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El Niño's Influence on WNY's Winter Weather

Over the past twenty five years there has been a dramatic increase in the research and understanding about the effects of long term global weather (e.g. climate) phenomena on sensible everyday weather. This is especially the case with El Niño Southern Oscillation (ENSO). While ENSO refers to a climate process based in the Equatorial regions of the
Pacific Ocean, its effects reach halfway around the globe to Western and North Central New York.

ENSO is currently in its warm phase. This is referred to as El Niño. During stronger El Nino events winter temperatures across Western and North Central New York typically average above normal, while weak El Niño’s tend to help produce neutral to below normal temperatures. Graphs shown below indicate these temperature trends for Buffalo, Rochester and Watertown. Unlike temperatures which show a moderate correlation to
stronger El Niño events, snowfall shows a very poor correlation.

The temperature information found within the graphs was obtained by matching the various strengths of El Niño (as determined by the Climate Prediction Center) to the corresponding monthly temperatures, then taking the difference between the mean of the monthly temperatures  versus the 30 year normal.


El Niño 
City Comparisons by Month

City El Nino Comparisons by Month

El Niño 
Monthly Comparisons by City

Monthly El Nino Comparisons by City

 El Niño 
Overall Temperature Departures

Overall El Nino Temperature Departures


EL NIÑO/SOUTHERN OSCILLATION (ENSO)
DIAGNOSTIC DISCUSSION
issued by
CLIMATE PREDICTION CENTER/NCEP
March 6, 2008
 

Synopsis: La Niña is expected to continue through the Northern Hemisphere spring 2008.

Atmospheric and oceanic conditions during February 2008 continued to reflect a strong La Niña. Equatorial SSTs were more than 2.0°C below average across large portions of the central and east-central equatorial Pacific (Fig. 1), and the corresponding weekly values of the Niño-4 and Niño-3.4 indices remained between -1.6°C and -2.1°C during the month (Fig. 2). In contrast, SSTs in the far eastern equatorial Pacific were above average during February 2008, in association with a warming trend that began in mid-December. The upper-ocean heat content (average temperatures in the upper 300m of the oceans between 180° - 100°W) remained below average across the equatorial Pacific during February (Fig. 3), with the largest temperature anomalies averaging -2°C to -6°C at thermocline depth (Fig. 4). Consistent with these oceanic conditions, stronger-than-average low-level easterly winds and upper-level westerly winds persisted across the central equatorial Pacific, convection remained suppressed throughout the central equatorial Pacific, and enhanced convection covered the far western Pacific. Collectively, these oceanic and atmospheric conditions are similar to those accompanying the last strong La Niña episode in 1998-2000.

The most recent dynamical and statistical SST forecasts for the Niño 3.4 region continue to indicate a moderate-to-strong La Niña through March 2008, and a weaker La Niña through April-May-June 2008 (Fig. 5). Thereafter, there is considerable spread in the forecasts, with approximately one-half indicating that La Niña could continue into the Northern Hemisphere fall. Current atmospheric and oceanic conditions and recent observed trends support the likely continuation of La Niña through the Northern Hemisphere spring 2008.

Expected La Niña impacts during March-May 2008 include a continuation of above-average precipitation over Indonesia and below-average precipitation over the central equatorial Pacific. The above average SSTs in the eastern equatorial Pacific may result in increased rainfall over Ecuador and northern Peru, similar to the evolution during the 1998-2000 La Niña episode. Compared to the Northern Hemisphere winter, La Niña impacts over the United States in spring are typically less pronounced. The primary springtime signal for the contiguous United States is an increased probability of below-average precipitation across the South, particularly in the Southeast.

This discussion is a consolidated effort of the National Atmospheric and Oceanic Administration (NOAA), NOAA’s National Weather Service, and their funded institutions. Oceanic and atmospheric conditions are updated weekly on the Climate Prediction Center web site (El Niño/La Niña Current Conditions and Expert Discussions). Forecasts for the evolution of El Niño/La Niña are updated monthly in the Forecast Forum section of CPC's Climate Diagnostics Bulletin. The next ENSO Diagnostics Discussion is scheduled for 10 April 2008. To receive an e-mail notification when the monthly ENSO Diagnostic Discussions are released, please send an e-mail message to: ncep.list.enso-update@noaa.gov.


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