Searcharxiv⌕ Search
Home/Archive/arXiv

arXiv · 2111.02222

Global fossil carbon emissions rebound near pre-COVID-19 levels

RB Jackson·P Friedlingstein·C Le Quere·S Abernethy·RM Andrew·JG Canadell·P Ciais·SJ Davis·Zhu Deng·Zhu Liu·GP Peters
View original source ↗Read source document ↗Export metadata ↓

Abstract

Global fossil CO2 emissions in 2020 decreased 5.4%, from 36.7 Gt CO2 in 2019 to 34.8 Gt CO2 in 2020, an unprecedented decline of ~1.9 Gt CO2. We project that global fossil CO2 emissions in 2021 will rebound 4.9% (4.1% to 5.7%) compared to 2020 to 36.4 Gt CO2, returning nearly to 2019 emission levels of 36.7 Gt CO2. Emissions in China are expected to be 7% higher in 2021 than in 2019 (reaching 11.1 Gt CO2) and only slightly higher in India (a 3% increase in 2021 relative to 2019, and reaching 2.7 Gt CO2). In contrast, projected 2021 emissions in the United States (5.1 Gt CO2), European Union (2.8 Gt CO2), and rest of the world (14.8 Gt CO2, in aggregate) remain below 2019 levels. For fuels, CO2 emissions from coal in 2021 are expected to rebound above 2019 levels to 14.7 Gt CO2, primarily because of increased coal use in China, and will remain only slightly (0.8%) below their previous peak in 2014. Emissions from natural gas use should also rise above 2019 levels in 2021, continuing a steady trend of rising gas use that dates back at least sixty years. Only CO2 emissions from oil remain well below 2019 levels in 2021.

Explore related subjects

physics.ao-ph

Keep this discovery

BibTeXRIS

RB Jackson, P Friedlingstein, C Le Quere, S Abernethy, RM Andrew, JG Canadell, P Ciais, SJ Davis, Zhu Deng, Zhu Liu, GP Peters. 2021-11-03. Global fossil carbon emissions rebound near pre-COVID-19 levels. https://doi.org/10.1088/1748-9326%2Fac55b6

Cite the original work for its findings. Save a collection to share your selection of sources.

KEEP EXPLORING

Related papers

arXiv2026

Windowed Envelope Statistics for Time-Domain Significant Wave Height Estimation From HF Radar

Significant wave height (SWH) retrieval from high-frequency (HF) radar typically relies on a weak second-order Doppler continuum that is sensitive to noise, interference, and spectral leakage. This letter presents a Windowed Envelope Statistics Estimator (WESE) that operates directly on beam-formed time-domain voltages. A second-order term obtained from a Neumann expansion of the rough-surface field equation motivates quadratic compensation of localized radar features. WESE extracts the mean, standard deviation, or variance from overlapping windows of the in-phase, quadrature, or envelope-magnitude sequence, followed by quadratic compensation, rank ordering, least-squares regression, and causal smoothing. Evaluation used 335 synchronized hourly observations from a 13.385 MHz, 12-element WERA system at Argentia, Newfoundland and Labrador. The optimal configuration used quadrature variance, a 16-sample window, 896 retained chronological samples, and 30-h smoothing, achieving an RMSE of 0.152 m and a Pearson correlation of 0.978. This represents RMSE reductions of 32.1% and 18.7% relative to previously reported linear and second-order compensated ordered-statistics models, respectively. The results demonstrate robust time-domain SWH estimation without explicit Doppler-spectrum construction.

physics.ao-ph↗
arXiv2026

KiloDA: Reconstructing kilometer-scale near-surface wind states from sparse station observations

Accurate kilometer-scale near-surface winds are important for understanding atmospheric processes over complex terrain, yet remain difficult to reconstruct from sparse and unevenly distributed observations. Here we introduce KiloDA, a diffusion framework for hourly kilometer-scale wind reconstruction from surface stations. KiloDA learns the statistical distribution and spatial structure of wind fields from historical 3-km Weather Research and Forecasting (WRF) model forecasts. At each reconstruction time, no contemporaneous WRF field is used. Instead, station observations provide the only constraints on the current atmospheric state and guide posterior sampling from the learned prior. In idealized WRF experiments, KiloDA recovers localized wind structures when only 0.24% of grid cells are observed and shows an overall advantage over conventional interpolation across terrain conditions and wind speed regimes. This capability largely transfers to real observations. In a fully withheld region, KiloDA reduces the median wind speed root mean square error (RMSE) by 19% relative to ERA5 reanalysis, using only observations outside the region, with the largest improvements over high-elevation and high-relief terrain. A random station holdout further confirms that this advantage extends across different complex-terrain locations and holdout configurations. These results show that historical model archives can provide useful structural knowledge for reconstructing kilometer-scale wind fields from sparse observations without requiring an accurate model estimate of the current atmospheric state.

physics.ao-ph↗