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The Madden-Julian Oscillation

The Madden-Julian Oscillation. ATS 553. Intraseasonal Oscillations. “Any quasiperiodic atmospheric fluctuation that is: Longer than synoptic features, but Shorter than the components of the annual cycle.”. Madden-Julian Oscillation. The most famous and most important of the ISOs.

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The Madden-Julian Oscillation

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  1. The Madden-Julian Oscillation ATS 553

  2. Intraseasonal Oscillations • “Any quasiperiodic atmospheric fluctuation that is: • Longer than synoptic features, but • Shorter than the components of the annual cycle.”

  3. Madden-Julian Oscillation • The most famous and most important of the ISOs. • “A pattern of tropical convection in which a given location experiences enhanced precipitation about every 40-50 days.”

  4. How MJO was discovered In the 1960s and 1970s, new computer power created the ability to look for patterns in meteorological observations. Could only look for patterns in TIME (at a location), not SPACE (at a given time). Tended to detect OSCILLATIONS.

  5. What They Found • Surface pressure oscillates with a period of 40-50 days. • ZONAL winds in the lower and upper troposphere also oscillate at this frequency, but 180° out-of-phase. • The signal was limited to the deep tropics. • They found little signal in the meridional wind, or in zonal winds in the midtroposphere.

  6. Their Interpretation MJO is a region of low-level convergence and convection. Propagating eastward only. Circumnavigates the globe in 40-50 days.

  7. Their Interpretation Pressure is LOW in the region of strongest convection. Upper-level outflow is only in the zonal direction.

  8. Kelvin Waves in the Atmosphere

  9. Kelvin Waves in the Atmosphere

  10. Features: Enhanced tradewinds AHEAD of the convection.

  11. Features: Weak tradewinds—maybe even westerlies—behind the convection.

  12. Features: Alternating areas of high and low pressure. H L H

  13. Features: Alternating areas of high and low OLR values! H L H

  14. Features: Notice that there shouldn’t be much signal in the midtropospheric winds!

  15. Features: An area of upper-tropospheric DIVERGENCE, best seen in the VELOCITY POTENTIAL.

  16. Equatorially trapped

  17. Equatorially trapped

  18. Circumnavigating the Globe? • Madden and Julian originally believed that this area of convection propagated all the way around the world every 40-50 days. • But this isn’t exactly right.

  19. Circumnavigating the Globe? • Rather, the convection is TRIGGERED in the eastern Indian Ocean (typically by intruding midlatitude systems). • Convection dies out in the eastern Pacific due to cold SSTs

  20. Circumnavigating the Globe? • However, the region of upper-level divergence WILL generally travel all the way around the world as a Kelvin Wave.

  21. Kelvin Waves and the Walker Circulation

  22. Kelvin Waves and the Walker Circulation Initially OPPOSES the Walker Circulation Later ENHANCES the Walker Circulation!

  23. Kelvin Waves and the Walker Circulation Later, it OPPOSES the Walker Circulation and the trade winds in the Pacific!

  24. Kelvin Waves and the Walker Circulation However, these tradewinds are what maintained the high sea surface temperatures and heights of the western Pacific Warm Pool…

  25. El Nino and the MJO • MJO events can TRIGGER El Nino events by weakening the trade winds (or even having a WESTERLY WIND BURST).

  26. El Nino and the MJO • Why doesn’t EVERY MJO trigger an El Nino event? • CHARGE/DISCHARGE THEORY: • MJO is the TRIGGER—it happens much more often than the El Nino event itself. • Not every trigger is exactly right. • Even when the trigger is right, maybe ocean conditions are not yet right. • A partial explanation for the timing of ENSO.

  27. An MJO that’s a little off the equator

  28. A very short MJO

  29. An MJO from the southwest

  30. Triggering MJO Events An MJO event in the Indian Ocean upsets the SSTs. It takes time for the SSTs to recover. Any intruding midlatitude systems during this period will FAIL to trigger an MJO event. Only when the environment is ready (another 40-50 days) will the next midlatitude system be able to trigger a new MJO!

  31. What are MJO events? • Described by “Nakazawa’s Hierarchy of Convection”

  32. What are MJO events? • Each MJO event is actually composed of a small number of “super cloud clusters”--SCCs

  33. What are MJO events? • SCCs: • Move EASTWARD • Last a day or two

  34. What are MJO events? • What are SCCs? • Made of Cloud Clusters (CCs)

  35. What are MJO events? • What are CCs? • Small groups of thunderstorms • Last less than a day • Move WESTWARD

  36. 1 MJO

  37. 4 SCCs

  38. Many CCs

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