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La Niña: Canadian Perspective

Wind, water and temperature are part of an intricate set of connected elements that affect weather patterns around the globe. Weather events half-way around the world can affect local forecasts. Perhaps the most striking examples of weather phenomena affecting global climate are El Niño and La Niña.

Environment Canada scientists are tracking the 1998-99 La Niña. In Canada, La Niña can bring considerable fluctuations in weather patterns. However, most La Niña winters tend to be colder and snowier than normal.

Most of the prediction models are indicating that the easterly trade winds in the tropics would strengthen. This will intensify the up-welling of cold waters in the eastern Pacific. A moderate strength La Niña is possible during the winter of 1998-99, but considerable uncertainty remains about the timing and strength of the event. The response of the global atmospheric circulation and its effects on Canadian winter weather conditions is even more uncertain.

What is La Niña?

La Niña is an extensive cooling of the central and eastern Pacific Ocean. La Niña is also characterized by climate conditions that are sometimes opposite to those of El Niño (which brings warm ocean temperatures in the equatorial Pacific).

La Niña occurs when easterly trade winds in the tropics strengthen, intensifying the up-welling of cold waters off the coast of Peru and Ecuador. During La Niña, sea surface temperature can fall as much as 4 °C below normal.

The effects of La Niña are strongest during the Northern Hemisphere winter. While La Niña occurs less frequently than El Niño, weather patterns over North America associated with La Niña tend to be more variable.

During La Niñas snowfall is abundant from the interior of British Columbia to the Great Lakes region. In the United States, winters are warmer and drier than normal in the Southeast and cooler and wetter than normal in the Northwest.

How does this year's La Niña compare with other La Niñas?

In May, water temperatures in the eastern tropical Pacific showed a rapid transition from El Niño to La Niña like conditions. The water temperatures dropped by 8 °C to reach 2-3 °C below normal in a few weeks. Since mid June however, there has been little change. Recent satellite imagery from NASA indicates that warm waters from the 1997-98 El Niño continues to linger in parts of the eastern tropical Pacific and raises questions about the strength and timing of the emerging La Niña. Since 1976, there have been considerably fewer La Niñas compared to El Niños - the previous strong La Niña occurred 10 years ago (1988-89).

What are La Niña's global impacts?

The effects of La Niña are generally more direct and dramatic during the Northern Hemisphere winter. La Niñas may also affect weather patterns in other parts of the world, sometimes causing abnormally high rainfall in Southeast Asia and dry conditions in the desert areas of South America. Some impacts of previous La Niñas include the following:

What has been the impact of previous La Niñas in Canada?

There have been 17 moderate-to-strong La Niñas since the 1900's. Each La Niña has its own unique characteristics, affecting Canada's weather patterns in different ways. These are some major weather events from the last two La Niñas in Canada.

La Niña 1995-96:

La Niña 1988-89:

Average winter conditions during past La Niñas

• The numbers indicate degrees Celsius by which the temperatures depart from normal.
• Environment Canada's official forecast for the 1998-99 winter can be viewed at http://weatheroffice.ec.gc.ca/saisons/index_e.html

Is there a link between climate change and La Niña?

Scientists are questioning whether climate change influences changes in climate associated with El Niño or La Niña. There is no consensus yet on any direct link. However, scientists are pursuing further research in order to provide confident answers to these questions.

Quick facts

For Further Information

Amir Shabbar
Environment Canada
(416) 739-4435

La Niña Web site :
http://www.tor.ec.gc.ca/lanina/


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Created : 2002-08-23
Modified : 2002-12-18
Reviewed : 2002-12-18
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