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The IRI Australian Tropical Cyclone Activity Experimental Dynamical ForecastsJanuary 2004 IRI Australian Tropical Cyclone Activity Forecast There is an enhanced probability (approximately 40%) that the number
of tropical cyclones in the Australian
region (105E to 165E) during the 2004 peak season (January to
March) will be in the normal category, which is defined as 5 to
8 named tropical cyclones. There is also a 35% probability that
the number of named tropical cyclones in this period will be in the
above normal category (9 or more named tropical cyclones). These
probabilities are greater than the long-term average probability of
33%. There is a 25% probability that the number of named tropical
cyclones in this period will be in the below normal category (4 or less
named tropical cyclones). This forecast is based on the IRI sea surface
temperature (SST) forecast that reflects the neutral ENSO conditions,
with a region of above normal SST along the equator in much (but most
strongly the Background InformationThe mean number of observed Autralian named tropical cyclones (1971 - 2002) in the peak season (January to March) is 7.1 with a standard deviation of 3.2. The near normal category is between 5 and 8 named tropical storms in the January-March peak season. The lowest number of tropical cyclones in the peak season during this historical period was 1 and the maximum was 13. This outlook was produced by tracking Australian tropical cyclone-like systems in one of our operational atmospheric general circulation models (AGCMs), ECHAM4.5, forced with IRI's predicted sea surface temperatures. AGCMs are not adequate for forecasts of individual tropical cyclones. However, they can have significant skill in predicting the amount of tropical cyclone activity over specific basins, as is the case for the ECHAM4.5 over the Australian region. Due to the low-resolution (approximately 2.8 degrees longitude and latitude) model tropical cyclones are weaker and larger than observed tropical cyclones, but have an identifiable signature with many observed tropical cyclone characteristics. The model skill is due to the variability of the tropical cyclone activity being mainly determined by large-scale variables that affect that activity, such as sea surface temperatures and vertical wind shear, which can be predicted using AGCMs. The seasonal distribution of these model tropical cyclones in the Australian region is similar to that of observed tropical cyclones in the region. The amount of tropical cyclone activity of both model and observations in the Australian region is strongly influenced by ENSO. The IRI January 2004 Australian tropical cyclone activity forecast
is somewhat different from the Tropical
Storm Risk December 2003 statistical forecasts of Australian
tropical cyclones for the 2003/2004 season (July 2003 to June 2004).
The Tropical Storm Risk forecast called for a below normal number of
named tropical cyclones. It is important to notice that the definition
of the Australian region is slightly different in this forecast. |