Monitoring and Prediction of Modes of Coherent Tropical Variability
Real-time filtering of OLR data to monitor and predict the convective
variations of the Madden-Julian
oscillation and various convectively coupled equatorial waves,
based on the "climatological" spectral peaks of a long record of
satellite-observed data.
(Last updated with OLR data from:
)
| Antisymmetric Modes |
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Symmetric Modes |
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^^ Click on images to enlarge and obtain additional information. ^^
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Fig 1. Regions of wavenumber-frequency filtering for the
outgoing
longwave radiation (OLR) signals of
certain modes of coherent tropical variability.
These modes are identified as spectral peaks (the shading) in
a wavenumber-frequency spectrum analysis of a long record of satellite-observed
OLR, a good proxy for deep tropical convection.
Filtering is for the Madden-Julian Oscillation (MJO; blue), Kelvin
wave (green), n = 1 equatorial Rossby (ER) wave (black), and mixed
Rossby-gravity (MRG) wave (brown). The so-called "convectively coupled
equatorial waves" are defined to be in either the antisymmetric or
symmetric components only, while the MJO is allowed to contain both
components. For details, see Wheeler and Kiladis (1999, Journal of the Atmospheric Sciences).
The full details of the real-time filtering technique and testing of its skill have
been provided in Wheeler and Weickmann (2001,
Monthly Weather Review).
- TIME-LONGITUDE PLOTS
- Northern Tropics (2.5N-17.5N)
- Near Equatorial (7.5S-7.5N)
- Southern Tropics (17.5S-2.5S)
- Wide Tropics (15.S-15.N)
- FORECAST MAPS
- MJO OLR Anomalies
-
5-day means (i.e., average of Days -4 to 0, 1 to 5, 6 to 10, etc.)
-
7-day means (i.e., average of Days -6 to 0, 1 to 7, etc.)
- n=1 Equatorial Rossby OLR Anomalies
-
3-day means (i.e., average of Days -1 to 0, 1 to 2, etc.)
-
5-day means (i.e., average of Days -4 to 0, 1 to 5, etc.)
- Kelvin wave OLR Anomalies
- MRG wave OLR Anomalies
- MAPS (ANIMATIONS)
- MJO, n=1 ER, Kelvin, MRG
- MJO and Anoms only
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Created and maintained by Matthew Wheeler