La Niña diversity and Northwest Indian Ocean Rim teleconnections
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The differences in tropical Pacific sea surface temperature (SST) expressions of El Niño-Southern Oscillation (ENSO) events of the same phase have been linked with different global atmospheric circulation patterns. This study examines the dynamical forcing of precipitation during October–December (OND) and March–May (MAM) over East Africa and during December–March (DJFM) over Central-Southwest Asia for 1950–2010 associated with four tropical Pacific SST patterns characteristic of La Niña events, the cold phase of ENSO. The self-organizing map method along with a statistical distinguishability test was used to isolate La Niña events, and seasonal precipitation forcing was investigated in terms of the tropical overturning circulation and thermodynamic and moisture budgets. Recent La Niña events with strong opposing SST anomalies between the central and western Pacific Ocean (phases 3 and 4), force the strongest global circulation modifications and drought over the Northwest Indian Ocean Rim. Over East Africa during MAM and OND, subsidence is forced by an enhanced tropical overturning circulation and precipitation reductions are exacerbated by increases in moisture flux divergence. Over Central-Southwest Asia during DJFM, the thermodynamic forcing of subsidence is primarily responsible for precipitation reductions, with moisture flux divergence acting as a secondary mechanism to reduce precipitation. Eastern Pacific La Niña events in the absence of west Pacific SST anomalies (phases 1 and 2), are associated with weaker global teleconnections, particularly over the Indian Ocean Rim. The weak regional teleconnections result in statistically insignificant precipitation modifications over East Africa and Central-Southwest Asia.
KeywordsENSO diversity La Niña Tropical warm pool Drought East Africa Central-Southwest Asia
The authors would like to thank two anonymous reviewers whose comments and suggestions helped to improve the manuscript and Martin Hoerling for providing the GFS simulations. NCEP Reanalysis and ERSST data were provided by the NOAA/OAR/ESRL PSD, Boulder, Colorado, USA, from their web site at http://www.esrl.noaa.gov/psd/. This research builds upon a multi-year research project carried out under a US Agency for International Development-funded Famine Early Warning Systems Network agreement with the US Geological Survey.
- Becker A, Finger P, Meyer-Christoffer A, Rudolf B, Schamm K, Schneider U, Ziese M (2013) A description of the global land-surface precipitation data products of the global precipitation climatology centre with sample applications including centennial (trend) analysis from 1901present. Earth Syst Sci Data 5(1):71–99. doi: 10.5194/essd-5-71-2013 CrossRefGoogle Scholar
- Hoell A, Funk C (2013) The ENSO-related west pacific sea surface temperature gradient. J Clim. doi: 10.1175/JCLI-D-12-00344.1
- Hoell A, Funk C, Barlow M (2013) The regional forcing of northern hemisphere drought during recent warm tropical west pacific ocean la nina events. Clim Dyn. doi: 10.1007/s00382-013-1799-4
- Holton JR (2004) An introduction to dynamic meteorology. Elsevier, AmsterdamGoogle Scholar
- Indeje M, Semazzi FH, Ogallo LJ (2000) ENSO signals in east african rainfall seasons. Int J Climatol 20(1):19–46. doi: 10.1002/(SICI)1097-0088(200001)20:1<19::AID-JOC449>3.0.CO;2-0 CrossRefGoogle Scholar
- 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 Am Meteorol Soc 77(3):437–471. doi: 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2 CrossRefGoogle Scholar
- Lyon B, Barnston A, DeWitt D (2013) Tropical pacific forcing of a 19981999 climate shift: observational analysis and climate model results for the boreal spring season. Clim Dyn 1–17. doi: 10.1007/s00382-013-1891-9
- Nicholson SE (1996) A review of climate dynamics and climate variability in eastern africa. In: Johnson TC, Odada EO (eds) The limnology, climatology and paleoclimatology of the East African Lakes. Overseas Publishers Association, pp 25–56Google Scholar
- Ratnam J, Behera S, Masumoto Y, Takahashi K, Yamagata T (2011) Anomalous climatic conditions associated with the el nino modoki during boreal winter of 2009. Clim Dyn 1–12. doi: 10.1007/s00382-011-1108-z
- Rienecker MM, Suarez MJ, Gelaro R, Todling R, Bacmeister J, Liu E, Bosilovich MG, Schubert SD, Takacs L, Kim GK, Bloom S, Chen J, Collins D, Conaty A, da Silva A, Gu W, Joiner J, Koster RD, Lucchesi R, Molod A, Owens T, Pawson S, Pegion P, Redder CR, Reichle R, Robertson FR, Ruddick AG, Sienkiewicz M, Woollen J (2011) MERRA: NASAs modern–era retrospective analysis for research and applications. J Clim 24(14):3624–3648. doi: 10.1175/JCLI-D-11-00015.1 CrossRefGoogle Scholar