The representation of sea salt aerosols and their role in polar climate within CMIP6

Lapere, Rémy; Thomas, Jennie L.; Marelle, Louis; Ekman, Annica M.L.; Frey, Markus M. ORCID: https://orcid.org/0000-0003-0535-0416; Lund, Marianne Tronstad; Makkonen, Risto; Ranjithkumar, Ananth; Salter, Matthew E.; Samset, Bjørn Hallvard; Schulz, Michael; Sogacheva, Larisa; Yang, Xin ORCID: https://orcid.org/0000-0002-3838-9758; Zieger, Paul. 2023 The representation of sea salt aerosols and their role in polar climate within CMIP6. Journal of Geophysical Research: Atmospheres, 128 (6), e2022JD038235. 36, pp. https://doi.org/10.1029/2022JD038235

Before downloading, please read NORA policies.

Preview

Text (Open Access) © 2023. The Authors. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. JGR Atmospheres - 2023 - Lapere - The Representation of Sea Salt Aerosols and Their Role in Polar Climate Within CMIP6.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (10MB) | Preview

Abstract/Summary

Natural aerosols and their interactions with clouds remain an important uncertainty within climate models, especially at the poles. Here, we study the behavior of sea salt aerosols (SSaer) in the Arctic and Antarctic within 12 climate models from CMIP6. We investigate the driving factors that control SSaer abundances and show large differences based on the choice of the source function, and the representation of aerosol processes in the atmosphere. Close to the poles, the CMIP6 models do not match observed seasonal cycles of surface concentrations, likely due to the absence of wintertime SSaer sources such as blowing snow. Further away from the poles, simulated concentrations have the correct seasonality, but have a positive mean bias of up to one order of magnitude. SSaer optical depth is derived from the MODIS data and compared to modeled values, revealing good agreement, except for winter months. Better agreement for AOD than surface concentration may indicate a need for improving the vertical distribution, the size distribution and/or hygroscopicity of modeled polar SSaer. Source functions used in CMIP6 emit very different numbers of small SSaer, potentially exacerbating cloud-aerosol interaction uncertainties in these remote regions. For future climate scenarios SSP126 and SSP585, we show that SSaer concentrations increase at both poles at the end of the 21st century, with more than two times mid-20th century values in the Arctic. The pre-industrial climate CMIP6 experiments suggest there is a large uncertainty in the polar radiative budget due to SSaer.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1029/2022JD038235
ISSN:	2169-897X
Additional Keywords:	CMIP6, Sea salt aerosol, Polar climate
Date made live:	08 Mar 2023 10:30 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/534187

Actions (login required)

View Item

Document Downloads

More statistics for this item...