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CINDY2011/DYNAMO Madden-Julian oscillation successfully reproduced in global cloud/cloud-system resolving simulations despite weak tropical wavelet power



Details

  • Journal Title:
    Scientific Reports
  • Personal Author:
  • NOAA Program & Office:
  • Description:
    The role of tropical atmospheric waves in the propagation mechanism of the Madden-Julian oscillation (MJO), a huge eastward-propagating atmospheric pulse that dominates intraseasonal variation of the tropics and affects the entire globe, has been long discussed but remains unclear. An MJO event observed in a major field campaign is reproduced using a front-running global cloud/cloud-system resolving model with 3.5 km, 7 km, and 14 km meshes. The eastward-migration speed of the MJO convective envelope in the 3.5 km and 14 km simulations agree well with observation, despite weak Kelvin wave signal power calculated by applying a combined Fourier-wavelet transform method. Our results suggest that the eastward propagation of this MJO event was principally controlled by an MJO-scale energy balance, and not by dynamical interaction of embedded tropical waves. The eastward propagation is delayed in the 7 km simulation, which features the highest surface latent heat flux to the west of the convective envelope center. This latent heat flux appears to be caused by prolonged existence of westward-migrating Rossby wave-like cyclonic disturbances near the equator; the embedded waves may not be part of the essential mechanism for the MJO eastward propagation, but can affect it by altering the energy balance.
  • Keywords:
  • Source:
    Scientific Reports 8 (11664) 
  • DOI:
  • Pubmed Central ID:
    PMC6076279
  • Document Type:
  • Funding:
  • Rights Information:
    CC BY
  • Compliance:
    PMC
  • Main Document Checksum:
    urn:sha-512:8b8ba73c985d24c76d8ab2f7049a6e1a106ac8c1506218adfe38887d7038cedea9b13db543fed046648e5295e8e56a13e023c78d0d37296d1c280ae2f6e240ca
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    Filetype[PDF - 4.02 MB ]
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