SSiRC
Stratospheric Sulfur and its Role in Climate

About SSiRC

SSiRC is an established SPARC (Stratosphere-Troposphere Processes and their role in Climate) activity, with SPARC being a core project within the World Climate Research Program (WCRP). SSiRC aims to foster collaboration across observational and modelling groups to better understand the stratospheric aerosol layer and the drivers for its observed variations. The abrupt volcanic enhancements of the stratospheric aerosol concentrations cause strong solar dimming and thereby surface cooling with important changes in circulation and atmospheric composition in response. SSiRC key science questions link with several foci of the WCRP grand challenges. The stratospheric aerosol layer was discovered 60 years ago, but it still poses us riddles. Aerosol above 15 km forms an optically thin veil with a small well characterized impact on climate, but then, in explosive episodes, it can intensify dramatically due to massive, aperiodic volcanic eruptions. Following such events, the stratospheric aerosol influences Earth's climate by cooling the planet as a whole and creates potentially devastating changes to regional weather patterns, such as winter warming in the Northern Hemisphere and reducing summer monsoon rainfall over Africa and Asia. It also increases the probability of an El Niño in the following Northern Hemisphere winter. In the modern era, large volcanic events can temporarily slow the pace of anthropogenic global warming.

Open Questions

While much is understood about the impact of stratospheric aerosol on climate, there are a number of open questions relevant to SSiRC, SPARC and the WCRP:
What is the uncertainty associated with estimates of aerosol properties such as aerosol optical depth over the satellite era, and what are the uncertainties at scales from the 1991 Pinatubo eruption to background levels?
Space-based measurements provide a record of microphysical and optical properties of stratospheric aerosol with good time resolution and near global coverage. But significant uncertainties as well as discrepancies between observations from different instruments still exist and need to be understood. New satellite missions are urgently needed as the future of space-based measurements beyond 2020 is uncertain.

Goals

By addressing these questions, SSiRC aims at better constraining the pathways of stratospheric aerosol and its precursors from emission to radiative forcing. By raising these questions and highlighting their importance, SSiRC stimulates research in this area, research that is relevant to WCRP's mission. SSiRC enables the assessment of our understanding the role of stratospheric aerosol in climate including the potential for catastrophic climate impacts following a major volcanic event, and decoupling more moderate climate changes in the stratospheric aerosol burden from those attributable to human activities. SSiRC builds a community from different fields of study and fosters collaboration. SSiRC connects to other WCRP/SPARC activities including ACAM, OCTV-UTLS and CCMI.

Science Steering Group

Landon Rieger
University of Saskatchewan
Mark von Hobe
Forschungszentrum Jülich
Anja Schmidt
Deutsches Zentrum für Luft- und Raumfahrt
Juan Carlos Antuña
Departamento de Física Teórica
Andrew Rollins
NOAA
Corinna Kloss
Forschungszentrum Jülich
Terry Deshler
University of Colorado
Jean-Paul Vernier
NASA Langley Research Center
Mahesh Kovilakam
Science Systems Applications Inc.
Graham Mann
School of Earth and Environment
Yunqian Zhu
University of Colorado Boulder
Eduardo Landulfo
Instituto de Pesquisas Energéticas e Nucleares
Suvarna Fadnavis
Indian Institute of Tropical Meteorology
Contact

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Landon Rieger
University of Saskatchewan
landon.rieger@usask.ca