23
Richter I, Xie SP (2008) On the origin of equatorial Atlantic biases
in coupled general circulation models. Clim Dyn 31(5):587–598.
https://doi.org/10.1007/s00382-008-0364-z
Richter I, Xie SP, Wittenberg AT et al (2012) Tropical Atlantic biases
and their relation to surface wind stress and terrestrial precipitation. Clim Dyn 38(5–6):985–1001. https://doi.org/10.1007/
s00382-011-1038-9
Richter I, Behera SK, Masumoto Y et al (2013) Multiple causes of interannual sea surface temperature variability in the equatorial Atlantic
Ocean. Nat Geosci 6(1):43–47. https://doi.org/10.1038/ngeo1660
Richter I, Behera SK, Doi T et  al (2014a) What controls equatorial
Atlantic winds in boreal spring? Clim Dyn 43(11):3091–3104.
https://doi.org/10.1007/s00382-014-2170-0
Richter I, Xie SP, Behera SK et  al (2014b) Equatorial Atlantic variability and its relation to mean state biases in CMIP5. Clim Dyn
42(1–2):171–188. https://doi.org/10.1007/s00382-012-1624-5
Richter I, Xie SP, Morioka Y et  al (2016) Phase locking of equatorial Atlantic variability through the seasonal migration of the
ITCZ.  Clim Dyn 48(11–12):3615–3629. https://doi.org/10.1007/
s00382-016-3289-y
Richter I, Doi T, Behera SK et al (2017) On the link between mean state
biases and prediction skill in the tropics: an atmospheric perspective.
Clim Dyn 50:3355. https://doi.org/10.1007/s00382-017-3809-4
Risien CM, Chelton DB (2008) A global climatology of surface
wind and wind stress fields from eight years of QuikSCAT scatterometer data. J  Phys Oceanogr 38(11):2379–2413. https://doi.
org/10.1175/2008JPO3881.1
Rodríguez-Fonseca B, Janicot S, Mohino E et al (2011) Interannual and
decadal SST-forced responses of the West African monsoon. Atmos
Sci Lett 12(1):67–74. https://doi.org/10.1002/asl.308
Roeckner E, Bäuml G, Bonaventura L et  al (2003) The atmospheric
general circulation model ECHAM5: part 1: model description.
MPI Report 349. https://doi.org/10.1029/2010JD014036
Roemmich D, Johnson GC, Riser S et  al (2009) The Argo program. Oceanography 22(2):34–43. https://doi.org/10.5670/
oceanog.2009.36
Schott FA, Dengler M, Brandt P et  al (2003) The zonal currents and
transports at 35°W in the tropical Atlantic. Geophys Res Lett
30(7):1349. https://doi.org/10.1029/2002GL016849
Sein DV, Danilov S, Biastoch A et  al (2016) Designing variable
ocean model resolution based on the observed ocean variability. J  Adv Model Earth Syst 8(2):904–916. https://doi.
org/10.1002/2016MS000650
Seo H, Jochum M, Murtugudde R et al (2006) Effect of ocean mesoscale
variability on the mean state of tropical Atlantic climate. Geophys
Res Lett 33(9):L09606. https://doi.org/10.1029/2005GL025651
Siongco AC, Hohenegger C, Stevens B (2015) The Atlantic ITCZ
bias in CMIP5 models. Clim Dyn 45(5):1169–1180. https://doi.
org/10.1007/s00382-014-2366-3
Stockdale TN, Balmaseda MA, Vidard A (2006) Tropical Atlantic
SST prediction with coupled ocean-atmosphere GCMs. J  Clim
19(23):6047–6061. https://doi.org/10.1175/JCLI3947.1
Sutton RT, Jewson SP, Rowell DP (2000) The elements of climate variability in the tropical Atlantic region. J Clim 13(18):3261–3284
Taylor KE, Stouffer RJ, Meehl GA (2012) An overview of CMIP5
and the experiment design. Bull Am Meteorol Soc 93(4):485–498.
https://doi.org/10.1175/BAMS-D-11-00094.1
Tozuka T, Doi T, Miyasaka T et  al (2011) Key factors in simulating
the equatorial Atlantic zonal sea surface temperature gradient
in a coupled general circulation model. J  Geophys Res Oceans
116(6):C06010. https://doi.org/10.1029/2010JC006717
Trenberth KE, Caron JM (2001) Estimates of meridional atmosphere
and ocean heat transports. J Clim 14(16):3433–3443
Trenberth KE, Fasullo JT, Kiehl J (2009) Earth’s global energy budget.
Bull Am Meteorol Soc 90(3):311–323. https://doi.org/10.1175/200
8BAMS2634.1
Voldoire A, Claudon M, Caniaux G et  al (2014) Are atmospheric
biases responsible for the tropical Atlantic SST biases in the
CNRM-CM5 coupled model? Clim Dyn 43(11):2963–2984. https://
doi.org/10.1007/s00382-013-2036-x
Wahl S, Latif M, Park W et al (2011) On the tropical Atlantic SST warm
bias in the Kiel climate model. Clim Dyn 36(5–6):891–906. https://
doi.org/10.1007/s00382-009-0690-9
Wang F, Chang P (2008) Coupled variability and predictability in a stochastic climate model of the tropical Atlantic. J Clim 21(23):6247–
6259. https://doi.org/10.1175/2008JCLI2283.1
Xie SP (2004) The shape of continents, air-sea interaction, and the
rising branch of the Hadley circulation. In: Diaz HF, Bradley RS
(eds) The Hadley circulation: present, past and future. Springer,
Dordrecht, pp 121–152
Xie P, Arkin PA (1997) Global precipitation: a 17-year monthly analysis based on gauge observations, satellite estimates, and numerical
model outputs. Bull Am Meteorol Soc 78(11):2539–2558. https://
doi.org/10.1175/1520-0477(1997)078<2539:GPAYMA>2.0.CO;2
Xie SP, Carton JA (2004) Tropical Atlantic variability: patterns,
mechanisms, and impacts. In: Wang C, Xie SP, Carton JA (eds)
Earth’s climate: the ocean-atmosphere interaction. American
Geophysical Union, Washington, DC, pp  121–142. https://doi.
org/10.1029/147GM07
Xie SP, Philander SGH (1994) A coupled ocean-atmosphere model of
relevance to the ITCZ in the eastern Pacific. Tellus A 46(4):340–
350. https://doi.org/10.1034/j.1600-0870.1994.t01-1-00001.x
Xu Z, Chang P, Richter I et  al (2014) Diagnosing southeast tropical Atlantic SST and ocean circulation biases in the CMIP5
ensemble. Clim Dyn 43(11):3123–3145. https://doi.org/10.1007/
s00382-014-2247-9
Zebiak SE (1993) Air-sea interaction in the equatorial Atlantic region.
J Clim 6(8):1567–1586
Zermeño-Diaz DM, Zhang C (2013) Possible root causes of surface westerly biases over the equatorial Atlantic in global climate models. J  Clim 26(20):8154–8168. https://doi.org/10.1175/
JCLI-D-12-00226.1
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