Cargando…
1.5 °C carbon budget dependent on carbon cycle uncertainty and future non-CO(2) forcing
Estimates of the 1.5 °C carbon budget vary widely among recent studies, emphasizing the need to better understand and quantify key sources of uncertainty. Here we quantify the impact of carbon cycle uncertainty and non-CO(2) forcing on the 1.5 °C carbon budget in the context of a prescribed 1.5 °C t...
Autores principales: | , , , |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2018
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5895820/ https://www.ncbi.nlm.nih.gov/pubmed/29643459 http://dx.doi.org/10.1038/s41598-018-24241-1 |
Sumario: | Estimates of the 1.5 °C carbon budget vary widely among recent studies, emphasizing the need to better understand and quantify key sources of uncertainty. Here we quantify the impact of carbon cycle uncertainty and non-CO(2) forcing on the 1.5 °C carbon budget in the context of a prescribed 1.5 °C temperature stabilization scenario. We use Bayes theorem to weight members of a perturbed parameter ensemble with varying land and ocean carbon uptake, to derive an estimate for the fossil fuel (FF) carbon budget of 469 PgC since 1850, with a 95% likelihood range of (411,528) PgC. CO(2) emissions from land-use change (LUC) add about 230 PgC. Our best estimate of the total (FF + LUC) carbon budget for 1.5 °C is therefore 699 PgC, which corresponds to about 11 years of current emissions. Non-CO(2) greenhouse gas and aerosol emissions represent equivalent cumulative CO(2) emissions of about 510 PgC and −180 PgC for 1.5 °C, respectively. The increased LUC, high non-CO(2) emissions and decreased aerosols in our scenario, cause the long-term FF carbon budget to decrease following temperature stabilization. In this scenario, negative emissions would be required to compensate not only for the increasing non-CO(2) climate forcing, but also for the declining natural carbon sinks. |
---|