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The Cloud Population of the Madden-Julian Oscillation

The Cloud Population of the Madden-Julian Oscillation. Early Results from DYNAMO. R. Houze and D. Hence, S. Brodzik , K. Rasmussen, S. Powell, H. Barnes, B. Dolan, K. Chakravarty , C. Burleyson , Z. Li, S. Ellis, T. Weckwerth , J. Vivekanandan , J. Hubbert , W.-C. Lee.

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The Cloud Population of the Madden-Julian Oscillation

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  1. The Cloud Population of the Madden-Julian Oscillation Early Results from DYNAMO R. Houze and D. Hence, S. Brodzik, K. Rasmussen, S. Powell, H. Barnes, B. Dolan, K. Chakravarty, C. Burleyson, Z. Li, S. Ellis, T. Weckwerth, J. Vivekanandan, J. Hubbert, W.-C. Lee Atmos. Sci. Colloquium, Seattle, 6 April 2012

  2. Indian Ocean 1 2 The MJO 3 Wheeler and Hendon 2004 4 5 6 7 8 DYNAMO

  3. 7N Equator

  4. NCAR S-PolKaRadar S Ka

  5. Project Data Flow Satellite Global models Soundings Other island radars Ship data NCAR field catalog Aircraft data Ship radars LIghtning NCAR radar processor S-PolKaradar UW workstations UW server Daily Science Summaries

  6. Radar experiment goal  Characteristics and evolution of the MJO cloud population in the region where the disturbance builds up Addu Atoll

  7. Rain over area scanned by S-PolKa Supp. Active Supp. Active Lull Active Supp.

  8. Suppressed conditionechoes

  9. Supp. Active Supp. Active Lull Active Supp.

  10. Suppressed phases: Lines of non-precipitating clouds

  11. Suppressed phases: The “worm echo”

  12. Slightly active moist layer Clouds building at cold pool boundaries

  13. Slightly active moist layer Clouds building at cold pool boundaries

  14. Cold pool boundaries seen in differential reflectivity (ZDR) Birds? Dragonflies? ???

  15. Birds caught on camera

  16. Moderate cumulonimbus begin to grow upscale Doppler velocity large non-melting ice small ice Hydrometeor type graupel meltingice heavyrain

  17. Supp. Active Supp. Active Lull Active Supp.

  18. October 16

  19. Conv. Refl. Rain Strat. October 16

  20. Intense melting layer 50 dBZ! graupel 10 km 5 km melting snow

  21. Active phase few days later Convection feeding into a large MCS

  22. Biggest MCS of first active phase: weak unidirectional shear

  23. Supp. Active Supp. Active Lull Active Supp.

  24. Giant Rings of Convection Larger than mesoscale organization of deep convection

  25. Squall line in late active phase westerlies Doppler velocity Hydrometeor type

  26. Supp. Active Supp. Active Lull Active Supp.

  27. Suppressed condition clouds

  28. Supp. Active Supp. Active Lull Active Supp.

  29. Supp. Active Supp. Active Lull Active Supp.

  30. Westerly Surges November Larger than mesoscale organization of deep convection October

  31. Supp. Active Supp. Active Lull Active Supp.

  32. Long arc line

  33. Long arc linesegment on radar

  34. Squall linein the strong westerlies

  35. Weak stratiform in the strong westerlies

  36. S-PolKa S-band Stratiform Rain Fraction Stratiform Rain Fraction

  37. Supp. Active Supp. Active Lull Active Supp.

  38. The most robust squall line in the strong westerlies… …robust momentum transport …only moderate stratiform

  39. Supp. Active Supp. Active Lull Active Supp.

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