The Response of the Indian Ocean Dipole Asymmetry to Anthropogenic Aerosols and Greenhouse Gases
Article
Article Title | The Response of the Indian Ocean Dipole Asymmetry to Anthropogenic Aerosols and Greenhouse Gases |
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ERA Journal ID | 1978 |
Article Category | Article |
Authors | Cowan, Tim, Cai, Wenju, Ng, Benjamin and England, Matthew |
Journal Title | Journal of Climate |
Journal Citation | 28 (7), pp. 2564-2583 |
Number of Pages | 20 |
Year | 2015 |
Publisher | American Meteorological Society |
Place of Publication | United States |
ISSN | 0894-8755 |
1520-0442 | |
Digital Object Identifier (DOI) | https://doi.org/10.1175/JCLI-D-14-00661.1 |
Web Address (URL) | https://journals.ametsoc.org/view/journals/clim/28/7/jcli-d-14-00661.1.xml |
Abstract | The tropical Indian Ocean has experienced a faster warming rate in the west than in the east over the twentieth century. The warming pattern resembles a positive Indian Ocean dipole (IOD) that is well captured by climate models from phase 5 of the Coupled Model Intercomparison Project (CMIP5), forced with the two main anthropogenic forcings, long-lived greenhouse gases (GHGs), and aerosols. However, much less is known about how GHGs and aerosols influence the IOD asymmetry, including the negative sea surface temperature (SST) skewness in the east IOD pole (IODE). Here, it is shown that the IODE SST negative skewness is more enhanced by aerosols than by GHGs using single-factor forcing experiments from 10 CMIP5 models. Aerosols induce a greater mean zonal thermocline gradient along the tropical Indian Ocean than that forced by GHGs, whereby the thermocline is deeper in the east relative to the west. This generates strong asymmetry in the SST response to thermocline anomalies between warm and cool IODE phases in the aerosol-only experiments, enhancing the negative IODE SST skewness. Other feedback processes involving zonal wind, precipitation, and evaporation cannot solely explain the enhanced SST skewness by aerosols. An interexperiment comparison in one model with strong skewness confirms that the mean zonal thermocline gradient across the Indian Ocean determines the magnitude of the SST–thermocline asymmetry, which in turn controls the SST skewness strength. The findings suggest that as aerosol emissions decline and GHGs increase, this will likely contribute to a future weakening of the IODE SST skewness. |
Keywords | Aerosols; Climate variability; Climate sensitivity; Atmosphere-ocean interaction |
ANZSRC Field of Research 2020 | 370103. Atmospheric aerosols |
370201. Climate change processes | |
370803. Physical oceanography | |
Public Notes | File reproduced in accordance with the copyright policy of the publisher/author. |
Byline Affiliations | Commonwealth Scientific and Industrial Research Organisation (CSIRO), Australia |
University of New South Wales |
https://research.usq.edu.au/item/z09x6/the-response-of-the-indian-ocean-dipole-asymmetry-to-anthropogenic-aerosols-and-greenhouse-gases
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