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A multi-model assessment of the efficacy of sea spray geoengineering

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Academic year: 2017

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Table 1. The accumulation mode background aerosol loading taken from Heintzenberg and Larssen (2004, HL04) and cloud droplet number concentration simulated using a range up updraught velocities
Table 2. Regional mean increase in total aerosol number (cm −3 ) at 1 km altitude arising from sea spray geoengineering as calculated using the simulation of Korhonen et al
Table 3. Summary of updraught velocities calculated in an LEM simulation for the ASTEX GCSS Sc-Cu transition case
Table 4. Summary of the 4 aerosol models used.
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