|
2006 Predictions of Seasonal Tropical Cyclone Activity over the Western North Pacific
1. Introduction |
Issued on 24 April 2006 |
Since 2000, the Laboratory for Atmospheric Research (LAR) at City University of Hong Kong has been issuing real-time predictions of the annual number of tropical cyclones (TCs) affecting the western North Pacific (WNP) and the South China Sea (SCS). From 2001 onwards, LAR also issued predictions on the annual number of TCs making landfall along the South China coast. Verifications of the predictions have shown that the predictions are mostly correct within the error bars.
These are all statistical predictions with predictors drawn from a large group of indices that represent the atmospheric and oceanographic conditions in the previous year up to the spring of the current year. The most prominent ones include the proxies for El Niño/Southern Oscillation (ENSO), the extent of the subtropical ridge, the intensity of the India-Burma trough. Details can be found in Chan et al. (1998, 2001) and Liu and Chan (2003).
As an important determinant is the status of the ENSO condition, it is useful to have a discussion on the possible ENSO situation in 2006. The oceanic and atmospheric conditions briefly approached the La Niña threshold at the beginning of the year. However, the ENSO conditions return to neutral with the recent warming of the central and eastern Pacific. A summary of the various ENSO model forecasts from different climate centres suggests that most of them predict a neutral condition in 5 to 8 months time (Table. 1). Out of the 12 forecasts, 10 suggest neutral conditions throughout the summer and fall while the others suggest a possible warm event. Based on these results, it appears that 2006 will likely be a neutral year.
2. 2006 predictions
Predictions of overall TC activity from the predictors all fall within the normal range (Table 2). For the number of tropical storms and typhoons, most of the predictors forecast slightly below-normal to normal activity except for the ENSO predictor which suggests above-normal activity. A weighted forecast from all the predictions therefore would suggest near-normal activity. Similar forecast is obtained for the number of typhoons. Thus, it is expected that the overall TC activity, the number of tropical storms and typhoons as well as the number of typhoons are likely to be near-normal. The quantitative predictions are given in Table 2.
While the predictors HIB and WP give near-normal TC activity, the predictor related to the subtropical high (HWNP) suggests a slightly below-normal TC activity. Such forecasts are partly because of the stronger-than-normal subtropical high observed between February and March in 2006 (Fig. 1).
The possible error in the current predictions is given by an envelope of the possible errors, which are based on the predictions from individual predictors. The smallest and largest numbers among the individual predictions are considered as the lower and upper bound of the final predictions. A larger (smaller) difference between the lower and upper bound might then indicate lower (higher) predictability. Based on this concept, we could see that for this year, predictions for the overall TC activity have the smallest spread and thus the highest predictability. The confidence of the predictions for the other parameters is lower, which may be related to the high uncertainty in the ENSO condition in 2006.
As discussed in Chan et al. (2001), we will provide an updated forecast sometime in June.
Summary of predictions
Entire western North Pacific |
|
All TC |
near normal |
Tropical storms and typhoons |
near normal |
Typhoons |
near normal |
Table 1. | Summary of model forecasts extracted from the Australian Bureau of Meteorology homepage. |
GROUP |
5
MONTHS |
8
MONTHS |
POAMA |
Neutral |
Warm |
Neutral |
Neutral |
|
Neutral |
Not Available |
|
Neutral |
Not Available |
|
Neutral |
Neutral |
|
Neutral |
Neutral |
|
Neutral |
Neutral |
|
Neutral |
Neutral |
|
Warm |
Warm |
|
Neutral |
Not Available |
|
Neutral |
Not Available |
|
Neutral |
Neutral |
Table 2. | Forecasts from various predictors and the weighted average of the forecasts. |
Entire western North Pacific |
||||||||||||||||||||||||||||
|
||||||||||||||||||||||||||||
|
||||||||||||||||||||||||||||
|
||||||||||||||||||||||||||||
|
Fig. 1. |
500-hPa geopotential height anomalies between February and March in 2006. Thick contours indicate the geopotential height (contour interval = 10 m) ³5860 m. |
Chan, J. C. L., J. E. Shi and C. M. Lam, 1998: Seasonal forecasting of tropical cyclone activity over the western North Pacific and the South China Sea. Weather Forecasting, 13, 997-1004. Abstract
Chan, J. C. L., J. E. Shi and K. S. Liu, 2001: Improvements in the seasonal forecasting of tropical cyclone activity over the western North Pacific. Weather Forecasting, 16, 491-498. Abstract
Liu, K. S. and J. C. L. Chan, 2003: Climatological characteristics and seasonal forecasting of tropical cyclones making landfall along the South China coast. Monthly Weather Review, 131, 1650-1662. Abstract