Articles | Volume 15, issue 10
https://doi.org/10.5194/acp-15-5827-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-15-5827-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Ocean mediation of tropospheric response to reflecting and absorbing aerosols
National Center for Atmospheric Research, Boulder, CO 80303, USA
S.-P. Xie
Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093, USA
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34 citations as recorded by crossref.
- Climatological patterns of subseasonal eddy flux transfer based on the co‐spectral analysis over the Indian region and the derivation of an index of eddy transfer for operational tracking M. Kalshetti et al. 10.1002/joc.6821
- Reassessing the relative role of anthropogenic aerosols and natural decadal variability in driving the mid-twentieth century global “cooling”: a focus on the latitudinal gradient of tropospheric temperature C. Diao & Y. Xu 10.1007/s00382-022-06235-y
- Impact of Asian aerosol forcing on tropical Pacific circulation and the relationship to global temperature trends L. Kuntz & D. Schrag 10.1002/2016JD025430
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- Changes in Extreme Rainfall Over India and China Attributed to Regional Aerosol‐Cloud Interaction During the Late 20th Century Rapid Industrialization L. Lin et al. 10.1029/2018GL078308
- Dynamics of Asian Summer Monsoon Response to Anthropogenic Aerosol Forcing H. Wang et al. 10.1175/JCLI-D-18-0386.1
- Larger Sensitivity of Precipitation Extremes to Aerosol Than Greenhouse Gas Forcing in CMIP5 Models L. Lin et al. 10.1029/2018JD028821
- Spatially similar surface energy flux perturbations due to greenhouse gases and aerosols G. Persad et al. 10.1038/s41467-018-05735-y
- Subsurface Ocean Temperature Responses to the Anthropogenic Aerosol Forcing in the North Pacific J. Shi et al. 10.1029/2022GL101035
- Responses of the East Asian summer monsoon to aerosol forcing in CMIP5 models: The role of upper‐tropospheric temperature change J. Mu & Z. Wang 10.1002/joc.6887
- Scattering and absorbing aerosols in the climate system J. Li et al. 10.1038/s43017-022-00296-7
- Anthropogenically Forced Decadal Change of South Asian Summer Monsoon Across the Mid‐1990s F. Luo et al. 10.1029/2018JD029195
- Seasonal Responses of Indian Summer Monsoon to Dust Aerosols in the Middle East, India, and China Q. Jin et al. 10.1175/JCLI-D-15-0622.1
- Equilibrium climate response of the East Asian summer monsoon to forcing of anthropogenic aerosol species Z. Wang et al. 10.1007/s13351-017-7059-5
- Strong Influence of Aerosol Reductions on Future Heatwaves A. Zhao et al. 10.1029/2019GL082269
- Detecting cross‐equatorial wind change as a fingerprint of climate response to anthropogenic aerosol forcing H. Wang et al. 10.1002/2016GL068521
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- Constraining Aging Processes of Black Carbon in the Community Atmosphere Model Using Environmental Chamber Measurements Y. Wang et al. 10.1029/2018MS001387
- The direct effects of black carbon aerosols from different source sectors in East Asia in summer B. Zhuang et al. 10.1007/s00382-019-04863-5
- The Role of Anthropogenic Aerosol Forcing in Interdecadal Variations of Summertime Upper‐Tropospheric Temperature Over East Asia Z. Wang et al. 10.1029/2018EF001052
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- The importance of aerosol scenarios in projections of future heat extremes Y. Xu et al. 10.1007/s10584-015-1565-1
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- Impacts of recent decadal changes in Asian aerosols on the East Asian summer monsoon: roles of aerosol–radiation and aerosol–cloud interactions B. Dong et al. 10.1007/s00382-019-04698-0
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Latest update: 12 Dec 2024
Short summary
Strong solar heating by absorbing aerosols (black carbon) is considered more effective in inducing atmospheric circulation change than reflecting aerosols (sulfate), which do not have direct atmospheric heating effect. Surprisingly, we show that reflecting aerosols induce tropospheric temperature and circulation response similar to that induced by absorbing aerosols. The common response is mediated by the ocean through SST gradient, a process overlooked so far in aerosol-climate connection.
Strong solar heating by absorbing aerosols (black carbon) is considered more effective in...
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