BUT it's important to note that in Earth System models, the RCP8.5 CO2 *concentration pathway* can still arise from a lower emissions scenario (eg. SRES A1B) if feedbacks are strong
Any particular emissions scenario can give rise to many different future concentration pathways, some rising faster and some slower, depending on the strength of carbon cycle feedbacks
Variants of the HadCM3C model can project a CO2 rise above that when driven by the lower emissions scenario SRES A1B
journals.ametsoc.org/doi/pdf/10.117…
(box: 25%-75% interquartile range, whiskers: full range)
This still suggests RCP8.5 concentrations are less likely, but can't be ruled out
Unfortunately many papers discussing RCP-driven climate projections say they're using an "emissions scenario" when in fact they're using a *concentrations scenario*