CPC ENSO Alert System Status: La Niña Advisory
Synopsis: La Niña is expected to last at least through the Northern Hemisphere winter 2010-11.
La Niña strengthened during August 2010, as negative sea surface temperature (SST) anomalies reached at least -1oC across most of the equatorial Pacific Ocean by the end of the month (Fig. 1). All of the Niño indices cooled to between –1.3oC and –1.8oC by the end of August (Fig. 2). Consistent with this evolution, the subsurface heat content (average temperatures in the upper 300m of the ocean, Fig. 3) decreased further, reflecting the additional cooling of sub-surface waters east of the Date Line (Fig. 4). Also convection was enhanced over Indonesia, while remaining suppressed over the western and central equatorial Pacific (Fig. 5). The pattern was associated with the continuation of enhanced low-level easterly trade winds and anomalous upper-level westerly winds over the western and central equatorial Pacific. Collectively, these oceanic and atmospheric anomalies reflect the strengthening of La Niña.
Nearly all models predict La Niña to continue at least through early 2011 (Fig. 6). However, the models continue to disagree on the eventual strength of La Niña. Based on current observations and model guidance, we expect the SST anomalies in the Niño-3.4 region to either persist near the present strength, or to strengthen into the winter as is consistent with the historical evolution of La Niña. Thus, it is likely that the peak strength of this event will be at least moderate (3-month average between –1oC to –1.4oC in Niño-3.4) to strong (3-month average of –1.5oC or less in Niño-3.4).
Expected La Niña impacts during September-November 2010 include suppressed convection over the central tropical Pacific Ocean, and enhanced convection over Indonesia. The transition into the Northern Hemisphere Fall means that La Niña will begin to exert an increasing influence on the weather and climate of the United States. These impacts include an enhanced chance of above-average precipitation in the Pacific Northwest, and below-average precipitation in the Southwest and in portions of the middle and lower Mississippi Valley and Tennessee Valley. Also, La Niña can contribute to increased Atlantic hurricane activity by decreasing the vertical wind shear over the Caribbean Sea and tropical Atlantic Ocean (see the August 5th update of the NOAA Atlantic Seasonal Hurricane Outlook), and to suppressed hurricane activity across the central and eastern tropical North Pacific.
La Niña impacts across the region include an increased risk of extreme precipitation events, as well as an enhanced threat for more frequent cold snaps. The trend for more frequent cold snaps continues into the following spring as well, but the threat for extreme precipitation events decreases. Extreme is defined as being in the highest or lowest 20% of the 100 year record. In other words, the statistical likelihood for a major snowstorm in any given winter season is 50/50. During La Niña winters, the threat is more than doubled. The graphics below, provided by the NOAA/ESRL Physical Sciences Division, Boulder Colorado from their Web site at http://www.esrl.noaa.gov/psd/ show the relative threat for a colder and snowier than normal winter when there is a La Niña ongoing in the Pacific.
Risk of extreme cold weather during the December-February time period during La Niña
Risk of extreme precipition during the December-February time period during La Nina
Risk of extreme cold weather during the March-May time period during La Niña
Risk of extreme precipitation during the March-May time period during La Niña
Image provided by the NOAA/ESRL Physical Sciences Division, Boulder Colorado from their Web site at http://www.esrl.noaa.gov/psd/
This discussion is a consolidated effort of the National Oceanic and Atmospheric 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 7 October 2010. To receive an e-mail notification when the monthly ENSO Diagnostic Discussions are released, please send an e-mail message to: firstname.lastname@example.org. For more information on the local impacts of La Niña, contact Mark Ewens, Climate Services Program Leader at 701.795.5198 or at Mark.Ewens@noaa.gov