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Climate mean, variability and dominant patterns of the Northern Hemisphere wintertime mean atmospheric circulation in the NCEP CFSv2

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Abstract

In this study, the climate mean, variability, and dominant patterns of the Northern Hemisphere wintertime mean 200 hPa geopotential height (Z200) in a CMIP and a set of AMIP simulations from the National Centers for Environmental Prediction (NCEP) Climate Forecast System Version 2 (CFSv2) are analyzed and compared with the NCEP/NCAR reanalysis. For the climate mean, it is found that a component of the bias in stationary waves characterized with wave trains emanating from the tropics into both the hemispheres can be attributed to the precipitation deficit over the Maritime continent. The lack of latent heating associated with the precipitation deficit may have served as the forcing of the wave trains. For the variability of the seasonal mean, both the CMIP and AMIP successfully simulated the geographical locations of the major centers of action, but the simulated intensity was generally weaker than that in the reanalysis, particularly for the center over the Davis Strait-southern Greenland area. It is also noted that the simulated action center over Aleutian Islands was southeastward shifted to some extent. The shift was likely caused by the eastward extension of the Pacific jet. Differences also existed between the CMIP and the AMIP simulations, with the center of actions over the Aleutian Islands stronger in the AMIP and the center over the Davis Strait-southern Greenland area stronger in the CMIP simulation. In the mode analysis, the El Nino-Southern Oscillation (ENSO) teleconnection pattern in each dataset was first removed from the data, and a rotated empirical orthogonal function (REOF) analysis was then applied to the residual. The purpose of this separation was to avoid possible mixing between the ENSO mode and those generated by the atmospheric internal dynamics. It was found that the simulated ENSO teleconnection patterns from both model runs well resembled that from the reanalysis, except for a small eastward shift. Based on the REOF modes of the residual data, six dominant modes of the reanalysis data had counterparts in each model simulation, though with different rankings in explained variance and some distortions in spatial structure. By evaluating the temporal coherency of the REOF modes between the reanalysis and the AMIP, it was found that the time series associated with the equatorially displaced North Atlantic Oscillation in the two datasets were significantly correlated, suggesting a potential predictability for this mode.

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References

  • Barnston A, Livezey RE (1987) Classification, seasonality and persistence of low-frequency circulation pattern. Mon Weather Rev 115:1083–1126

    Article  Google Scholar 

  • Branstator G (1992) The maintenance of low-frequency atmospheric anomalies. J Atmos Sci 49:1924–1946

    Article  Google Scholar 

  • Bretherton CS, Battisti DS (2000) An interpretation of the results from atmospheric general circulation models forced by the time history of the observed sea surface temperature distribution. Geophys Res Lett 27:767–770

    Article  Google Scholar 

  • DeWeaver E, Nigam S (2004) On the forcing of ENSO teleconnections by anomalous heating and cooling. J Clim 17:3225–3235

    Article  Google Scholar 

  • Fan M, Schneider E (2012) Observed decadal North Atlantic tripole SST variability. Part I: weather noise forcing and coupled response. J Atmos Sci 69:35–50

    Article  Google Scholar 

  • Frankignoul C (1985) Sea surface temperature anomalies, planetary waves and air–sea feedback in the middle latitudes. Rev Geophys 23:357–390

    Article  Google Scholar 

  • Gill A (1982) Atmosphere-ocean dynamics. Academic Press, London

    Google Scholar 

  • Held IM, Lyons SW, Nigam S (1989) Transients and the extratropical response to El Niño. J Atmos Sci 46:163–174

    Article  Google Scholar 

  • Held IM, Ting M, Wang H (2002) Northern winter stationary waves: theory and modeling. J Clim 15:2125–2144

    Article  Google Scholar 

  • Hoerling MP, Kumar A (2002) Atmospheric response patterns associated with tropical forcing. J Clim 15:2184–2203

    Google Scholar 

  • Hoerling MP, Kumar A, Zhong M (1997) El Niño, La Niña, and the nonlinearity of their teleconnections. J Clim 10:1769–1786

    Article  Google Scholar 

  • Horel JD (1981) A rotated Principal component analysis of the interannual variability of the northern hemisphere 500 mb height field. Mon Weather Rev 110:2080–2092

    Article  Google Scholar 

  • Hoskins BJ, James IN, White GH (1983) The shape, propagation and mean-flow interaction of large-scale weather systems. J Atmos Sci 40:1595–1612

    Article  Google Scholar 

  • Hu Z–Z, Huang B, Pegion K (2008) Low-cloud errors over the southeastern Atlantic in the NCEP CFS and their association with lower-tropospheric stability and air-sea interaction. J Geophys Res 113:D12114. doi:10.1029/2007JD009514

    Article  Google Scholar 

  • Huang B, Hu Z–Z, Jha B (2007) Evolution of model systematic errors in the tropical Atlantic basin from the NCEP coupled hindcasts. Clim Dyn 28(7/8):661–682. doi:10.1007/s00382-006-0223-8

    Article  Google Scholar 

  • Jha B, Hu Z–Z, Kumar A (2013) SST and ENSO variability and change simulated in historical experiments of CMIP5 models. Clim Dyn. doi:10.1007/s00382-013-1803-z

  • Kalnay E et al (1996) The NCEP/NCAR 40-year reanalysis project. Bull Am Meteor 77:437–471

    Article  Google Scholar 

  • Kang I-S, Lau N-C (1986) Principal modes of atmospheric variability in model atmospheres with and without anomalous sea surface temperature forcing in the tropical Pacific. J Atmos Sci 43:2719–2735

    Article  Google Scholar 

  • Kumar A, Hoerling MP (2000) Analysis of a conceptual model of seasonal climate variability and implications for seasonal prediction. Bull Amer Meteor Soc 81:255–264

    Google Scholar 

  • Kumar A, Zhang Q, Peng P, Jha B (2005) SST-forced atmospheric variability in an atmospheric general circulation model. J Clim 18:3953–3967

    Article  Google Scholar 

  • Kumar A, Chen M, Zhang L, Wang W, Xue Y, Wen C, Marx L, Huang B (2012) An analysis of the nonstationarity in the bias of sea surface temperature forecasts for the NCEP climate forecast system (CFS) version 2. Mon Weather Rev 140:3003–3016

    Article  Google Scholar 

  • Kushnir Y, Wallace JM (1989) Low-frequency variability in the Norther Hemisphere winter: geographical distribution, structure and time-scale dependence. J Atmos Sci 46:3122–3142

    Article  Google Scholar 

  • Kushnir Y, Robinson WA, Bladé I, Hall NMJ, Peng S, Sutton R (2002) Atmospheric GCM response to extratropical SST anomalies: synthesis and evaluation. J Clim 16:2233–2256

    Article  Google Scholar 

  • Linkin ME, Nigam S (2008) The North Pacific Oscillation-West Pacific teleconnection pattern: mature-phase structure and winter impacts. J Clim 21:1979–1997

    Article  Google Scholar 

  • Mo KC, Livezey RE (1986) Tropical-extratropical geopotential height teleconnections during the northern hemisphere winter. Mon Weather Rev 114:2488–2515

    Article  Google Scholar 

  • Newman M, Sardeshmukh PD (1998) The impact of the annual cycle on the north pacific/North American response to remote low-frequency forcing. J Atmos Sci 55:1336–1353

    Article  Google Scholar 

  • Nigam S, Held IM, Lyons SW (1986) Linear simulation of the stationary eddies in a general circulation model. Part I: the no-mountain model. J Atmos Sci 43:2944–2961

    Article  Google Scholar 

  • Nigam S, Held IM, Lyons SW (1988) Linear simulation of the stationary eddies in a general circulation model. Part II: the “mountain” model. J Atmos Sci 45:1433–1452

    Article  Google Scholar 

  • O’Lenic A, Livezey RE (1988) Considerations in the use of rotated principal component analysis (RPCA) in diagnostic studies of upper-air height fields. Mon Weather Rev 116:1682–1689

    Article  Google Scholar 

  • Peña M, Cai M, Kalnay E (2004) Life span of subseasonal coupled anomalies. J Clim 17:1597–1604

    Article  Google Scholar 

  • Peng P (1995) Dynamics of stationary wave anomalies associated with ENSO in the COLA GCM. Ph.D. thesis, University of Maryland, College Park, 180 pp

  • Peng P, Kumar A (2005) A large ensemble analysis of the influence of tropical SSTs on seasonal atmospheric variability. J Clim 18:1068–1085

    Article  Google Scholar 

  • Peng P, Barnston AG, Kumar A (2013) A comparison of skill between two versions of the NCEP climate forecast system (CFS) and CPC’s operational short-lead seasonal outlooks. Weather Forecast 28:445–462

    Article  Google Scholar 

  • Saha S et al (2014) The NCEP climate forecast system version 2. J Clim 27:2185–2208

    Google Scholar 

  • Sardeshmukh PD, Brian JH (1988) The generation of global rotational flow by steady idealized tropical divergence. J Atmos Sci 45:1228–1251

    Google Scholar 

  • Smith TM, Reynolds RW, Peterson TC, Lawrimore J (2008) Improvements to NOAA’s historical merged land-ocean surface temperature analysis (1880–2006). J Clim 21:2283–2296

    Article  Google Scholar 

  • Straus DM, Shukla J (2002) Does ENSO Force the PNA? J Clim 15:2340–2358

    Google Scholar 

  • Ting Mingfang (1996) Steady linear response to tropical heating in Barotropic and Baroclinic models. J Atmos Sci 53:1698–1709

    Article  Google Scholar 

  • Ting M, Sardeshmukh PD (1993) Factors determining the extratropical response to equatorial diabatic heating anomalies. J Atmos Sci 50:907–918

    Article  Google Scholar 

  • Trenberth KE, Branstrator GW, Karoly D, Kumar A, Lau N-C, Ropelewski C (1998) Progress during TOGA in understanding and modeling global teleconnections associated with tropical sea surface temperatures. J Geophys Res 103(C7):14291–14324

    Article  Google Scholar 

  • Van den Dool HM, Peng P, Johansson Å, Chelliah M, Shabbar A, Saha S (2006) Seasonal-to-decadal predictability and prediction of North American climate—the Atlantic influence. J Clim 19:6005–6024

    Google Scholar 

  • Wallace JM, Blackmon ML (1983) Large-scale dynamical processes in the atmosphere by B. Hoskins and R. Pearce. Academic Press, London, pp 55–91

    Google Scholar 

  • Wallace JM, Gutzler DS (1981) Teleconnections in the geopotential height field during the Northern Hemisphere winter. Mon Weather Rev 109:784–812

    Article  Google Scholar 

  • Wang H, Kumar A, Wang W, Xue Y (2012) Influence of ENSO on Pacific decadal variability: an analysis based on the NCEP climate forecast system. J Clim 25:6136–6151

    Article  Google Scholar 

  • Xie P, Akin PA (1996) Analysis of global monthly precipitation using gauge observations, satellite estimates, and numerical model predictions. J Clim 9:840–858

    Article  Google Scholar 

  • Xie P, Wang W, Higgins WR, Arkin PA, Cronin M, Weller R (2006) An examination of the bias in the NCEP GFS, CFS simulations associated with the marine stratus clouds. In: AMS 18th conference on climate variability and global change, Jan. 29–Feb. 2, 2006. Atlanta, GA

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Acknowledgments

We would like to thank Drs. Mingyue Chen, Hui Wang for CPC internal reviewing and Z.-Z. Hu and Wanqiu Wang for helpful discussions. We would very appreciate the comments and suggestions from Prof. Edwin Schneider and two anonymous reviewers.

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Authors and Affiliations

  1. Climate Prediction Center, NCWCP, NECP/NOAA, 5830 University Research Court, College Park, MD, 20740, USA

    Peitao Peng & Arun Kumar

  2. INNOVIM, LLC, Greenbelt, MD, USA

    Bhaskar Jha

Authors
  1. Peitao Peng
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  2. Arun Kumar
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  3. Bhaskar Jha
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Correspondence to Peitao Peng.

Additional information

This paper is a contribution to the Topical Collection on Climate Forecast System Version 2 (CFSv2). CFSv2 is a coupled global climate model and was implemented by National Centers for Environmental Prediction (NCEP) in seasonal forecasting operations in March 2011. This Topical Collection is coordinated by Jin Huang, Arun Kumar, Jim Kinter and Annarita Mariotti.

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Peng, P., Kumar, A. & Jha, B. Climate mean, variability and dominant patterns of the Northern Hemisphere wintertime mean atmospheric circulation in the NCEP CFSv2. Clim Dyn 42, 2783–2799 (2014). https://doi.org/10.1007/s00382-014-2116-6

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  • DOI: https://doi.org/10.1007/s00382-014-2116-6

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