Abstract

Black Carbon (BC) aerosols substantially affect the global climate. However, accurate simulation of BC atmospheric transport remains elusive, due to shortcomings in modeling and a shortage of constraining measurements. Recently, several studies have compared simulations with observed vertical concentration profiles, and diagnosed a global-mean BC atmospheric residence time of <5 days. These studies have, however, been focused on limited geographical regions, and used temporally and spatially coarse model information. Here we expand on previous results by comparing a wide range of recent aircraft measurements from multiple regions, including the Arctic and the Atlantic and Pacific oceans, to simulated distributions obtained at varying spatial and temporal resolution. By perturbing BC removal processes and using current best-estimate emissions, we confirm a constraint on the global-mean BC lifetime of <5.5 days, shorter than in many current global models, over a broader geographical range than has so far been possible. Sampling resolution influences the results, although generally without introducing major bias. However, we uncover large regional differences in the diagnosed lifetime, in particular in the Arctic. We also find that only a weak constraint can be placed in the African outflow region over the South Atlantic, indicating inaccurate emission sources or model representation of transport and microphysical processes. While our results confirm that BC lifetime is shorter than predicted by most recent climate models, they also cast doubt on the usability of the concept of a “global-mean BC lifetime” for climate impact studies, or as an indicator of model skill.

Highlights

  • Black carbon (BC) aerosols play an important role in the Earth’s climate system through absorption of solar radiation, interaction with clouds, and deposition on snow and ice

  • The global-mean BC lifetimes, defined as the global burden divided by total emissions, of these models in the baseline configuration are 4.4 and 6.5 days for OsloCTM3 and ECHAM-HAM, respectively

  • This is seen in both models, which have different aerosol treatments and emission inventories, and across several seasons covered by Atmospheric Tomography (ATom) and SALTRACE campaigns

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Summary

INTRODUCTION

Black carbon (BC) aerosols play an important role in the Earth’s climate system through absorption of solar radiation, interaction with clouds, and deposition on snow and ice. We find significant regional differences in the diagnosed “lifetime”, and a shortcoming of the method over the Atlantic Ocean, indicating either uncertainties in emission sources or a poor representation of transport and microphysical processes Such discrepancies are likely to affect studies using average BC distributions and a globalmean lifetime to diagnose RF or climate impacts

RESULTS
DISCUSSION AND CONCLUSIONS
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