Special Report: COLA Regional Forecast for Winter 1998 - North America

The Center for Ocean-Land-Atmosphere Studies, as part of its ongoing research into the predictability of seasonal to interannual climate variations, has prepared a forecast for the winter mean (January - March 1998 average conditions) based on information available as of 31 August 1997 (5-7 months lead forecast).

The forecast was prepared by first making a long lead forecast of the tropical Pacific sea surface temperature anomaly (SSTA) using an anomaly coupled model of the Earth's climate. More information on the anomaly coupled model and the latest forecast of Pacific SSTA are available. The Pacific SSTA forecast of the anomaly coupled model is statistically projected to estimate the global SSTA. The later is then applied as a lower boundary condition to the COLA global atmospheric general circulation model (AGCM) to produce a forecast of the large scale global atmospheric circulation and precipitation. The U.S. National Weather Service Environmental Modeling Center's Eta model is nested in the COLA AGCM global forecast to produce a more detailed forecast over North America.

Temperature

This nested model forecast calls for generally warmer than normal conditions over most of North America (Figure 1). The bulk of the continental U.S. and Canada are predicted to experience warmer than normal seasonal average temperatures by at least 20° F. The largest departure from normal in the U.S. is in the northern plains where temperatures are forecast to be as much as 4-6° F above normal. Over the continent as a whole, the largest anomaly is forecast to occur in northern central Canada, where the temperature is predicted to exceed its normal value by more than 6°F above normal.

 

These warm temperature anomalies are smaller and somewhat different in structure than those forecast by the COLA AGCM alone, which can be easily seen in the Nested model minus COLA AGCM difference in the forecast temperature anomaly (Figure 2). The warm temperature anomaly over Canada is up to 6°F less in the nested model and over the southern U.S. the nested model is 2°F warmer than the AGCM alone.

 

Precipitation

The predicted precipitation (Figure 3) is generally above normal for the southern U.S. and Mexico and below normal for the northern U.S. and southern Canada. The extreme values for the seasonal average are forecast for northern California where over 20 inches more than the normal precipitation is predicted. The southwest U.S. and the states bordering the Gulf of Mexico are expected to receive over five inches more than normal precipitation for the season. Reductions in precipitation from the normal precipitation are forecast in the maritime provinces of Canada and parts of the Canadian Rockies; however, these anomalies are modest in magnitude (about two inches below normal for the entire season).

 

Although these forecast anomalies appear similar to those forecast by the AGCM alone, there are important differences between the two precipitation anomaly forecasts (Figure 4). The nested model forecasts two to five inches less excessive precipitation throughout much of the western U.S. and Canada and five to ten inches less precipitation along the Sierra Nevadas and northern Mexico. However, in northern coastal California the nested model forecasts a precipitation anomaly of over 20 inches, roughly double that predicted by the AGCM alone. The nested model also tends to forecast less anomalous precipitation over the central U.S. and Canada.

In discussion of any climate forecasts produced by a numerical model, it must be stressed that there is a substantial element of uncertainty in any such product.

The calculations required to produce this forecast were conducted as part of the Dynamical Seasonal Prediction project. Computing resources were provided at the Climate Simulation Laboratory of the National Center for Atmospheric Research Scientific Computing Division, and they are gratefully acknowledged.


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