1 / 9

THE MADDEN-JULIAN OSCILLATION AND CALIFORNIA RAINFALL Charles Jones University of California Santa Barbara

THE MADDEN-JULIAN OSCILLATION AND CALIFORNIA RAINFALL Charles Jones University of California Santa Barbara. Madden and Julian (1972). The Madden-Julian Oscillation. * Significant case-to-case variability. Modulate the variability of the monsoons in Asia-Australia, Africa and Americas

agrata
Download Presentation

THE MADDEN-JULIAN OSCILLATION AND CALIFORNIA RAINFALL Charles Jones University of California Santa Barbara

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. THE MADDEN-JULIAN OSCILLATION AND CALIFORNIA RAINFALL Charles Jones University of California Santa Barbara

  2. Madden and Julian (1972) The Madden-Julian Oscillation

  3. * Significant case-to-case variability

  4. Modulate the variability of the monsoons in Asia-Australia, Africa and Americas • Teleconnections with extratropics in both hemispheres • Modulate thermocline variability in the tropical Pacific Ocean • Influence on forecast skills in the tropics and extratropics

  5. Outgoing Longwave Radiation Climatology TC TS TC < TS

  6. MJO • Pentads of OLR 1979-2002 (winter) Filtered 20-90 days anomalies • EOF of OLR anomalies • Active MJO: amplitudes of PC1 and PC2

  7. The Life Cycle of the MJO: Convective Activity Time OLR Data are filtered in time (20-90 days) and composites of OLR anomalies are made Enhanced Convection Suppressed Convection Jones (2000)

  8. Zonal (U) wind component (850 hPa) is filtered in time (20-90 days) and composites of anomalies are made Time Enhanced Convection Easterly anomalies Westerly anomalies

More Related