monthly averages of synoptic-scale variability ratios of atmospheric CO2 and CH4 (ΔCO2/ΔCH4) observed at HAT and YON in JFM are sensitive to changes in continental emissions. From the analysis based on an atmospheric transport model with all components of CO2 and CH4 fluxes, we found that the ΔCO2/ΔCH4 ratio was linearly related to the FFCO2/CH4 emission ratio in China because calculating the variability ratio canceled out the transport influences. Using the simulated linear relationship, we converted the observed ΔCO2/ΔCH4 ratios into FFCO2/CH4 emission ratios in China. The change rates of the emission ratios for 2020–2022 were calculated relative to those for the preceding 9-year period (2011–2019), during which relatively stable ΔCO2/ΔCH4 ratios were observed. These changes in the emission ratios can be read as FFCO2 emission changes under the assumption of no interannual variations in CH4 emissions and biospheric CO2 fluxes for JFM. The resulting average changes in the FFCO2 emissions in January, February, and March 2020 were 17 ± 8%, − 36 ± 7%, and − 12 ± 8%, respectively, (− 10 ± 9% for JFM overall) relative to 2011–2019. These results were generally consistent with previous estimates. The emission changes for January, February, and March were 18 ± 8%, − 2 ± 10%, and 29 ± 12%, respectively, in 2021 (15 ± 10% for JFM overall) and 20 ± 9%, − 3 ± 10%, and − 10 ± 9%, respectively, in 2022 (2 ± 9% for JFM overall). These results suggest that the FFCO2 emissions from China rebounded to the normal level or set a new high record in early 2021 after a reduction during the COVID-19 lockdown. In addition, the estimated reduction in March 2022 might be attributed to the influence of a new wave of COVID-19 infections in Shanghai.https://doi.org/10.1186/s40645-023-00542-6Fossil fuel CO2 emissionsSynoptic-scale variationsAtmospheric CO2Atmospheric CH4COVID-19 lockdownEast Asian Monsoon
spellingShingle Yasunori Tohjima
Yosuke Niwa
Prabir K. Patra
Hitoshi Mukai
Toshinobu Machida
Motoki Sasakawa
Kazuhiro Tsuboi
Kazuyuki Saito
Akihiko Ito
Near-real-time estimation of fossil fuel CO2 emissions from China based on atmospheric observations on Hateruma and Yonaguni Islands, Japan
Progress in Earth and Planetary Science
Fossil fuel CO2 emissions
Synoptic-scale variations
Atmospheric CO2
Atmospheric CH4
COVID-19 lockdown
East Asian Monsoon
title Near-real-time estimation of fossil fuel CO2 emissions from China based on atmospheric observations on Hateruma and Yonaguni Islands, Japan
title_full Near-real-time estimation of fossil fuel CO2 emissions from China based on atmospheric observations on Hateruma and Yonaguni Islands, Japan
title_fullStr Near-real-time estimation of fossil fuel CO2 emissions from China based on atmospheric observations on Hateruma and Yonaguni Islands, Japan
title_full_unstemmed Near-real-time estimation of fossil fuel CO2 emissions from China based on atmospheric observations on Hateruma and Yonaguni Islands, Japan
title_short Near-real-time estimation of fossil fuel CO2 emissions from China based on atmospheric observations on Hateruma and Yonaguni Islands, Japan
title_sort near real time estimation of fossil fuel co2 emissions from china based on atmospheric observations on hateruma and yonaguni islands japan
topic Fossil fuel CO2 emissions
Synoptic-scale variations
Atmospheric CO2
Atmospheric CH4
COVID-19 lockdown
East Asian Monsoon
url https://doi.org/10.1186/s40645-023-00542-6
work_keys_str_mv AT yasunoritohjima nearrealtimeestimationoffossilfuelco2emissionsfromchinabasedonatmosphericobservationsonhaterumaandyonaguniislandsjapan
AT yosukeniwa nearrealtimeestimationoffossilfuelco2emissionsfromchinabasedonatmosphericobservationsonhaterumaandyonaguniislandsjapan
AT prabirkpatra nearrealtimeestimationoffossilfuelco2emissionsfromchinabasedonatmosphericobservationsonhaterumaandyonaguniislandsjapan
AT hitoshimukai nearrealtimeestimationoffossilfuelco2emissionsfromchinabasedonatmosphericobservationsonhaterumaandyonaguniislandsjapan
AT toshinobumachida nearrealtimeestimationoffossilfuelco2emissionsfromchinabasedonatmosphericobservationsonhaterumaandyonaguniislandsjapan
AT motokisasakawa nearrealtimeestimationoffossilfuelco2emissionsfromchinabasedonatmosphericobservationsonhaterumaandyonaguniislandsjapan
AT kazuhirotsuboi nearrealtimeestimationoffossilfuelco2emissionsfromchinabasedonatmosphericobservationsonhaterumaandyonaguniislandsjapan
AT kazuyukisaito nearrealtimeestimationoffossilfuelco2emissionsfromchinabasedonatmosphericobservationsonhaterumaandyonaguniislandsjapan
AT akihikoito nearrealtimeestimationoffossilfuelco2emissionsfromchinabasedonatmosphericobservationsonhaterumaandyonaguniislandsjapan