What to expect this winter: NOAA’s outlook reveals what conditions are favored across the US
Four years of drought in California. Back-to-back cold and snowy winters over the Midwest and Northeast, while balmy in the West. What’s next, thunder, hail, or maybe locusts and frogs? Or will this winter bring more “normal” winter weather? Actually thunder and hail isn’t too far-fetched this winter, at least in the Southeast, but more about that later. The jury’s still out on the locusts and frogs. So what can we expect this winter?
Since this post is appearing on the ENSO blog, readers are well aware that El Niño developed last spring and is currently among the strongest events on record back to 1950. In addition, previous posts have discussed how El Niño can impact the weather and climate over the United States, particularly during winter. El Niño in general acts to tilt the odds toward wetter and cooler than average conditions across much of the South, and toward drier and warmer conditions in many of the northern regions. These effects vary from one El Niño to another, however.
Starting with precipitation, the figure below shows winter (December-February) differences from average precipitation for 20 El Niños between 1950 and 2010. The precipitation departures are in shown in order from the strongest event (1997/98) to one of the weakest (2004/05) (1).
The most consistent signal is along the Gulf Coast, where almost all of the strong episodes were associated with greater than average precipitation. Other fairly reliable signals for the stronger events include a tendency for below average precipitation in the Ohio and Tennessee Valleys and above-normal precipitation in southern California and the Southwest. Of course, these impacts are not ensured during every El Niño, not even the strongest ones.
The companion temperature figure shows more variability than the precipitation maps, even for just the 6 strongest episodes. The CPC forecasters take this greater variability into account which helps explain why forecast probabilities tend to be a bit higher for a precipitation outlook than a temperature outlook during El Niño winters.
For the six strong events, three of them (1997/98, 1982/83, and 1991/92) are very similar with a dearth of below-average temperatures as much of the country (especially in the northern and central regions) experienced above-average temperatures. However, somewhat surprising is the generally cooler appearance in the other three cases, all prior to 1980. Admittedly it’s not wise to draw conclusions from such a small number of events, but it’s interesting that there may be decadal variability, which are ups and downs acting on a much longer (10 or more year) time scale, superimposed on these six cases, something not evident in the precipitation cases.
Although the seasonal outlooks issued by the Climate Prediction Center (CPC) are based on more than just El Niño, during a strong event, like the one we’re having, it certainly plays a large role. Still, CPC forecasters consider other factors, such as long term trends, as well as input from a suite of statistical tools and dynamical models.
And before discussing the actual winter outlook, I want to remind folks that these are tercile-based probabilistic outlooks with the most likely of the three categories (below normal, near normal, and above normal) shown on the maps (2). “Tercile-based” means that at every location, the forecast includes three probabilities: the chance for precipitation that is below average by a sufficient margin to be in the wettest one-third of the historical record, the chance for likewise except above average, and the chance for near-average precipitation (i.e., in the middle one-third of the historical record). We can’t put all three colors on the map in the same place, so we choose the color based on the category having the highest probability.
In other words, this does not mean that if you’re in a particular location that has a color on it, you will definitely experience climate departures that match the color. The outlooks show the most probable outcome, which means—as we’ve explained in earlier blog posts—that there is still always a chance that a less favored outcome will occur.
The CPC winter precipitation outlook favors wetter-than-normal conditions across the southern tier of the nation extending northward along the East Coast, and in southeastern Alaska. Drier-than-normal conditions are favored in western and central Alaska, Hawaii, parts of the Pacific Northwest and northern Rockies and around the Great Lakes and Ohio Valley. This pattern is quite consistent with the average precipitation patterns seen during previous El Niño winters.
Probabilities are quite high this year across parts of the country—particularly in the Southeast, where the chance of a wetter-than-normal winter exceeds 70% for much of Florida (3). And while this is not something that CPC specifically forecasts at this time, this area also has the potential to see severe weather, since during El Niño winters, organized tornado activity is often restricted to the area immediately adjacent to the Gulf of Mexico (Cook and Schaefer 2008, Allen et al. 2015).
The chance of a wetter-than-normal winter exceeds 50% from the Southeast coast, along the Gulf Coast, across most of Texas, and through the Southwest to southern California. This is certainly positive news for California, although even a wet winter would be very unlikely to eradicate 4 years of drought. But you’ve got to start somewhere. On the flip side, the largest probabilities for below-average precipitation exceed 50% in the Northern Rockies, a region where drought has recently developed and is likely to persist or intensity through the winter.
The temperature outlook favors a warmer-than-normal winter over Alaska, much of Hawaii, the Western United States, and across the northern half of the contiguous U.S., while below-normal temperatures are favored across much of the south-central and southeastern regions. Probabilities for above-normal temperature exceed 60% in the Pacific Northwest, the Alaskan Panhandle and the extreme northern Great Lakes (4).
The chance of a milder-than-normal winter in the Northeast is also enhanced (5), because it exceeds 33.33%, but is less than 50%. The likelihood of below average temperatures across the South is also enhanced but less than 50%. Also note that both maps include areas where neither above- nor below-normal is favored. Those areas are shown in white, which represents “equal chances,” and it means that the odds for below-, near-, or above-normal conditions are all equal, at 33.33% (6). The “equal chances” forecast means that upon considering all of the relevant factors, we see no reason for favoring any of the three categories.
Making seasonal forecasts is a very challenging endeavor. Seasonal climate models are not as skillful as weather models, and phenomena like El Niño or La Niña only provide clues as to what might occur during an upcoming season, although the occasional strong episode certainly provides stronger clues than usual. CPC issues probabilistic seasonal forecasts so users can take risk and opportunities into account when making climate-sensitive decisions. However, probabilities this winter are as high as you’ll ever see for a seasonal outlook, so if I were ever going to pay attention to them, this would be the year. If you live somewhere in the South and were thinking about replacing your roof in the next 6 months, I might do it before winter, instead of waiting until afterward.
(1) This list is slightly different from what appeared last June, as the underlying data set used to calculate our Oceanic Niño Index (ONI; the 3-month average SST departure from average in the NINO3.4 box in the east-central tropical Pacific) was changed, shuffling a few of the episodes around. Also, note that these years are ranked by the peak ONI value that was achieved during the second half of the year or very early in the following year, which may not be in DJF.
(2) The terciles are the boundaries that define three categories of the precipitation or temperature: “below normal (A)”, “near normal (N)” and “above normal (A)”. The two tercile boundaries (one separating B and N, the other separating N and A) are defined such that over a recent 30-year historical period, one-third of the years (10 out of the 30) have been in each of the three categories. The tercile-based probability forecasts then consist of the probabilities that the precipitation or the temperature will be in each of the three categories. In order to show the forecast on a single map, only the probabilities of the most likely category are shown. However, the probabilities for the less likely categories are also defined, even though they are not shown on the map. The white areas on the map show where all three probabilities are forecast with equal probability (33.3%).
(3) This also means that the likelihood of a drier-than-normal winter is very low, only 3% (although still not zero).
(4) This means that for these regions, in addition to a fairly high chance of a warmer-than-average winter, there’s also less than a 10% chance winter temperatures will be in the below normal category.
(5) Any probability above 33% is considered “enhanced,” because 33% is the expected climatological average probability when there are designed to be three historically equally likely categories. When the probability is above 33% but less than 50%, the given category has higher probability than its historical 33% average, but may be the most likely of the three categories but is nonetheless more likely not to occur than to occur. This effect from the use of three categories, instead of just two (such as simply “below average” vs “above average), is a source of confusion for some readers and users of the forecast.
(6) This “equal chances” forecast means that there’s no tilt in the odds toward any of the 3 categories. Note that this does not indicate a preference for the near normal category, as either of the other two categories is also equally likely. It indicates an informed “we do not know.” By “informed” we mean that we did our homework and still find no cause for favoring any of the categories over the others.
Lead reviewer: Tony Barnston, IRI.
A. R. Cook and J. T. Schaefer, 2008: The Relation of El Niño–Southern Oscillation (ENSO) to Winter Tornado Outbreaks. Mon. Wea. Rev., 136, 3121–3137.
Allen, J.T., Tippett, M.K., Sobel, A.H. (2015). Influence of the El Niño/Southern Oscillation on tornado and hail frequency in the United States. Nature Geoscience, 8, 278–283.
The ENSO blog is written, edited, and moderated by Michelle L’Heureux (NOAA CPC), Emily Becker and Tom DiLiberto (contractors to CPC), Anthony Barnston (IRI), and Rebecca Lindsey (contractor to NOAA CPO). Posts reflect the views of the bloggers themselves and not necessarily Climate.gov, NOAA, or Columbia University/IRI.