The Fingerprint of Global Warming in the Tropical Pacific

Noel KEENLYSIDEand Dietmar DOMMENGET

1Geophysical Institute,University of Bergen/Bjerknes Center for Climate Research,Bergen 5007,Norway

2Nansen Environmental and Remote Sensing Center/Bjerknes Center for Climate Research,Bergen 5006,Norway

3ARC Centre of Excellence for Climate System Science,School of Earth,Atmosphere and Environment, Monash University,Clayton,VIC,Australia

The Fingerprint of Global Warming in the Tropical Pacific

Noel KEENLYSIDE∗1,2and Dietmar DOMMENGET3

1Geophysical Institute,University of Bergen/Bjerknes Center for Climate Research,Bergen 5007,Norway

2Nansen Environmental and Remote Sensing Center/Bjerknes Center for Climate Research,Bergen 5006,Norway

3ARC Centre of Excellence for Climate System Science,School of Earth,Atmosphere and Environment, Monash University,Clayton,VIC,Australia

The impacts of global warming will be felt most strongly at regional scales.However,great uncertainties exist in climate change projections at these scales,limiting our ability to provide useful information for the planning and implementation of appropriate adaptation measures.Thus,there is an urgent need to reduce these uncertainties.

What determines regional climate change and how can we reduce uncertainties in the future climate projections at these scales?The new article by Ying et al.(2016)(p433 in this issue)makes an important contribution towards addressing the first part of this question for the Tropical Pacific and provides a framework for addressing the second part.Understanding the mechanisms for climate change is essential to provide confidence in model based future projections,especially given that the models exhibit many common systematic errors.

The Tropical Pacific is a key region for global climate,as diabatic heating released there through precipitation powers the atmospheric general circulation.Changes in precipitation patterns in the Tropical Pacific can,through atmospheric teleconnections,impact climate in distant regions.Furthermore,precipitation patterns in this region are closely related to the underlying sea surface temperature.

How global warming will impact precipitation and SST patterns in the Tropical Pacific is a subject of great scientific debate.Thermodynamic arguments predict that global warming will lead to a weakening of the Walker Circulation.In particular,the increased moisture carrying capacity of a warmer atmosphere will firstly lead to increased evaporation and precipitation,in what is known as a wet gets wetter and dry gets drier mechanism.The resulting greater diabatic heating at upper levels will act to stabilize the atmosphere,weakening the increase in precipitation and as a consequence also the atmospheric general circulation(Held and Soden,2006).However,the wet gets wetter picture holds mostly over the oceans, and even there is not able to explain many of projected regional changes(Chadwick et al.,2013).In particular,the strong coupled nature of ocean-atmosphere interaction in the tropics may modify this picture,and more recently,a warmer gets wetter hypothesis has been put forward where increases in tropical precipitation are collocated with the regions of greatest warming(Xie et al.,2010).Dynamical interactions,such as the Bjerknes feedback,may also play an important role in shaping the changes in the Tropical Pacific(Bayr et al.,2014).

Ying et al.focus on understanding how global warming will impact the SST and consider the two most commonly discussed patterns:The Eastern Pacific SST Warming(EPSW)and the equatorial peak warming(EPW).For this purpose they use the model simulations performed for the IPCC AR5.The multi-model mean predicts an El Ni˜no-like warming.Going well beyond previous studies,they present a very careful analysis of the different terms driving upper ocean temperature in the multi-model ensemble mean.A key finding of their study is that the distribution of climatological latent heat flux is the most important term driving both the EPSW and EPW patterns.Ocean circulation changes tend to damp the EPSW,mostly through an equatorial upwelling feedback(Clement et al.,1996).In contrast,ocean circulation changes associated with a weakened Walker Circulation tend to enhance the EPW;this is a key difference to previous studies(Liu et al.,2005).

Importantly,Ying et al.(2016)'s approach can be extended to understand how model biases may impact the projected changes and to explain the factors causing the large intermodel spread.Such future work has the potential to reduce uncertainties in regional climate change in the Tropical Pacific,and in areas around the globe teleconnected to it.

REFERENCES

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Chadwick,R.,I.Boutle,and G.Martin,2013:Spatial patterns of precipitation change in CMIP5:Why the rich do not get richer in the tropics.J.Climate,26,3803-3822.

Clement,A.C.,R.Seager,M.A.Cane,and S.E.Zebiak,1996:An ocean dynamical thermostat.J.Climate,9,2190-2196.

Held,I.M.,and B.J.Soden,2006:Robust responses of the hydrological cycle to global warming.J.Climate,19,5686-5699.

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Ying,J.,P.Huang,and R.H.Huang,2016:Evaluating the formation mechanisms of the equatorial Pacific SST warming pattern in CMIP5 models.Adv.Atmos.Sci.,33(4),doi:10.1007/s00376-015-5184-6.

Keenlyside,N.and D.Dommenget,2016:The fingerprint of global warming in the Tropical Pacific. Adv.Atmos.Sci.,33(4),533-534,

10.1007/s00376-016-6014-1.

∗Noel KEENLYSIDE,noel.keenlyside@uib.no