EGU25-6015, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-6015
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Wednesday, 30 Apr, 09:50–10:00 (CEST)
 
Room F2
Distinct climate responses to regional aerosol emissions
Laura Wilcox1, Bjørn Samset2, Camilla Stjern2, Robert Allen3, and the RAMIP Team*
Laura Wilcox et al.
  • 1University of Reading, National Centre for Atmospheric Science, Department of Meteorology, Reading, United Kingdom of Great Britain – England, Scotland, Wales (l.j.wilcox@reading.ac.uk)
  • 2CICERO Center for International Climate Research, Oslo, Norway
  • 3University of California, Riverside
  • *A full list of authors appears at the end of the abstract

Anthropogenic aerosol emissions have had a major influence on global climate over the industrial era, counteracting some of the warming and precipitation increases due to rising greenhouse gas concentrations. These greenhouse gas driven changes are now rapidly being unmasked, through a range of national and regional policies aimed at improving air quality. However, unlike greenhouse gases, aerosol emissions have strongly regional response patterns, and influence the climate both near to, and far from emission sources. These regional influences have to date not been quantified in a consistent, multi-model framework.

Here, we present results from the Regional Aerosol Model Intercomparison Project (RAMIP). Ten CMIP6 era models have performed 10- member ensemble simulations investigating the climate response to aerosol emissions, separately, from South Asia, East Asia, Africa and the Middle East, and Europe and North America. All RAMIP experiments are based on two CMIP6-era SSPs: SSP3-7.0 (strong GHG increases, minimal aerosol reductions) and a hybrid SSP370-126aer (anthropogenic emissions of SO2, organic carbon, and black carbon are rapidly reduced following SSP1-2.6, either globally or regionally).

We find a rapid surface warming in response to aerosol reductions, and strong precipitation increases, but with marked regional differences in the magnitude of the response. While there are many robust responses, strong inter-model differences in the pattern and strength of the responses in some regions highlights where aerosol related uncertainty is large in the near-future.

We discuss the linearity of the effective radiative forcing and climate responses from regional aerosol perturbations, and demonstrate that emission location is key to the amplitude and extent of the response. In particular, emission changes in East Asia and North America and Europe have a larger global temperature impact than those over South Asia due to their influence on Pacific clouds. This initial analysis demonstrates the need for aerosol awareness in the design of future scenario ensembles, and in climate risk and impact studies both near to and far from aerosol emission sources.

RAMIP Team:

Laura Wilcox, Bjørn Samset, Robert Allen, Declan O'Donnell, Luke Fraser-Leach, Paul Griffiths, James Keeble, Tsuyoshi Koshiro, Paul Kushner, Anna Lewinschal, Risto Makkonen, Joonas Merikanto, Pierre Nabat, Naga Oshima, David Paynter, Steve Rumbold, Toshihiko Takemura, Kostas Tsigaridis, Dan Westevelt

How to cite: Wilcox, L., Samset, B., Stjern, C., and Allen, R. and the RAMIP Team: Distinct climate responses to regional aerosol emissions, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-6015, https://doi.org/10.5194/egusphere-egu25-6015, 2025.