Forecast of Tropical Cyclone Activity over the Western North Pacific
Johnny C. L. Chan
Dept. of Physics & Materials Science
City University of Hong Kong
Kowloon, HONG KONG
The long-awaited forecast of tropical cyclone (TC) activity over the
Western North Pacific (WNP) has finally come. We, at the City University
of Hong Kong, are putting out the following forecast for the 1997 season:
[Normals (calculated from JTWC data for 1965-94) are in parentheses]
Annual for the WNP:
No. of TCs : 33 +/- 3 (31)
No. of TCs reaching at least tropical storm intensity: 30 +/- 3 (27)
No. of typhoons: 19 +/- 2 (17)
May to December for the WNP:
No. of TCs from May to Dec: 30 +/- 3 (28)
No. of TCs reaching at least tropical storm intensity: 27 +/- 2 (25)
No. of typhoons: 18 +/- 2 (16)
Annual for the South China Sea (SCS):
No. of TCs: 12 +/- 2 (13)
No. of TCs reaching at least tropical storm intensity: 9 +/- 2 (10)
Boundaries:
WNP: 100-180°E, 0-40°N
SCS: 100-120°E, 0-25°N
The predictions are based on three sets of monthly parameters for the
months from April of the previous year to March of the current year. Not
all parameters are chosen. The three sets are as follows:
1. SOI and NINO-4 anomalies
2. Indices describing the winter conditions over East Asia and the Western
North Pacific. These include the following:
NOAA/CAC West Pacific Pattern Index
Strength of the subtropical high over the South China Sea
Area of the 500-hPa polar vortex over the Pacific sector
500-hPa height anomalies over the Tibetan Plateau
500-hPa trough over the India-Burma region
Western extent of the 500-hPa ridge
Cold-air intrusions into China
3. Climatology-Persistence of the number of TCs (CLIPER-type)
The test data set consists of TCs for the years 1965-94 and the
predictions are based on the projection-pursuit regression method for
individual parameters and then a weighted combination of individual
forecasts (up to a maximum of five) gives the final forecast. Tests have
been made using the jackknife method and found to be satisfactory.
This study was sponsored by the Risk Prediction Initiative of the Bermuda
Biological Station for Research.
A paper is being written up for publication. Comments are welcome.
Prof. Johnny C. L. Chan
Dept. of Physics & Materials Science
City University of Hong Kong
83 Tat Chee Ave.
Kowloon, HONG KONG
Tel: 852-2788-7820, Fax: 852-2788-7830
E-mail: apjcchan@cityu.edu.hk