Table 1 Model simulations and corresponding prescribed isoprene emissions

From: Atmospheric isoprene measurements reveal larger-than-expected Southern Ocean emissions

Simulation

Isoprene emissions

Ratio of simulated / observed Isop concentration (\({{{{{\rm{median}}}}}}_{25{{{{{\rm{th}}}}}}\; {{{{{\rm{percentile}}}}}}}^{75{{{{{\rm{th}}}}}}\; {{{{{\rm{percentile}}}}}}}\))

TI_base

Terrestrial only

\( < 1{0}^{-9}\)

TI_2x_30S

Terrestrial only with emissions below 30°S doubled.

\( < 1{0}^{-9}\)

TI_MI_MEAN

Terrestrial emissions and marine emissions calculated following ISOREMS parameterisation12

\({0.025}_{0.008}^{0.062}\)

TI_MI_20x

As TI_MI_MEAN but marine emissions scaled by 20.

\({0.490}_{0.166}^{1.153}\)

TI_MI_MEAN_D

As TI_MI_MEAN but with a diurnal scaling applied to marine isoprene emissions.

\({0.019}_{0.006}^{0.046}\)

TI_MI_20x_D

As TI_MI_20x but with a diurnal scaling applied to marine isoprene emissions.

\({0.368}_{0.146}^{0.838}\)

TI_MI_MEAN_D_sink

As TI_MI_MEAN_D with an extra species, “OH-sink”, which has (non-diurnally varying) emissions equal to those of marine isoprene. OH-sink has a rate constant half that of isoprene + OH and does not regenerate any OH.

\({0.018}_{0.006}^{0.045}\)

TI_MI_MEAN_D_sink_100x

As TI_MI_MEAN_D_sink but OH-sink emissions are 100x those of marine isoprene.

\({0.021}_{0.008}^{0.053}\)

  1. All simulations were performed for the period Dec 2016 - Mar 2017 (inclusive). Terrestrial emissions were taken from the 2001–2010 MEGAN-MACC climatology (Methods) and featured a diurnal scaling. Marine isoprene emissions did not have a diurnal scaling unless otherwise stated.