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| Statistical prediction of weekly tropical
cyclone activity in the Southern Hemisphere |
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| > Forecasts | |||||
The maps below show the forecasted probability that at least one cyclone
will occur (i.e. including the whole track) or form (i.e. genesis of a
new storm) over coming weeks (Weeks 1, 2, and 3) in a grid of overlapping
regions. Top : total probability (%). Bottom: anomaly probability (%)
relative to the daily climatology. Use tabs to select "Occurrence"
or "Genesis", and buttons to select the forecast week. Each
region is 20deg in longitude by 15deg in latitude. Move cursor over the
maps to see the forecast history and verification TC data (black bars
and TC names). Please note that the verification data comes from real-time
bulletin of various official warning center and has not been quality controlled. Last update : Tuesday 09 February 2010 |
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> Presentation of the method |
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These forecasts are made using the known influence of the Madden Julian Oscillation (MJO) and other large-scale variability (e.g. El Nino Southern Oscillation, ENSO and the Indian Dipole Mode ) on tropical cyclone (TC) activity across the Southern Hemisphere. As the state of the MJO is predictable out to about 3-4 weeks, there is some potential for the statistical prediction of week-to-week TC activity on this timescale. Specifically, the predictions are made using logistic regression with a total of six possible predictors : two to measure the state of the MJO ; three to measure the state of large-scale tropical interannual variability (e.g. ENSO and the Indian Dipole Mode) ; and one to measure the climatological seasonal cycle of TC activity. The original implementation of the technique was for 4 large regions, as described in Leroy and Wheeler (2008 ; Monthly Weather Review). Independent verification results for the 2006/07 and 2007/08 seasons are provided here (pdf file - 170 kB). The current implementation of the technique differs from the original
in two ways :
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| > Collaborators and sponsors |
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| Austalian Bureau of Meteorology
Indian Ocean Climate Initiative UK Met Office for the verification data
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> Input data |
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TNI is calculated form NINO4 , NINO1
and NINO2
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