Robust Multiyear Climate Impacts of Volcanic Eruptions in Decadal Prediction Systems. Issue 9 (4th May 2020)

• Record Type: Journal Article
• Authors: Hermanson, Leon; Bilbao, Roberto; Dunstone, Nick; Ménégoz, Martin; Ortega, Pablo; Pohlmann, Holger; Robson, Jon I.; Smith, Doug M.; Strand, Gary; Timmreck, Claudia; Yeager, Steve; Danabasoglu, Gokhan
• Is Part Of: Journal of geophysical research. Volume 125:Issue 9(2020)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2020-05-04
• Subjects: climate -- volcano -- coupled model -- NAO -- ENSO; Atmospheric physics -- Periodicals; Geophysics -- Periodicals; 551.5
• DOI: 10.1029/2019JD031739
• Languages: English
• ISSNs: 2169-897X

Abstract

Abstract: Major tropical volcanic eruptions have a large impact on climate, but there have only been three major eruptions during the recent relatively well‐observed period. Models are therefore an important tool to understand and predict the impacts of an eruption. This study uses five state‐of‐the‐art decadal prediction systems that have been initialized with the observed state before volcanic aerosols are introduced. The impact of the volcanic aerosols is found by subtracting the results of a reference experiment where the volcanic aerosols are omitted. We look for the robust impact across models and volcanoes by combining all the experiments, which helps reveal a signal even if it is weak in the models. The models used in this study simulate realistic levels of warming in the stratosphere, but zonal winds are weaker than the observations. As a consequence, models can produce a pattern similar to the North Atlantic Oscillation in the first winter following the eruption, but the response and impact on surface temperatures are weaker than in observations. Reproducing the pattern, but not the amplitude, may be related to a known model error. There are also impacts in the Pacific and Atlantic Oceans. This work contributes toward improving the interpretation of decadal predictions in the case of a future large tropical volcanic eruption. Key Points: Models simulate an increased chance of a positive NAO in the first winter following a volcanic eruption In the first winter, zonal winds, mean sea‐level pressure, and surface temperature are weaker in the models than in the observations Models simulate an increased chance of a positive ENSO in the second winter following a volcanic eruption