Constraint of satellite CO2 retrieval on the global carbon cycle from a Chinese atmospheric inversion system

Scientists from the Institute of Tibetan Plateau Research, Chinese Academy of Sciences developed an atmospheric inversion system GONGGA (Global ObservatioN-based system for monitoring Greenhouse GAes) to infer CO₂ sources and sinks from atmospheric CO₂ observations.

In the study published in Science China Earth Sciences, GONGGA assimilated Orbiting Carbon Observatory-2 (OCO-2) satellite column CO₂ retrievals during the period 2015–2019 and compared their estimates to five other state-of-the-art inversions. The global net terrestrial carbon sink (net biome productivity, NBP) was estimated to be 1.03±0.39 petagrams of carbon per year (PgC yr⁻¹); this estimate is consistent with Global Carbon Project and other satellite-based inversions, but slightly lower than the surface-based inversions of 1.46–2.52 PgC yr⁻¹. In the regional distribution, GONGGA estimated a weak northern uptake of 1.30 PgC yr⁻¹ and weak tropical release of −0.26 PgC yr⁻¹, consistent with multiple independent lines of evidence.

During the 2015–2016 El Niño event, the tropical land biosphere released a significant amount of CO₂ and was mainly responsible for a higher global CO₂ growth rate. The northern extratropics, on the contrary, was an anomalously high carbon sink during the same period, due to the concurrent extreme Northern Hemisphere greening, partially offsetting the tropical carbon losses.

The satellite constraint from GONGGA refines the current understanding of flux partitioning between northern and tropical terrestrial regions.

Scientists from the Institute of Tibetan Plateau Research, Chinese Academy of Sciences developed an atmospheric inversion system GONGGA (Global ObservatioN-based system for monitoring Greenhouse GAes) to infer CO₂ sources and sinks from atmospheric CO₂ observations.

In the study published in Science China Earth Sciences, GONGGA assimilated Orbiting Carbon Observatory-2 (OCO-2) satellite column CO₂ retrievals during the period 2015–2019 and compared their estimates to five other state-of-the-art inversions. The global net terrestrial carbon sink (net biome productivity, NBP) was estimated to be 1.03±0.39 petagrams of carbon per year (PgC yr⁻¹); this estimate is consistent with Global Carbon Project and other satellite-based inversions, but slightly lower than the surface-based inversions of 1.46–2.52 PgC yr⁻¹. In the regional distribution, GONGGA estimated a weak northern uptake of 1.30 PgC yr⁻¹ and weak tropical release of −0.26 PgC yr⁻¹, consistent with multiple independent lines of evidence.

During the 2015–2016 El Niño event, the tropical land biosphere released a significant amount of CO₂ and was mainly responsible for a higher global CO₂ growth rate. The northern extratropics, on the contrary, was an anomalously high carbon sink during the same period, due to the concurrent extreme Northern Hemisphere greening, partially offsetting the tropical carbon losses.

The satellite constraint from GONGGA refines the current understanding of flux partitioning between northern and tropical terrestrial regions.