2009/10 Predictions of Seasonal Tropical Cyclone Activity in the Australian
region
The Guy Carpenter Asia-Pacific
Climate Impact Centre (GCACIC) at City University of Hong Kong has embarked on
the development of real-time predictions of the annual number of tropical
cyclones (TCs) affecting the Australian region (90°E-160°E, 40°S-0°N) (NA)
and its subregion (western Australian region, 90°E-135°E, 40°S-0°N) (NWA).
Hindcasts for the period of 1983-2008 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 during the pre-season. The most prominent ones
include the proxies for the El Niño/Southern Oscillation (ENSO) and the Indian
Ocean Dipole (IOD). These results are currently being written up (Liu
and Chan 2009). It should also be noted that predictions for the eastern
Australian region are not made at this point because of the difficulty in
identifying significant predictors. Further investigation will be necessary in
this area and results will be reported in the future.
Starting from the 2009/10 season,
we will attempt to issue real-time forecasts of NA and NWA.
These should be considered as experimental forecasts and verifications will be
made after each season. A more thorough evaluation of the performance of the
prediction equation will be made in a few years.
2. ENSO and IOD conditions in 2009/10
As an
important determinant is the status of the ENSO condition, it is useful to have
a discussion on the possible ENSO situation in 2009/10. An El Niño event has
developed in the summer. In October, SSTs remain warmer than normal in the
central and eastern equatorial Pacific Ocean. The Niño3.4 and Niño4 indices in
October are 0.99 and 1.12 respectively. A summary of
the various ENSO model
forecasts from different climate centres
suggests that warm conditions will persist in the next 5 to 7 months.
Based on observations and model forecasts, the El Niño is
expected to continue into the Southern Hemisphere summer.
The IOD is currently in its neutral
condition, as suggested by the small values of the Dipole Mode Index (DMI)
during the last few months.
Thus, ENSO tends to be the dominant factor
affecting the TC activity in the Australian region during the 2009/10 season and
the effect of IOD appears to be less significant.
3. Predictions for 2009/10
For the entire Australian
region, all the ENSO predictors (NINO4 index, trade wind index and OLR
index) consistently forecast a below-normal activity (ranging from 7 to 9).
The IOD predictor suggests a near-normal TC activity (predicted number being
10). Therefore, a below-normal TC activity (8 TCs with tropical storm
intensity or above) is expected for this region.
A similar forecast is obtained for
the western Australian region. The ENSO predictors suggest a below-normal TC
activity, with the predicted numbers ranging from 4 to 6 while the IOD predictor
gives a near-normal TC number. Therefore, the final forecast is 5 TCs with
tropical storm intensity or above, which is below the normal number.
Thus, it is expected that the TC
activities in both the entire Australian and the western Australian regions are
likely to be below-normal. See the quantitative predictions in
Table 1.
As an El
Niño event has developed in 2009 (see
section 2), it is useful to
discuss the TC activity during previous El
Niño years. Out of the 9
TC seasons associated with El
Niño, 6 are associated with below-normal TC activity (TC number
£
9) and 3 are associated with normal TC activity (TC number between 10 and 12) in
the Australian region (Table 2). Thus, the
annual number of TCs with tropical storm intensity or above tends to be normal
or below-normal
in the Australian
region during El
Niño years. The effect of
ENSO appears to be more significant for the western Australian region. Most of
the TC seasons have the below-normal TC activity (TC number
£
6) except for the 2004/05 season (Table 2). Therefore,
the TC activity in the 2009/10 season will likely to be below normal, with the
possibility of a near-normal TC
number,
which is consistent with our forecast.
Summary of predictions
|
Forecast |
Normal |
Entire
Australian region
(90°E-160°E, 40°S-0°N) |
8 (below-normal) |
11 |
Western
Australian region
(90°E-135°E, 40°S-0°N) |
5 (below-normal) |
8 |
Reference:
Liu, K. S. and J. C. L. Chan,
2009: Interannual variation of Southern Hemisphere tropical cyclone activity and
seasonal forecast of tropical cyclone number in the Australian region.
Manuscript under preparation.
Table 1. |
Forecasts from various predictors and the weighted
average of the forecasts. |
Annual number of tropical storms and typhoons |
Entire Australian region |
|
NINO4 |
TW |
OLR |
DMI |
Final forecast |
Normal
|
Prediction |
7 |
8 |
9 |
10 |
8 |
11 |
Weight |
0.75 |
0.70 |
0.75 |
0.64 |
|
|
|
Western Australian region |
|
NINO4 |
TW |
OLR |
DMI |
Final forecast |
Normal
|
Prediction |
4 |
6 |
5 |
7 |
5 |
8 |
Weight |
0.70 |
0.78 |
0.77 |
0.64 |
|
|
|
|
NINO4 |
Sea surface temperature (SST)
anomalies in the NINO4 region (5oS-5oN, 160oE-150oW) |
TW |
Trade wind
index: mean 850-hPa zonal wind anomaly index over the West Pacific (5oS-5oN,
135oE-180oE) |
OLR |
Outgoing long wave radiation (OLR) index near equator (160°E-160°W) |
DMI |
Dipole mode
index: difference in SST anomaly between tropical western Indian Ocean
(60°E-80°E, 10°S-10°N) and tropical south-eastern Indian Ocean (90°E-110°E,
10°S-0°) |
|
Table 2. |
Annual number of TCs with tropical storm intensity or above in the entire
Australian region and the western Australian region in an El Niño year. Red
and blue shadings indicate the above-normal and below-normal TC activity
respectively. |
TC season with
El Niño event |
Entire
Australian region
(90o-160oE) |
Western
Australian region (90o-135oE) |
1982/83 |
7 |
5 |
1986/87 |
7 |
5 |
1987/88 |
5 |
3 |
1991/92 |
11 |
5 |
1994/95 |
6 |
4 |
1997/98 |
11 |
6 |
2002/03 |
6 |
5 |
2004/05 |
11 |
10 |
2006/07 |
5 |
4 |
|