The IRI has prepared this experimental Climate Outlook for Australia for December 2002 - May 2003. Of relevance in the preparation of this outlook is the prediction of moderate El Nino conditions in the central and eastern equatorial Pacific through the end of 2002 and lasting at least into early 2003. The sea surface temperatures (SSTs) across much of the central equatorial Pacific are more than 1 degree C above their long-term average (SSTs), and have been so for the last several months. In the last month, SST anomalies in the central Pacific have exceeded 2 degrees C. Warm SST anomalies for the central equatorial Pacific are predicted by the coupled model throughout the forecast period December-February 2003, January-March 2003, February-April 2003, March-May 2003. However, the coupled model forecast has not captured the strength of the currently observed warm conditions, and it is believed that the SST anomalies observed in the next 2-3 months may be warmer than indicated in the coupled model SST forecast. Warmer than average SSTs continue to dominate much of the central and western Indian Ocean. These are expected to decrease slowly through the forecast period. There are currently no substantial SST anomalies in the tropical Atlantic Ocean, but this may change near the end of the forecast period as the northern tropical Atlantic frequently develops warm SST anomalies in the February-May season in response to El Nino conditions in the Pacific (note, however, that these are not represented in the SST forecasts made this month).

METHODS -

This Outlook was prepared using the following procedures and information:

A) Coupled ocean-atmosphere model predictions of tropical Pacific SST covering the forecast period. Particularly heavy weighting has been given to predictions from the coupled model operated by the NOAA National Centers for Environmental Prediction, Climate Modeling Branch. This model suggests a continuation of near-average conditions during the first forecast season. The forecast for near-neutral conditions is consistent with some, but not all, numerical and statistical forecasts of central and eastern Pacific SSTs.

B) Forecasts of the tropical Indian ocean using a statistical model developed by the IRI.

C) Global atmospheric general circulation model (GCM) predictions of the atmospheric response to the present and predicted sea-surface temperature patterns.

D) Other sources of information include NASA's Seasonal to Interannual Prediction Project (GSFC-NASA) and also seasonal prediction research at COLA.

The procedures, models, and data used to derive this Climate Outlook may be somewhat different from those used by the national meteorological services in the region. Thus, this product may differ from the official forecasts issued in those areas. The Climate Outlook for December 2002 - May 2003 is dependent on the accuracy of the SST predictions. For the tropical Pacific, these predictions can be expected to provide useful information, but there is some uncertainty concerning the evolution of SSTs. Spread in global SST predictions is a source of uncertainty in the Outlook provided here. Note that even if perfectly accurate SST forecasts were possible, there would still be uncertainty in the climate forecast due to chaotic internal variability of the atmosphere. These uncertainties are reflected in the probabilities given in the forecast.

It is stressed that the current status of seasonal-to-interannual climate forecasting allows prediction of spatial and temporal averages, and does not fully account for all factors that influence regional and national climate variability. This Outlook is relevant only to seasonal time scales and relatively large areas; local variations should be expected, and variations within the 3-month season should also be expected. For further information concerning this and other guidance products, users are strongly advised to contact their National Meteorological Services.

OUTLOOK -

This Outlook covers four seasons: December-February 2003, January-March 2003, February-April 2003 and March-May 2003. Maps are given showing tercile probabilities of precipitation and temperature. The maps for precipitation indicate the probabilities that the seasonal precipitation will fall into the wettest third of the years (top number), the middle third of the years (middle number), or the driest third of the years (bottom number). The color shading indicates the probability of the most dominant tercile -- that is, the tercile having the highest forecast probability. The color bar alongside the map defines these dominant tercile probability levels. The upper side of the color bar shows the colors used for increasingly strong probabilities when the dominant tercile is the above-normal tercile, while the lower side shows likewise for the below-normal tercile. The gray color indicates an enhanced probability for the near-normal tercile (nearly always limited to 40%). As before, numbers and their associated histograms show the probabilities of the three terciles. In areas with lots of spatial detail, there may not be sufficient room on the map, to allow histograms for each region. In those cases, some idea of the probabilities may be gained from the color alone. A qualitative outlook of climatology ("C") indicates that there is no basis for favoring any particular category. Areas that are marked by "D" represent regions for which less than 3cm of precipitation typically occurs over the season. Otherwise, for example, in the case of the western portion of Western Autralia in December-February 2003 (Map A), there is a 25% probability that the precipitation will be in the wettest third of the years, a 35% chance it will be in the near-normal third of the years, and a 40% chance that the precipitation will be in the driest third of the years.

Maps of temperature show expected probabilities that the seasonal temperatures will fall into the warmest third of the years, the middle third of the years, or the coldest third of the years (Map A). The numbers for each region on the temperature maps indicate the probabilities of temperatures to fall in each of the three categories, above-, near-, and below-normal.

An additional precipitation map is provided for the first season indicating probabilities for extreme precipitation anomalies. Extremes are defined as anomalies that fall within the top and bottom 15th percentile of the observed records. A priori, there is a 15% probability of being within the extremely wet category, and a 15% probability of being within the extremely dry category, leaving a 70% probability that the precipitation will not be extreme. The maps indicate areas of increased risk of extreme precipitation totals. Three levels of increased risk are defined: slightly enhanced risk, enhanced risk, and greatly enhanced risk. For slightly enhanced risk, there is a 25-40% probability that precipitation will be within the indicated extreme, i.e. wet or dry. This represents an approximate doubling of the climatological risk. For enhanced risk, there is a 40-50% probability that precipitation will be within the indicated extreme. This represents an approximate tripling of the climatological risk. For greatly enhanced risk, the probability that precipitation will be within the indicated extreme exceeds 50%, i.e. the indicated extreme is the most likely outcome. A similar map is provided in the first season indicating probabilities of extreme temperature anomalies.

Boundaries between sub-regions should be considered as transition zones, and their location considered to be only qualitatively correct.

December-February 2003 through March-May 2003:

The following discussion briefly describes the probability anomaly forecasts:

Enhanced probabilities for below normal precipitation are forecast for much of Indonesia and for the northern, western and eastern coastal regions of Australia for most of the four forecast periods, in association with the moderate El Nino. This is most strongly the case in the first two of the four periods. During the third and fourth forecast periods, the portion of Indonesia with enhanced probabilities for below normal precipitation moves northward, and a region along the southern coast of Australia begins having enhanced probabilities for above normal precipitation. Enhanced probabilities for above normal precipitation are forecast for the tropical Pacific islands along the immediate equator in the western part of the Pacific Basin, while the opposite tendency is noted for islands well south of the equator (e.g. Fiji).

An enhanced probability for above normal temperature is forecast for much of Australia for all four forecast periods (but less so in the fourth period), with the exception of portions of the southern coast and Tasmania where en enhanced probability for below normal temperature is forecast for the first three forecast periods. An enhanced probability for below normal temperature is forecast for central Indonesia for the second, third and fourth forecast periods, with the opposite tendency being forecast for the first period and for western Indonesia and Papua New Guinea for all four forecast periods.

OBSERVED CLIMATOLOGY DATA for Dec-Jan-Feb, Jan-Feb-Mar, Feb-Mar-Apr and Mar-Apr-May