4.7 Article

Global terrestrial isoprene emission models: sensitivity to variability in climate and vegetation

期刊

ATMOSPHERIC CHEMISTRY AND PHYSICS
卷 11, 期 15, 页码 8037-8052

出版社

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/acp-11-8037-2011

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资金

  1. Human Frontier Science Programme
  2. EU [FP7-ENV-2010/265148]
  3. Swedish Research Council Formas [2007-331]
  4. Swedish Research Council VR [2005-4039, 2009-4290]
  5. Alexander von Humboldt Foundation
  6. UK Natural Environment Research Council [NE/C001621/1]
  7. Natural Environment Research Council [NE/D002117/1, ceh010010, NE/C001672/1] Funding Source: researchfish
  8. NERC [NE/D002117/1] Funding Source: UKRI

向作者/读者索取更多资源

Due to its effects on the atmospheric lifetime of methane, the burdens of tropospheric ozone and growth of secondary organic aerosol, isoprene is central among the biogenic compounds that need to be taken into account for assessment of anthropogenic air pollution-climate change interactions. Lack of process-understanding regarding leaf isoprene production as well as of suitable observations to constrain and evaluate regional or global simulation results add large uncertainties to past, present and future emissions estimates. Focusing on contemporary climate conditions, we compare three global isoprene models that differ in their representation of vegetation and isoprene emission algorithm. We specifically aim to investigate the between-and within model variation that is introduced by varying some of the models' main features, and to determine which spatial and/or temporal features are robust between models and different experimental set-ups. In their individual standard configurations, the models broadly agree with respect to the chief isoprene sources and emission seasonality, with maximum monthly emission rates around 20-25 Tg C, when averaged by 30-degree latitudinal bands. They also indicate relatively small (approximately 5 to 10% around the mean) interannual variability of total global emissions. The models are sensitive to changes in one or more of their main model components and drivers (e. g., underlying vegetation fields, climate input) which can yield increases or decreases in total annual emissions of cumulatively by more than 30 %. Varying drivers also strongly alters the seasonal emission pattern. The variable response needs to be interpreted in view of the vegetation emission capacities, as well as diverging absolute and regional distribution of light, radiation and temperature, but the direction of the simulated emission changes was not as uniform as anticipated. Our results highlight the need for modellers to evaluate their implementations of isoprene emission models carefully when performing simulations that use nonstandard emission model configurations.

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