Climate Dynamics

, Volume 43, Issue 1–2, pp 517–534 | Cite as

Representation of tropical subseasonal variability of precipitation in global reanalyses

  • Daehyun Kim
  • Myong-In LeeEmail author
  • Dongmin Kim
  • Siegfried D. Schubert
  • Duane E. Waliser
  • Baijun Tian


Tropical subseasonal variability of precipitation from five global reanalyses (RAs) is evaluated against Global Precipitation Climatology Project (GPCP) and Tropical Rainfall Measuring Mission (TRMM) observations. The RAs include the three generations of global RAs from the National Center for Environmental Prediction (NCEP), and two other RAs from the European Centre for Medium-Range Weather Forecasts (ECMWF) and the National Aeronautics and Space Administration/Goddard Space Flight Center (NASA/GSFC). The analysis includes comparisons of the seasonal means and subseasonal variances of precipitation, and probability densities of rain intensity in selected areas. In addition, the space–time power spectrum was computed to examine the tropical Madden-Julian Oscillation (MJO) and convectively coupled equatorial waves (CCEWs). The modern RAs show significant improvement in their representation of the mean state and subseasonal variability of precipitation when compared to the two older NCEP RAs: patterns of the seasonal mean state and the amplitude of subseasonal variability are more realistic in the modern RAs. However, the probability density of rain intensity in the modern RAs show discrepancies from observations that are similar to what the old RAs have. The modern RAs show higher coherence of CCEWs with observed variability and more realistic eastward propagation of the MJO precipitation. The modern RAs, however, exhibit common systematic deficiencies including: (1) variability of the CCEWs that tends to be either too weak or too strong, (2) limited coherence with observations for waves other than the MJO, and (3) a systematic phase lead or lag for the higher-frequency waves.


Reanalysis Precipitation Tropics Subseasonal variability Madden-Julian oscillation Convectively-coupled equatorial waves 



This work was supported by the Korea Meteorological Administration Research and Development Program under Grant APCC 2013-3141. Also, this work was supported by the NASA grant NNX09AK34G for DK, and the NASA Modeling, Analysis, and Prediction (MAP) program for SDS. DEW’s and BT’s contribution to this research was performed at Jet Propulsion Laboratory (JPL), California Institute of Technology (Caltech), under a contract with National Aeronautics and Space Administration (NASA). The authors are grateful for the computing resources provided by NASA and the Supercomputing Center at Korea Institute of Science and Technology Information (KSC-2013-C2-011).


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Copyright information

© Springer-Verlag Berlin Heidelberg 2013

Authors and Affiliations

  • Daehyun Kim
    • 1
  • Myong-In Lee
    • 2
    Email author
  • Dongmin Kim
    • 2
  • Siegfried D. Schubert
    • 3
  • Duane E. Waliser
    • 4
  • Baijun Tian
    • 4
  1. 1.Lamont-Doherty Earth ObservatoryColumbia UniversityPalisadesUSA
  2. 2.School of Urban and Environmental EngineeringUlsan National Institute of Science and TechnologyUlsanRepublic of Korea
  3. 3.NASA Goddard Space Flight CenterGreenbeltUSA
  4. 4.NASA Jet Propulsion LaboratoryPasadenaUSA

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