Abstract

The measurements of one of the major greenhouse gases, carbon dioxide (CO2), are being made using dedicated satellite remote sensing since the launch of the greenhouse gases observing satellite (GOSAT) by a three-way partnership between the Japan Aerospace Exploration Agency (JAXA), the Ministry of Environment (MoE) and the National Institute for Environmental Studies (NIES), and the National Aeronautics and Space Administration (NASA) Orbiting Carbon Observatory-2 (OCO-2). In the past 10 years, estimation of CO2 fluxes from land and ocean using the earth system models (ESMs) and inverse modelling of in situ atmospheric CO2 data have also made significant progress. We attempt, for the first time, to evaluate the CO2 fluxes simulated by an earth system model (MIROC-ES2L) and the fluxes estimated by an inverse model (MIROC4-Inv) using in situ data by comparing with GOSAT and OCO-2 observations. Both MIROC-ES2L and MIROC4-Inv fluxes are used in the MIROC4-atmospheric chemistry transport model (referred to as ACTM_ES2LF and ACTM_InvF, respectively) for calculating total column CO2 mole fraction (XCO2) that are sampled at the time and location of the satellite measurements. Both the ACTM simulations agreed well with the GOSAT and OCO-2 satellite observations, within 2 ppm for the spatial maps and time evolutions of the zonal mean distributions. Our results suggest that the inverse model using in situ data is more consistent with the OCO-2 retrievals, compared with those of the GOSAT XCO2 data due to the higher accuracy of the former. This suggests that the MIROC4-Inv fluxes are of sufficient quality to evaluate MIROC-ES2L simulated fluxes. The ACTM_ES2LF simulation shows a slightly weaker seasonal cycle for the meridional profiles of CO2 fluxes, compared with that from the ACTM_InvF. This difference is revealed by greater XCO2 differences for ACTM_ES2LF vs GOSAT, compared with those of ACTM_InvF vs GOSAT. Using remote sensing–based global products of leaf area index (LAI) and gross primary productivity (GPP) over land, we show a weaker sensitivity of MIROC-ES2L biospheric activities to the weather and climate in the tropical regions. Our results clearly suggest the usefulness of XCO2 measurements by satellite remote sensing for evaluation of large-scale ESMs, which so far remained untested by the sparse in situ data.

Highlights

  • Carbon dioxide (CO2) is the most important anthropogenically produced greenhouse gas (Myhre et al 2013)

  • We have corrected the Global Carbon Budget (GCB) land and ocean fluxes for riverine export (Resplandy et al 2018), i.e. 0.78 PgC year−1 is added to the land sink and removed from the ocean sink for this comparison because the inversion and earth system model (ESM) fluxes are used in the Atmospheric chemistry transport model (ACTM) simulations for atmospheric CO2 without any spatial adjustment for riverine export flux

  • 4 Conclusions We have compared the simulated total column CO2 concentrations (XCO2) by Japan Agency for Marine-Earth Science and Technology (JAMSTEC)’s ACTM, using CO2 fluxes from an atmospheric CO2 inversion (ACTM_InvF) and an ESM (ACTM_ES2LF), with the XCO2 observed by gases observing satellite (GOSAT) and Orbiting Carbon Observatory-2 (OCO-2)

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Summary

Introduction

Carbon dioxide (CO2) is the most important anthropogenically produced greenhouse gas (Myhre et al 2013). Uncertainties in the emissions are larger for non-Annex I counties relative to the Annex I countries (Andres et al 2012). This leads to lower confidence of our knowledge of the changes in terrestrial biospheric fluxes in response to climate change and climate variabilities, and CO2 fertilisation feedbacks (Ainsworth and Rogers 2007; Keenan et al 2013; Saeki and Patra 2017; Bastos et al 2020)

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