Abstract
African Easterly Waves (AEWs) impact Sahel rainfall and tropical cyclones (TCs). Gaining a detailed understanding of AEW behavior within global climate models can yield higher confidence in Sahel rainfall and TC projected trends. This study uses a Hovmöller tracking technique to track AEWs at 850 hPa in three reanalysis products and simulations from the fifth phase of the Coupled Model Intercomparison Project (CMIP5). AEW track characteristics are compared between reanalysis and CMIP5 historical simulations to establish historical biases. The resolution of the models is found to be more important in reducing biases in northern track AEWs compared to southern track AEWs, but large biases exist in the genesis and dissipation of AEWs over land and ocean. The tracking technique was then applied to future simulations (Representative Concentration Pathway 8.5). Between 1980–2000 and 2080–2100, models project an average increase of 1.5 AEWs (range of − 5.0 to + 7.6 AEWs) in the northern track, including an increased frequency of higher intensity waves. Projections of southern track AEWs are more varied compared to the northern track, with a projected model mean decrease of 1.1 AEWs but with a range of − 11.5 to + 11.6 AEWs in individual models. There is an indication of a shift in seasonality of southern track AEWs towards the later summer months, which may impact the timing of the Atlantic TC season. No clear differences were found in projected changes between models characterized as having high or low biases in the historical period.
Similar content being viewed by others
References
Adachi Y, Yukimoto S, Deushi M, Obata A, Nakano H, Tanaka TY, Hosaka M, Sakami T, Yoshimura H, Hirabara M, Shindo E, Tsujino H, Mizuta R, Yabu S, Koshiro T, Ose T, Kitoh A (2013) Basic performance of a new earth system model of the Meteorological Research Institute (MRI-ESM1). Pap Meteorol Geophys 64:1–19
Bain CL, Williams KD, Milton SF, Heming JT (2014) Objective tracking of African easterly waves in Met Office models. Q J R Meteorol Soc 140:47–57
Bentsen M, Bethke I, Debernard JB, Iversen T, Kirkevag A, Seland O, Drange H, Roelandt C, Seierstad IA, Hoose C, Kristjansson JE (2013) The Norwegian earth system model, NorESM1-M—part 1: description and basic evaluation of the physical climate. Geosci Model Dev 6:687–720
Bi D, Dix M, Marsland SJ, O’Farrell S, Rashid HA, Uotila P, Hirst AC, Kowalczyk E, Golebiewski M, Sullivan A, Yan H, Hannah N, Franklin C, Sun Z, Vohralik P, Watterson I, Zhou X, Fiedler R, Collier M, Ma Y, Noonan J, Stevens L, Uhe P, Zhu H, Stephen M, Griffies RH, Harris C, Puri K (2013) The ACCESS coupled model: description, control climate and evaluation. Aust Meteorol Oceanogr J 63:41–64
Brammer A, Thorncroft CD (2015) Variability and evolution of African easterly wave structures and their relationship with tropical cyclogenesis over the Eastern Atlantic. Mon Weather Rev 143(12):4975–4995
Burpee RW (1972) The origin and structure of easterly waves in the lower troposphere of North Africa. J Atmos Sci 29:77–90
Burpee RW (1974) Characteristics of North African easterly waves during the summers of 1968 and 1969. J Atmos Sci 31:1556–1570
Camargo SJ (2013) Global and regional aspects of tropical cyclone activity in the CMIP5 models. J Clim 26:9880–9902
Carlson TN (1969) Some remarks on African disturbances and their progress over the tropical Atlantic. Mon Weather Rev 97:716–726
Chen TC, Wang SY, Clark AJ (2008) North Atlantic hurricanes contributed by African easterly waves north and south of the African easterly jet. J Clim 21:6767–6776
Cook KH (1999) Generation of the African easterly jet and its role in determining west African precipitation. J Clim 12:1165–1184
Diaconescu EP, Gachon P, Scinocca J, Laprise R (2015) Evaluation of daily precipitation statistics and monsoon onset/retreat over Western Sahel in multiple data sets. Clim Dyn 45:1325–1354
Diedhiou A, Janicot S, Viltard A, de Felice P, Laurent H (1999) Easterly wave regimes and associated convection over west Africa and tropical Atlantic: results from the NCEP/NCAR and ECMWF reanalyses. Clim Dyn 15:795–822
Donner LJ, Wyman BL, Hemler RS, Horowitz LW, Ming Y, Zhao M, Golaz JC, Ginoux P, Lin SJ, Schwarzkopf MD, Austin J, Alaka G, Cooke WF, Delworth TL, Freidenreich SM, Gordon CT, Griffies SM, Held IM, Hurlin WJ, Klein SA, Knutson TR, Langenhorst AR, Lee HC, Lin Y, Magi BI, Malyshev SL, Milly PCD, Naik V, Nath MJ, Pincus R, Ploshay JJ, Ramaswamy V, Seman CJ, Shevliakova E, Sirutis JJ, Stern WF, Stouffer RJ, Wilson RJ, Winton M, Wittenberg AT, Zeng F (2011) The dynamical core, physical parameterizations, and basic simulation characteristics of the atmospheric component AM3 of the GFDL global coupled model CM3. J Clim 24:3484–3519
Dunne JP, John JG, Adcroft AJ, Griffies SM, Hallberg RW, Shevliakova E, Stouffer RJ, Cooke W, Dunne KA, Harrison MJ, Krasting JP, Malyshev SL, Milly PCD, Phillipps PJ, Sentman LT, Samuels BL, Spelman MJ, Winton M, Wittenberg AT, Zadeh N (2012) GFDL’s ESM2 global coupled climate-carbon earth system models. part I: physical formulation and baseline simulation characteristics. J Clim 25:6646–6665
Dwyer JG, Camargo SJ, Sobel AH, Biasutti M, Emanuel KA, Vecchi GA, Zhao M, Tippett MK (2015) Projected twenty-first-century changes in the length of the tropical cyclone season. J Clim 28:6181–6192
Emanuel KA (2013) Downscaling CMIP5 climate models shows increased downscaling CMIP5 climate models shows increased tropical cyclone activity over the 21st century. Proc Natl Acad Sci 110:12219–12224
Fink AH, Reiner A (2003) Spatiotemporal variability of the relation between African easterly waves and west African squall lines in 1998 and 1999. J Geophys Res 108:4332–4348
Flaounas E, Bastin S, Janicot S (2011) Regional climate modelling of the 2006 west African monsoon: sensitivity to convection and planetary boundary layer parameterisation using wrf. Clim Dyn 36:1083–1105
Fujiwara M, Wright JS, Manney GL, Gray LJ, Anstey J, Birner T, Davis S, Gerber EP, Harvey VL, Hegglin MI, Homeyer CR, Knox JA, Krüger K, Lambert A, Long CS, Martineau P, Molod A, Monge-Sanz BM, Santee ML, Tegtmeier S, Chabrillat S, Tan DGH, Jackson DR, Polavarapu S, Compo GP, Dragani R, Ebisuzaki W, Harada Y, Kobayashi C, McCarty W, Onogi K, Pawson S, Simmons A, Wargan K, Whitaker JS, Zou CZ (2017) Introduction to the sparc reanalysis intercomparison project (s-rip) and overview of the reanalysis systems. Atmos Chem Phys 17(2):1417–1452
Giorgetta MA, Jungclaus J, Reick CH, Legutke S, Bader J, Böttinger M, Brovkin V, Crueger T, Esch M, Fieg K, Glushak K, Gayler V, Haak H, Hollweg HD, Ilyina T, Kinne S, Kornblueh L, Matei D, Mauritsen T, Mikolajewicz U, Mueller W, Notz D, Pithan F, Raddatz T, Rast S, Redler R, Roeckner E, Schmidt H, Schnur R, Segschneider J, Six KD, Stockhause M, Timmreck C, Wegner J, Widmann H, Wieners KH, Claussen M, Marotzke J, Stevens B (2013) Climate and carbon cycle changes from 1850 to 2100 in MPI-ESM simulations for the coupled model intercomparison project phase 5. J Adv Model Earth Syst 5:572–597
Goldenberg S, Shapiro L (1996) Physical mechanisms for the association of El niño and west African rainfall with Atlantic major hurricane activity. J Clim 9:1169–1187
Grist JP (2002) Easterly waves over Africa. Part I: the seasonal cycle and contrasts between wet and dry years. Mon Weather Rev 130:198–211
Hagos SM, Cook KH (2008) Ocean warming and late-twentieth-century Sahel drought and recovery. J Clim 212:3797–3814
Hall NMJ, Kiladis GN, Thorncroft CD (2006) Three-dimensional structure and dynamics of African easterly waves. Part II: dynamical modes. J Atmos Sci 63:2231–2245
Hannah WM, Aiyyer A (2017) Reduced african easterly wave activity with quadrupled CO\(_2\) in the superparameterized cesm. J Clim 30(20):8253–8274
Hodges KI, Hoskins BJ, Boyle J, Thorncroft C (2003) A comparison of recent reanalysis datasets using objective feature tracking: storm tracks and tropical easterly waves. Mon Weather Rev 131:2012–2037
Hopsch SB, Thorncroft CD, Hodges K, Aiyyer A (2007) West African storm tracks and their relationship to Atlantic tropical cyclones. J Clim 20:2468–2483
Hopsch SB, Thorncroft CD, Tyle KR (2010) Analysis of African easterly wave structures and their role in influencing tropical cyclogenesis. Mon Weather Rev 138:1399–1419
Kobayshi S, Ota Y, Harada Y, Ebita A, Moriya M, Onoda H, Onogi K, Kamahori H, Kobayashi C, Endo H, Miyaoka K, Takahashi K (2015) The JRA-55 reanalysis: general specifications and basic characteristics. J Meteorol Soc Jpn 93:5–48
Landsea CW, Gray WM (1992) The strong association between Western Sahelian monsoon rainfall and intense Atlantic hurricanes. J Clim 5:435–453
Lavaysse C, Diedhiou A, Laurent H, Lebel T (2006) African easterly waves and convective activity in wet and dry sequences of the west African monsoon. Clim Dyn 27(2):319–332
Martin ER, Thorncroft C (2015) Representation of African easterly waves in CMIP5 models. J Clim 28:7702–7715
Mathon V, Laurent H, Lebel T (2002) Mesoscale convective system rainfall in the Sahel. J Appl Meteorol 41:1081–1092
McCrary RR, Randall DA, Stan C (2014) Simulations of the West African monsoon with a superparameterized climate model. part II: African easterly waves. J Clim 27:8323–8341
Mekonnen A, Thorncroft CD, Aiyyer A (2006) Analysis of convection and its association with African easterly waves. J Clim 19:5405–5421
Pasch RJ, Avila LA (1994) Atlantic tropical systems of 1992. Mon Weather Rev 122:539–548
Rotstayn L, Collier M, Feng Y, Gordon H, O’Farrell S, Smith I, Syktus J (2010) Improved simulation of Australian climate and ENSO-related rainfall variability in a GCM with an interactive aerosol treatment. Int J Climatol 30:1067–1088
Russell JO, Aiyyer A, White JD, Hannah W (2017) Revisiting the connection between African easterly waves and Atlantic tropical cyclogenesis. Geophys Res Lett 44:587–595
Ruti PM, Dell’Aquila A (2010) The twentieth century African easterly waves in reanalysis systems and IPCC simulations, from intra-seasonal to inter-annual variability. Clim Dyn 35:1099–1117
Saha S, Moorthi S, Pan HL, Wu X, Wang J, Nadiga S, Tripp P, Kistler R, Woollen J, Behringer D, Liu H, Stokes D, Grumbine R, Gayno G, Wang J, Hou YT, Chuang HY, Juang HMH, Sela J, Iredell M, Treadon R, Kleist D, Delst PV, Keyser D, Derber J, Ek M, Meng J, Wei H, Yang R, Lord S, Dool HVD, Kumar A, Wang W, Long C, Chelliah M, Xue Y, Huang B, Schemm JK, Ebisuzaki W, Lin R, Xie P, Chen M, Zhou S, Higgins W, Zou CZ, Liu Q, Chen Y, Han Y, Cucurull L, Reynolds RW, Rutledge G, Goldberg M (2010) The NCEP climate forecast system reanalysis. Bull Am Meteorol Soc 91:1015–1057
Serra YL, Geil K (2017) Historical and projected Eastern Pacific and intra-Americas sea td-wave activity in a selection of IPCC ar5 models. J Clim 30(7):2269–2294
Simmons A, Uppala S, Dee D, Kobayashi S (2007) Era-Interim: New ECMWF reanalysis products from 1989 onwards. ECMWF Newslett 110:25–35
Skinner CB, Diffenbaugh NS (2013) The contribution of African easterly waves to monsoon precipitation in the CMIP3 ensemble. J Geophys Res Atmos 118:3590–3609
Skinner CB, Diffenbaugh NS (2014) Projected changes in African easterly wave intensity and track in response to greenhouse forcing. Proc Natl Acad Sci USA 111(19):6882–6887
Taylor KE, Stouffer RJ, Meehl GA (2012) An overview of CMIP5 and the experiment design. Bull Am Meteorol Soc 93:485–498
Thorncroft C, Hodges K (2001) African easterly wave variability and its relationship to Atlantic tropical cyclone activity. J Clim 14:1166–1179
Thorncroft CD, Hall NMJ, Kiladis GN (2008) Three-dimensional structure and dynamics of African easterly waves. Part III: genesis. J Atmos Sci 65:3596–3607
Vellinga M, Roberts M, Vidale PL, Mizielinski MS, Demory ME, Schiemann R, Strachan J, Bain C (2016) Sahel decadal rainfall variability and the role of model horizontal resolution. Geophys Res Lett 43(1):326–333
Ventrice MJ, Thorncroft CD, Janiga MA (2012) Atlantic tropical cyclogenesis: a three-way interaction between an African easterly wave, diurnally varying convection, and a convectively coupled atmospheric Kelvin wave. Mon Weather Rev 140:1108–1124
Voldoire A, Sanchez-Gomez E, y Melia DS, Decharme B, Cassou C, Senesi S, Valcke S, Beau I, Alias A, Chevallier M, Deque M, Deshayes J, Douville H, Fernandez E, Madec G, Maisonnave E, Moine MP, Planton S, Saint-Martin D, Szopa S, Tyteca S, Alkama R, Belamari S, Braun A, Coquart L, Chauvin F (2013) The CNRM-CM5.1 global climate model: description and basic evaluation. Clim Dyn 40:2091–2121
Volodin E, Dianskii N, Gusev A (2010) Simulating present-day climate with the INMCM4.0 coupled model of the atmospheric and oceanic general circulations. Izvestiya Atmos Ocean Phys 46:414–431
Watanabe M, Suzuki T, O’ishi R, Komuro Y, Watanabe S, Emori S, Takemura T, Chikira M, Ogura T, Sekiguchi M, Takata K, Yamazaki D, Yokohata T, Nozawa T, Hasumi H, Tatebe H, Kimoto M (2010) Improved climate simulation by MIROC5: mean states, variability, and climate sensitivity. J Clim 23:6312–6335
You Q, Min J, Zhang W, Pepin N, Kang S (2015) Comparison of multiple datasets with gridded precipitation observations over the Tibetan Plateau. Clim Dyn 45:791–806
Yukimoto S, Adachi Y, Hosaka M, Sakami T, Yoshimura H, Hirabara M, Tanaka TY, Shindo E, Tsujino H, Deushi M, Mizuta R, Yabu S, Obata A, Nakano H, Koshiro T, Ose T, Kitoh A (2012) A new global climate model of the Meteorological Research Institute: MRI-CGCM3-model description and basic performance. J Meteorol Soc Jpn 90A:23–64
Zhou T, Song F, Chen X (2013) Historical evolution of global and regional surface air temperature simulated by FGOALS-s2 and FGOALS-g2: how reliable are the model results? Adv Atmos Sci 30:638–657
Acknowledgements
The authors would like to thank two anonymous reviewers for insightful suggestions and comments that significantly enhanced this manuscript. We thank Alan Brammer for sharing the Hovmöller tracking algorithm and for his help in adjusting the settings for use within climate models. We acknowledge the World Climate Research Programme’s Working Group on Coupled Modelling, which is responsible for CMIP5, and thank the climate modeling groups for producing and making available their model output. For CMIP5, the U.S. Department of Energy’s Program for Climate Model Diagnosis and Intercomparison provides coordinating support and led development of software infrastructure in partnership with the Global Organization for Earth System Science Portals. ERA-Interim data is provided courtesy of the European Centre for Medium-Range Weather Forecasts. The JRA-55 reanalysis data is contributed by the Japan Meteorological Agency. CFSR data is graciously supplied by the National Centers for Environmental Prediction.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Brannan, A.L., Martin, E.R. Future characteristics of African Easterly Wave tracks. Clim Dyn 52, 5567–5584 (2019). https://doi.org/10.1007/s00382-018-4465-z
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00382-018-4465-z