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WESTERN PRODUCER — Most of us know about El Nino, an unusual warming of the central and eastern parts of the equatorial Pacific Ocean. This warming changes the general circulation of the atmosphere over the Pacific.

The recent El Nino helped drive nearly two years of temperature records we just experienced.

La Nina is the opposite. It means the little girl, and can sometimes be called El Viejo, the anti-El Nino, or simply a cold event.

It occurs when strength increases in the normal pattern of trade wind circulation. Under normal conditions, these winds move westward, carrying warm surface water to Indonesia and Australia and allowing cooler water to upwell along the 麻豆传媒AV American coast.

When a La Nina event occurs, these trade winds are stronger, which helps increase the amount of upwelling. This creates more cool water along the coast of 麻豆传媒AV and Central America and builds up warmer water on the western side of the Pacific Ocean.

On the western side of the Pacific, the influx of warmer water causes an increase in cloud over 麻豆传媒AVeast Asia and results in wetter than normal conditions for that region during the Northern Hemisphere winter.

What does this have to do with our weather in Western Canada? Changes in the tropical Pacific are usually accompanied by large changes in the jet stream across the mid-latitudes (our part of the world), shifting the usual location of the jet stream across North America.

This can contribute to large changes in the normal location and strength of storm paths and can cause temperature and precipitation anomalies over North America that can persist for months. These changes are most strongly felt in the winter.

According to the latest La Nina advisory, nearly all models predict it will continue through early 2025. The different models disagree over the eventual strength of this La Nina event, but recent data suggests it will be weak and short-lived.

This would likely result in limited impact on our weather this winter, so confidence in the long-range forecast is low. Let’s look at what has happened during previous La Nina winters.

Sometimes it easier to show the impact of different weather events with a map. The acommpanying map shows the typical impact on our weather during a La Nina winter across Canada and the U.S. Typically we see colder than average temperatures, as indicated in the long-range computer forecasts. In our recent winter weather outlook, the computer models almost all predicted a warm start to the winter, followed by colder than average conditions in the second half.

The map shows a strong La Nina, but it looks like we will only see a weak one this winter. In the last dozen weak La Ninas, six brought near- to below-average temperatures, five were near- to above-average, and one saw above-average temperatures over the eastern prairies and below-average temperatures over western regions.

Statistically, this does not help much in predicting this winter’s temperature forecast.

What about snowfall? During a weak La Nina winter we will, on average, see above-average snowfall over most of Alberta and parts of extreme southern Saskatchewan, along with the north-central parts of Saskatchewan.

The rest of south-central Saskatchewan and southern and central Manitoba typically see below-average snowfall.

A map that depicts the difference from average snowfall across Canada and the U.S. during the previous nine weak La Ninas would show a band of above-average snowfall to our south. It wouldn’t take much of a northward nudge to put the southern Prairies into above-average snowfall.

It will be interesting to watch how this winter plays out.

Daniel Bezte is a teacher by profession with a BA in geography, specializing in climatology, from the University of Winnipeg. He operates a computerized weather station near Birds Hill Park, Man. Contact him at [email protected].

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