Articles | Volume 16, issue 12
https://doi.org/10.5194/acp-16-7559-2016
© Author(s) 2016. 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-16-7559-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
21 Jun 2016
Research article |
| 21 Jun 2016
Strong modification of stratospheric ozone forcing by cloud and sea-ice adjustments
Department of Atmospheric and Oceanic Sciences, McGill University,
Montréal, Canada
Yongyun Hu
Department of Atmospheric and Oceanic Sciences, Peking University,
Beijing, China
Department of Atmospheric and Oceanic Sciences, McGill University,
Montréal, Canada
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A. Jones, J. Haywood, O. Boucher, B. Kravitz, and A. Robock
Atmos. Chem. Phys., 10, 5999–6006, https://doi.org/10.5194/acp-10-5999-2010, https://doi.org/10.5194/acp-10-5999-2010, 2010
A. I. Jonsson, V. I. Fomichev, and T. G. Shepherd
Atmos. Chem. Phys., 9, 8447–8452, https://doi.org/10.5194/acp-9-8447-2009, https://doi.org/10.5194/acp-9-8447-2009, 2009
Cited articles
Bekki, S., Bodeker, G. E., Bais, A. F., Butchart, N., Eyring, V., Fahey, D. W., Kinnison, D. E., Langematz, U., Mayer, B., Portmann, R. W., Rozanov, E., Braesicke, P., Charlton-Perez, A. J., Chubarova, N. E., Cionni, I., Diaz, S. B., Gillett, N. P., Giorgetta, M. A., Komala, N., Lefèvre, F., McLandress, C., Perlwitz, J., Peter, T., and Shibata, K.: Future ozone and its impact on surface UV, Chapter 3, in: Scientific Assessment of Ozone Depletion: 2010, Global Ozone Research and Monitoring Project – Report No. 52, World Meteorological Organization, Geneva, Switzerland, 516 pp., 2011.
Bitz, C. M. and Polvani, L. M.: Antarctic climate response to stratospheric ozone depletion in a fine resolution ocean climate model, Geophys. Res. Lett., 39, L20705, https://doi.org/10.1029/2012GL053393, 2012.
Briegleb, B. P., Bitz, C. M., Hunke, E. C., Lipscomb, W. H., Holland, M. M., Schramm, J. L., and Moritz, R. E.: Scientific description of the sea ice component in the Community Climate System Model, Version Three, Tech., NCAR/TN-463STR, National Center for Atmospheric Research, Boulder, CO, 70 pp., 2004.
Ceppi, P. and Hartmann, D. L.: Connections Between Clouds, Radiation, and Midlatitude Dynamics: a Review, Current Climate Change Reports, 1, 94–102, https://doi.org/10.1007/s40641-015-0010-x, 2015.
Ceppi, P., Zelinka, M. D., and Hartmann, D. L.: The response of the Southern Hemispheric eddy-driven jet to future changes in shortwave radiation in CMIP5, Geophys. Res. Lett., 41, 3244–3250, 2014.
Collins, W. D., Rasch, P. J., Boville, B. A., Hack, J. J., McCaa, J. R., Williamson, D. L., Briegleb, B. P., Bitz, C. M., Lin, S. J., and Zhang, M. H.: The formulation and atmospheric simulation of the Community Atmosphere Model version 3 (CAM3), J. Climate, 19, 2144–2161, 2006.
Conley, A. J., Lamarque, J.-F., Vitt, F., Collins, W. D., and Kiehl, J.: PORT, a CESM tool for the diagnosis of radiative forcing, Geosci. Model Dev., 6, 469–476, https://doi.org/10.5194/gmd-6-469-2013, 2013.
Cronin, T. W.: On the Choice of Average Solar Zenith Angle, J. Atmos. Sci., 71, 2994–3003, 2014.
Danabasoglu, G. and Gent, P. R.: Equilibrium Climate Sensitivity: Is It Accurate to Use a Slab Ocean Model?, J. Climate, 22, 2494–2499, 2009.
Dee, D. P., Uppala, S. M., Simmons, A. J., Berrisford, P., Poli, P., Kobayashi, S., Andrae, U., Balmaseda, M. A., Balsamo, G., Bauer, P., Bechtold, P., Beljaars, A. C. M., van de Berg, L., Bidlot, J., Bormann, N., Delsol, C., Dragani, R., Fuentes, M., Geer, A. J., Haimberger, L., Healy, S. B., Hersbach, H., Holm, E. V., Isaksen, L., Kallberg, P., Kohler, M., Matricardi, M., McNally, A. P., Monge-Sanz, B. M., Morcrette, J. J., Park, B. K., Peubey, C., de Rosnay, P., Tavolato, C., Thepaut, J. N., and Vitart, F.: The ERA-Interim reanalysis: configuration and performance of the data assimilation system, Q. J. Roy. Meteor. Soc., 137, 553–597, 2011.
Flato, G. M. and Hibler, W. D.: On a simple sea-ice dynamics model for climate studies, Ann. Glaciol., 14, 72–77, 1990.
Flato, G. M. and Hibler, W. D.: Modeling pack ice as a cavitating fluid, J. Phys. Oceanogr., 22, 626–651, 1992.
Forster, P. M. D. and Shine, K. P.: Radiative forcing and temperature trends from stratospheric ozone changes, J. Geophys. Res.-Atmos., 102, 10841–10855, 1997.
Grise, K. M. and Polvani, L. M.: Southern Hemisphere Cloud-Dynamics Biases in CMIP5 Models and Their Implications for Climate Projections, J. Climate, 27, 6074–6092, 2014.
Grise, K. M., Polvani, L. M., Tselioudis, G., Wu, Y., and Zelinka, M. D.: The ozone hole indirect effect: Cloud-radiative anomalies accompanying the poleward shift of the eddy-driven jet in the Southern Hemisphere, Geophys. Res. Lett., 40, 3688–3692, https://doi.org/10.1002/grl.50675, 2013.
Hansen, J., Sato, M., Ruedy, R., Nazarenko, L., Lacis, A., Schmidt, G. A., Russell, G., Aleinov, I., Bauer, M., Bauer, S., Bell, N., Cairns, B., Canuto, V., Chandler, M., Cheng, Y., Del Genio, A., Faluvegi, G., Fleming, E., Friend, A., Hall, T., Jackman, C., Kelley, M., Kiang, N., Koch, D., Lean, J., Lerner, J., Lo, K., Menon, S., Miller, R., Minnis, P., Novakov, T., Oinas, V., Perlwitz, J., Perlwitz, J., Rind, D., Romanou, A., Shindell, D., Stone, P., Sun, S., Tausnev, N., Thresher, D., Wielicki, B., Wong, T., Yao, M., and Zhang, S.: Efficacy of climate forcings, J. Geophys. Res.-Atmos., 110, D18104, https://doi.org/10.1029/2005JD005776, 2005.
Hu, Y., Xia, Y., and Fu, Q.: Tropospheric temperature response to stratospheric ozone recovery in the 21st century, Atmos. Chem. Phys., 11, 7687–7699, https://doi.org/10.5194/acp-11-7687-2011, 2011.
Hu, Y., Xia, Y., Liu, J., and Huang, Y.: Stratospheric ozone-induced indirect radiative effects on Antarctic sea ice, Nature, in preparation, 2016.
Huang, Y.: On the Longwave Climate Feedbacks, J. Climate, 26, 7603–7610, 2013.
Huang, Y. and Zhang, M. H.: The implication of radiative forcing and feedback for meridional energy transport, Geophys. Res. Lett., 41, 1665–1672, 2014.
Huang, Y., Zhang, M. H., Xia, Y., Hu, Y. Y., and Son, S. W.: Is there a stratospheric radiative feedback in global warming simulations?, Clim. Dynam., 46, 177–186, 2016.
Jenkins, G. S.: Examining the sensitivity of Earth's climate to the removal of ozone, landmasses and enhanced ocean heat transport in the GENESIS global climate model, Global Planet. Change, 20, 257–279, 1999.
Kay, J. E., Hillman, B. R., Klein, S. A., Zhang, Y., Medeiros, B., Pincus, R., Gettelman, A., Eaton, B., Boyle, J., Marchand, R., and Ackerman, T. P.: Exposing Global Cloud Biases in the Community Atmosphere Model (CAM) Using Satellite Observations and Their Corresponding Instrument Simulators, J. Climate, 25, 5190–5207, 2012.
Kay, J. E., Medeiros, B., Hwang, Y. T., Gettelman, A., Perket, J., and Flanner, M. G.: Processes controlling Southern Ocean shortwave climate feedbacks in CESM, Geophys. Res. Lett., 41, 616–622, 2014.
Kiehl, J. T., Shields, C. A., Hack, J. J., and Collins, W. D.: The climate sensitivity of the Community Climate System Model version 3 (CCSM3), J. Climate, 19, 2584–2596, 2006.
Koll, D. D. B. and Abbot, D. S.: Why Tropical Sea Surface Temperature is Insensitive to Ocean Heat Transport Changes, J. Climate, 26, 6742–6749, 2013.
Lacis, A. A., Wuebbles, D. J., and Logan, J. A.: Radiative Forcing of Climate by Changes in the Vertical-Distribution of Ozone, J. Geophys. Res.-Atmos., 95, 9971–9981, 1990.
Macintosh, C. R., Allan, R. P., Baker, L. H., Bellouin, N., Collins, W., Mousavi, Z., and Shine, K. P.: Contrasting fast precipitation responses to tropospheric and stratospheric ozone forcing, Geophys. Res. Lett., 43, 1263–1271, https://doi.org/10.1002/2015GL067231, 2016.
McLandress, C., Perlwitz, J., and Shepherd, T. G.: Comment on “Tropospheric temperature response to stratospheric ozone recovery in the 21st century” by Hu et al. (2011), Atmos. Chem. Phys., 12, 2533–2540, https://doi.org/10.5194/acp-12-2533-2012, 2012.
Mlawer, E. J., Taubman, S. J., Brown, P. D., Iacono, M. J., and Clough, S. A.: Radiative transfer for inhomogeneous atmospheres: RRTM, a validated correlated-k model for the longwave, J. Geophys. Res.-Atmos., 102, 16663–16682, 1997.
Myhre, G., Shindell, D., Bréon, F.-M., Collins, W., Fuglestvedt, J., Huang, J., Koch, D., Lamarque, J.-F., Lee, D., Mendoza, B., Nakajima, T., Robock, A., Stephens, G., Takemura, T., and Zhang, H.: Anthropogenic and Natural Radiative Forcing, in: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, edited by: Stocker, T. F., Qin, D., Plattner, G.-K., Tignor, M., Allen, S. K., Boschung, J., Nauels, A., Xia, Y., Bex, V., and Midgley, P. M., Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, 659–740, 2013.
Neale, R. B., Chen, C.-C., Gettelman, A., Lauritzen, P. H., Park, S., Williamson, D. L., Conley, A. J., Garcia, R., Kinnison, D., and Lamarque, J.-F.: Description of the NCAR community atmosphere model (CAM 5.0), NCAR Tech. Note NCAR/TN-486+ STR, 2010.
Nowack, P. J., Abraham, N. L., Maycock, A. C., Braesicke, P., Gregory, J. M., Joshi, M. M., Osprey, A., and Pyle, J. A.: A large ozone-circulation feedback and its implications for global warming assessments, Nature Climate Change, 5, 41–45, https://doi.org/10.1038/nclimate2451, 2015.
Ramanathan, V. and Dickinson, R. E.: Role of Stratospheric Ozone in the Zonal and Seasonal Radiative Energy-Balance of the Earth-Troposphere System, J. Atmos. Sci., 36, 1084–1104, 1979.
Shell, K. M., Kiehl, J. T., and Shields, C. A.: Using the radiative kernel technique to calculate climate feedbacks in NCAR's Community Atmospheric Model, J. Climate, 21, 2269–2282, 2008.
Sigmond, M. and Fyfe, J. C.: Has the ozone hole contributed to increased Antarctic sea ice extent?, Geophys. Res. Lett., 37, L18502, https://doi.org/10.1029/2010GL044301, 2010.
Smith, K. L., Polvani, L. M., and Marsh, D. R.: Mitigation of 21st century Antarctic sea ice loss by stratospheric ozone recovery, Geophys. Res. Lett., 39, L20701, https://doi.org/10.1029/2012GL053325, 2012.
Thompson, D. W. J., Solomon, S., Kushner, P. J., England, M. H., Grise, K. M., and Karoly, D. J.: Signatures of the Antarctic ozone hole in Southern Hemisphere surface climate change, Nat. Geosci., 4, 741–749, 2011.
WMO: Scientific Assessment of Ozone Depletion: 2006, Global Ozone Research and Monitoring Project-Report No. 50, Geneva, Switzerland, 572 pp., 2007.
WMO: Scientific Assessment of Ozone Depletion: 2010, Global Ozone Research and Monitoring Project-Report No. 52, Geneva, Switzerland, 516 pp., 2011.
Yang, J., Hu, Y., and Peltier, W. R.: Radiative effects of ozone on the climate of a Snowball Earth, Clim. Past, 8, 2019–2029, https://doi.org/10.5194/cp-8-2019-2012, 2012.
Zhang, M. H. and Huang, Y.: Radiative Forcing of Quadrupling CO2, J. Climate, 27, 2496–2508, 2014.
Short summary
In this work, we discover a strong cloud radiative adjustment that affects the sign of the global surface temperature change in response to stratospheric ozone forcing. We believe this discovery is both interesting, in that our GCM experiments show that a global cooling can result from a warming forcing, and new, in that a strong cloud adjustment to ozone forcing, to the best of our knowledge, has not being documented before.
In this work, we discover a strong cloud radiative adjustment that affects the sign of the...
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