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Home | Prediction -> Products -> Hurricane Forecasts The IRI Atlantic Hurricane Activity Experimental Dynamical ForecastsJuly 2006 IRI Atlantic Hurricane Activity ForecastThere is an enhanced probability (approximately 40%) that the number of tropical cyclones in the Atlantic during the 2006 peak season (August to October) will be in the normal category, which is defined as between 6 and 9 named tropical cyclones. There is also a 35% probability that the number of named storms in this period will be in the above normal (10 or more named tropical cyclones) category. These probabilities are greater than the long-term average probability of 33%. The probability that the number of named storms in this period will be in the below normal (5 or less named tropical cyclones) category is 25%. Fig. 1 - Probability Forecasts for Number of Tropical Cyclones
Fig. 2 - Probability Forecasts for Accumulated Cyclone Energy This forecast was obtaining by forcing the atmospheric model with slightly above SSTs in the central Pacific and above normal SSTs in the northern Atlantic, as shown in our SST forecast for the ASO period. The probabilities for Atlantic NTCs (or ACE) were subjectively adjusted slightly toward the above normal category because the SST predictions for the northern tropical Atlantic were thought to weaken the current positive anomalies somewhat too quickly, and the SST predictions for the tropical Pacific were suspected to show slightly too much warming by the peak season of Aug-Sep-Oct. Background InformationThe mean number of observed Atlantic named tropical cyclones (1971-2001) in the peak season is 8.1 with a standard deviation of 3.2. The near normal category is between 6 and 9 named tropical cyclones in the August to October peak season. The lowest number of tropical cyclones in the peak season during this historical period was 3 and the maximum was 15. If the peak season climatological median ACE in the period 1971-2001 is defined as 100%, the normal range varies between 68% and 129%. The standard deviation of the ACE index is 71%, and in extreme years the index can exceed 300% or be less than 20%. The historical variability in the ACE index is proportionally larger than the variability of the number of named tropical cyclones, as it takes into account not only the number of tropical cyclones but also their intensity and duration. This outlook was produced by tracking Atlantic hurricane-like systems in one of our operational atmospheric general circulation models (AGCMs), ECHAM4.5, forced with IRI's predicted sea surface temperatures. While low-resolution (approximately 2.8 degrees longitude and latitude) AGCMs are not adequate for forecasts of individual hurricanes, 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 North Atlantic. Model tropical cyclones are weaker and larger than observed, 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 temporal distribution of these model tropical cyclones in the North Atlantic is similar to that of observed tropical cyclones in the region. The amount tropical cyclone activity of both model and observations in the Atlantic is strongly influenced by ENSO. The IRI July 2006 hurricane activity forecast differs from
the Tropical Storm Risk
July 2006 statistical forecasts of Atlantic hurricanes for the
calendar year 2006, which calls for an active season in the
Atlantic, both in the number of hurricanes and in the ACE index. An
extremely above-normal Atlantic tropical cyclone activity season is
also the
Colorado State University May 31st, 2006 forecast. The
NOAA 2006 Atlantic hurricane outlook, released in May 22nd, is as well
for a very active season * The ACE index is calculated by summing the squares of the estimated 6-hourly maximum sustained wind speed in knots for all periods in which the tropical cyclones are either of named storm or typhoon intensity. Reference: Bell, G.D., and Coauthors, 2000: Bull. Amer. Met. Soc., 81, S1-S50 (see also http://www.cpc.noaa.gov/products/outlooks/background_information.html). |