EGU24-20722, updated on 11 Mar 2024
https://doi.org/10.5194/egusphere-egu24-20722
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Enhanced aerosol-induced near-term Arctic warming due to remote regional aerosol perturbations in RAMIP

Daniel Westervelt1,2, Yanda Zhang1, Joe Adabouk Amooli1, Kostas Tsigaridis1,2, Larissa Nazarenko2, Bjørn Samset3, Laura Wilcox4, and Robert Allen5
Daniel Westervelt et al.
  • 1Columbia University, Lamont Doherty Earth Observatory, Ocean and Climate Physics, New York, United States of America (dan.westervelt@gmail.com)
  • 2NASA Goddard Institute for Space Studies, New York, USA
  • 3CICERO, Oslo, Norway
  • 4University of Reading, Reading, United Kingdom
  • 5University of California Riverside, Riverside, USA

The climatic implications of regional aerosol and precursor emissions reductions implemented to protect human health are poorly understood. However, quantitative estimates of climate responses to emission perturbations are needed by the climate assessment and impacts community. The Regional Aerosol Model Intercomparison Project (RAMIP) project builds on recent CMIP5 and CMIP6-era studies to help address this knowledge gap. Briefly, RAMIP will use contrasting SSP aerosol emissions (SO2, BC, OC) scenarios (SSP3-7.0 and SSP1-2.6) to isolate the impact of realistic, near term aerosol changes on climate and air quality over rapidly developing regions of South Asia, East Asia, and Africa, and over North America and Europe. At least 9 CMIP6-generation global climate models are contributing to this new MIP, which uniquely focuses on specific regional aerosol emissions changes rather than simultaneous global changes. This presentation will specifically present the first results from several participating models in RAMIP, namely the NASA Goddard Institute for Space Studies (GISS) ModelE, UKESM, CESM2, and NorESM. All Tier 1 simulations of RAMIP are included, with 10 ensembles for each simulation. Initial analysis at the time of writing confirms the anticipated changes in aerosol optical depth, downwelling shortwave radiation, and aerosol mass concentration over each of the regions. The warming response to a decrease in SO2, BC, and OC is strongest in the US and Europe perturbation simulations, both globally and regionally, with Arctic warming up to 0.3 K due to a removal of US and European anthropogenic aerosol emissions alone; however, even emissions from regions more remote to the Arctic, such as South Asian aerosols, can significantly warm the Arctic up to 0.2 K. In most regions, temperatures are most sensitive to emissions perturbations within that region. Arctic warming is the most robust model response across the regional aerosol emissions perturbations. 

How to cite: Westervelt, D., Zhang, Y., Amooli, J. A., Tsigaridis, K., Nazarenko, L., Samset, B., Wilcox, L., and Allen, R.: Enhanced aerosol-induced near-term Arctic warming due to remote regional aerosol perturbations in RAMIP, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-20722, https://doi.org/10.5194/egusphere-egu24-20722, 2024.