Abstract
The present study focuses on the leading interannual mode of continental-scale atmospheric variability over South America, which is characterized by an equivalent barotropic vortex (referred to as VOSA in the text) centered over the eastern subtropical coast of the continent. The principal aim is to determine whether and in what season VOSA is the downstream extension of the leading Pacific South American mode (PSA1). Another objective is to examine the extent to which VOSA and PSA1 are forced by El Niño Southern Oscillation (ENSO). The research is based on examination of reanalysis data and output of experiments with an atmospheric general circulation model. The emphasis is on the southern spring, summer and fall seasons, during which VOSA modulates the interannual precipitation variability over the continent. A similar relationship is not found during the southern winter. It is found that VOSA is an integral part of PSA1 during spring and fall. In these seasons, PSA1/VOSA is originated primarily by large-scale atmospheric internal variability with the forcing by ENSO accounting for 14 and 8% of the total variance, respectively. During the southern summer season, when ENSO peaks, PSA1 is not a dominant mode of atmospheric variability, and VOSA primarily results from continental-scale internal variability.
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References
Aceituno P (1988) On the functioning of the Southern Oscillation in the South American sector. Part I Surface Clim Mon Wea Rev 116:505–524
Andreoli RV, Kayano MT (2005) ENSO-related rainfall anomalies in South America and associated circulation features during warm and cold Pacific decadal oscillation regimes. Int J Climatol 25:2017–2030. doi:10.1002/joc.1222
Barreiro M, Tippmann A (2008) Atlantic modulation of El Niño influence on summertime rainfall over southeastern South America. Geophys Res Lett 35:L16704. doi:10.1029/2008GL035019
Barreiro M (2009) Influence of ENSO and the south Atlantic ocean on climate predictability over Southeastern South America. Clim Dyn 35:1493–1508. doi:10.1007/s00382-009-0666-9
Bracco A, Kucharski F, Kallummal R, Molteni F (2004) Internal variability, external forcing and climate trends in multi-decadal AGCM ensembles. Clim Dyn 23:659–678
Cai W, Watterson IG (2002) Modes of interannual variability of the Southern Hemisphere circulation simulated by the CSIRO climate model. J Clim 15:1159–1174
Carril AF, Navarra A (2001) The interannual leading modes of the extratropical variability in the Southern Hemisphere simulated by the ECHAM-4 atmospheric model. Clim Dyn 18:1–16
Cazes-Boezio G, Robertson AW, Mechoso CR (2003) Seasonal Dependence of ENSO teleconnections over South America and relationships with precipitation over Uruguay. J Clim 16:1159–1176
Diaz A, Aceituno P (2003) Atmospheric circulation anomalies during episodes of enhanced and reduced convective cloudiness over Uruguay. J Clim 16:3171–3185
Garreaud RD, Battisti DS (1999) Interannual (ENSO) and interdecadal (ENSO-like) variability in the Southern Hemisphere tropospheric circulation. J Clim 12:2113–2123
Ghil M, Mo K (1991) Intraseasonal oscillations in the global atmosphere. Part II Southern Hemisphere. J Atmos Sci 48:780–790
Grimm AM, Ferraz SET, Gomes J (1998) Precipitation anomalies in Southern Brazil associated with El Niõ and La Niã events. J Clim 11:2863–2880
Grimm AM, Barros VR, Doyle ME (2000) Climate variability in Southern South America associated with El Niõ and La Niã events. J Clim 13:35–58
Grimm AM (2003) The El Niõ impact on the summer monsoon in Brazil) regional processes versus remote influences. J Clim 16:263–280
Grimm AM, Pal JS, Giorgi F (2007) Connection between spring conditions and peak summer monsoon rainfall in South America role of soil moisture, surface temperature, and topography in Eastern Brazil. J Clim 20:5929–5945
Herceg Bulic I, Brankovic C (2007) ENSO forcing of the Northern Hemisphere climate in a large ensemble of model simulations based on a very long SST record. Clim Dyn 28:231–254
Kalnay E, Kanamitsu M, Kistler R, Collins W, Deaven D, Gandin L, Iredell M, Saha S, White G, Woollen J, Zhu Y, Leetmaa A, Reynolds R, Chelliah M, Ebisuzaki W, Higgins W, Janowiak J, Mo KC, Ropelewski C, Wang J, Jenne R, Joseph D (1996) The NCEP/NCAR 40-year reanalysis project. Bull Amer Meteor Soc 77:437–470
Karoly DJ (1989) Southern Hemisphere circulation features associated with El Niõ-Southern Oscillation events. J Clim 2:1239–1252
Kidson JW (1988) Interannual variations in the Southern Hemisphere circulation. J Clim 1:1177–1198
Kidson JW (1999) Principal Modes of Southern Hemisphere low-frequency variability obtained from NCEP-NCAR reanalyses. J Clim 12:2808–2830
Kiladis GN, Mo KC (1998) Interannual and intraseasonal variability in the Southern Hemisphere. In: Karoly DJ, Vincent D (eds) The meteorology of the Southern Hemisphere. American Meteorological Society, Boston, pp 307–336
Kucharski F, Molteni F, Bracco A (2006) Decadal interactions between the Western Tropical Pacific and the North Atlantic Oscillation. Clim Dyn 26:79–91. doi:10.1007/s00382-005-0085-5
Kucharski F, Molteni F, Yoo JH (2006) SST forcing of decadal Indian monsoon rainfall variability. Geophys Res Lett 33:L03709. doi:10.10029/2005GL025371
Kucharski F, Bracco A, Yoo JH, Tompkins AM, Feudale L, Ruti P, Dell’Aquila A (2009) A Gill-Matsun-type mechanism explains the tropical Atlantic influence on African and Indian monsoon rainfall. Quart J R Met Soc 135:569–579. doi:10.1002/qj.406
Kucharski F, Bracco A, Barimalala R, Yoo JH (2010) Contribution of the east-wets thermal heating contrast to the South Asian Monsoon and consequences for its variability. Clim Dyn. doi:10.1007/s00382-010-0858-3
Lau KM, Sheu PJ, Kang IS (1994) Multiscale low-frequency circulation modes in the global atmosphere. J Atmos Sci 51:1169–1193
Mo KC, Ghil M (1987) Statistics and dynamics of persistent anomalies. J Atmos Sci 44:877–902
Mo KC, Higgins RW (1998) The Pacific-South American modes and tropical convection during the Southern Hemisphere winter. Mon Wea Rev 126:1581–1596
Mo KC (2000) Relationships between low-frequency variability in the Southern Hemisphere and Sea surface temperature anomalies. J Clim 13:3599–3610
Mo KC, Paegle JN (2001) The Pacific-South American modes and their downstream effects. Int J Climatol 21:1211–1229
Molteni F (2003) Atmospheric simulations using a GCM with simplified physical parametrizations. (I) Model climatology and variability in multi-decadal experiments. Clim Dyn 20:175–191
Montecinos A, Diaz A, Aceituno P (2002) Seasonal diagnostic and predictability of rainfall in subtropical South America based on tropical pacific SST. J Clim 13:746–758
Pisciottano GJ, Diaz AF, Cazes-Boezio G, Mechoso CR (1994) El Niõ-Southern Oscillation impact on rainfall in Uruguay. J Clim 7:1286–1302
Rao VB, Hada K (1990) Characteristics of rainfall over Brazil: annual variations and connections with the Southern Oscillation. Theor Appl Climatol 42:81–91
Rasmusson EM, Mo K (1993) Linkages between 200-mb tropical and extratropical circulation anomalies during the 1986–1989 ENSO cycle. J Clim 6:595–616
Robertson AW, Mechoso CR (2000) Interannual and interdecadal variability of the South Atlantic convergence zone. Mon Wea Rev 128:2947–2957
Robertson AW, Mechoso CR (2003) Circulation regimes and low-frequency oscillations in the South Pacific sector. Mon Wea Rev 131:1566–1576
Silvestri GE (2004) El Niõ signal variability in the precipitation over southeastern South America during austral summer. Geophys Res Lett 31:L18206. doi:10.1029/2004GL020590
Smith TM, Reynolds RW (2004) Improved extended reconstruction of SST (1854–1997). J Clim 17:2466–2477
Straus DM, Shukla J (2000) Distinguishing between the SST-forced variability and internal variability in mid latitudes. Analysis of observations and GCm simulations. Q J R Meteorol Soci 126:2323–2350
Yadav RK, Yoo JH, Kucharski F, Abid MA (2010) Why is ENSO influencing Northwest India winter precipitation in recent decades? J Clim 23:1979–1993
Zamboni L, Mechoso CR, Kucharski F (2010) Relationships between upper-level circulation over South America and rainfall over Southeastern South America. A physical base for seasonal predictions. J Clim 23(12):3300–3315
Zhou J, Lau KM (2001) Principal modes of interannual and decadal variability of summer rainfall over South America. Int J Climatol 21:1623–1644
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This research was supported by NOAA under grant NA05OAR4310009 and by the Abdus Salam International Centre for Theoretical Physics.
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Zamboni, L., Kucharski, F. & Mechoso, C.R. Seasonal variations of the links between the interannual variability of South America and the South Pacific. Clim Dyn 38, 2115–2129 (2012). https://doi.org/10.1007/s00382-011-1116-z
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DOI: https://doi.org/10.1007/s00382-011-1116-z