China’s Carbon Dioxide (CO2) Emissions Have Been Overestimated
— Advancement in verification of fossil fuel CO2 and CH4 sources from China —
| Anthropogenic CO2 emission increase during 2003-2007 has very likely been overestimated for China, which suggests estimated CO2 sink increase over East Asia (China, Japan, Korea and Mongolia) during 2002-2012 may be due to high bias in CO2 emissions from China, according to a new study by Dr. Prabir K Patra at the Department of Environmental Geochemical Cycle Research, Japan Agency for Marine-Earth Science and Technology (JAMSTEC: Asahiko Taira, President), with Dr. Tazu Saeki at the Center for Global Environmental Research, National Institute for Environmental Studies (Chiho Watanabe, President).
Based on high-precision measurements of atmospheric concentration and an atmospheric chemistry-transport model*1, they estimated surface sources and sinks of CO2 and CH4 as the most significant greenhouse gases*2. Distinction between CO2 sources and sinks at regional scales is important for future predictions of atmospheric concentration and quantification of global warming as well as for greenhouse gases emission management. Presently, the sources and sinks on the Earth’s surface are calculated by country-level statistics (bottom-up modeling; Fig. 1), which are then refined with atmospheric concentrations (top-down modeling). High bias in bottom-up anthropogenic CO2 emissions seems to result in larger land CO2 sink estimates due to the top-down constraint on the total CO2 flux by the atmospheric CO2 growth rate.
In addition, the scientist’s independent results from methane (CH4) inversion (as reported in press release on February 01, 2016) supported lowering the East Asian CH4 emission increase rate by 41% during the period of 2002-2012 (Fig. 2). Long-term aircraft measurements of CH4 over Sendai carried out by Tohoku University have also provided a key verification on the rate of CH4 emission increase from the East Asia region. By applying a scaling factor of 0.59, based on CH4 inversion (Fig. 2), to the rate of bottom-up anthropogenic CO2 emission growth rate for China (1.7 petagram of Carbon over a period of 2002-2012), they find no systematic increase in land CO2 uptake over East Asia during 1993-2010 or 2000-2009 (Fig. 3). No significant change of East Asian CO2 sink is in better agreement with the terrestrial biospheric model simulations that include CO2-fertlization and climate effect, and bottom-up estimation from the country reporting to the Food and Agriculture Organization (FAO) between the 1990s and 2000s (Fig. 3).
These results have large implications for greenhouse gas management as per the Intended Nationally Determined Contributions (INDCs) under the Paris Agreement, contributing to efforts for reduction of greenhouse gas emissions and how the terrestrial ecosystems models are tuned for climate prediction studies.
This study has been carried out as part of the Environment Research and Technology Development Fund (Research Number: 2-1401) by Ministry of the Environment, Japan. The above results were published on the Geoscience Letters, the official journal of the Asia Oceania Geosciences Society on May 16, 2017 (JST).
Title: Implications of overestimated anthropogenic CO2 emissions on East Asian and global land CO2 flux inversion
Authors: T. Saeki1,2, P. K. Patra1
1. Department of Environmental Geochemical Cycle Research, JAMSTEC 2. Present address: Center for Global Environmental Research, National Institute for Environmental Studies
*1 Atmospheric Chemistry Transport Model: Numerical simulations are performed using atmospheric chemistry-transport model to calculate spatial distributions and time evolution of chemical species in the atmosphere using large-scale super computers. The JAMSTEC’s atmospheric chemistry-transport model (ACTM) is based on the CCSR/NIES/FRCGC atmospheric general circulation model (AGCM). It is also used for top-down modeling of emission refinements using atmospheric concentration observations.
*2 Greenhouse gases: Carbon dioxide (CO2) and methane (CH4) are the two most prevalent anthropogenically produced greenhouse gas. Both are colorless and odorless, having large impacts on global warming. About 73% and 42% of the net anthropogenic greenhouse effect is attributed to CO2 and CH4 respectively over the period of 1750-2011. According to the IPCC 5th Assessment Report, emissions of CO2 and CH4 together contribute 78% of the anthropogenic radiative forcing increase since the preindustrial era. By sending it back to the Earth’s surface, GHGs trap heat in the atmosphere, which is measured by radiative forcing that is integrated since a pre-industrial reference period of 1750,
Reference: Lifetime and radiative forcing (RF) of main greenhouse gases, quoted from Figure SPM.5 of the IPCC Fifth Assessment Report. Concentrations are taken for World Data Centre for Greenhouse Gases (WDCGG) (The World Meteorological Organization (WMO) Greenhouse Gas Bulletin, No.12, 2016; http://ds.data.jma.go.jp/gmd/wdcgg).
(For this study)
Prabir K. Patra, Senior Scientist, Department of Environmental Geochemical Cycle Research, JAMSTEC Email:firstname.lastname@example.org
(For press release)
Tsuyoshi Noguchi, Press Division, Public Relations Department, JAMSTEC
Riho Takahashi, Public Relations, National Institute for Environmental Studies
Email: press(add “@nies.go.jp”)
May 16th, 2017