U.S. Winter Outlook Dominated by Dire Drought News
- Published: November 21st, 2013 , Last Updated: November 21st, 2013
By
Andrew Freedman
Follow @afreedma
Drought, and not widespread snowstorms, may be the biggest story this winter according to the official U.S. winter outlook.
The
outlook, issued by the
National Oceanic and Atmospheric Administration (NOAA) on Thursday, shows that the winter of 2013-14 is likely to feature an expansion and intensification of drought conditions across the Southwest and Southeast. That includes California, which has had its driest year on record so far in 2013, and which needs sufficient mountain snowfall this winter to prevent water supply shortages during the summer months.
Temperature outlook for the winter of 2013-14.
Click image to enlarge. Credit: NOAA.
As was the case last winter, the lack of an El Niño or La Niña event in the tropical Pacific Ocean has introduced more uncertainty into the forecast, since those events typically influence temperature and precipitation patterns across the U.S.
“Despite recent advancements, this year’s outlook has again proven to be quite challenging,” said Mike Halpert, the acting director of NOAA’s
Climate Prediction Center in Maryland.
In the absence of a clear signal from the tropical Pacific Ocean, NOAA based its outlook on factors that have a less definitive influence for much of the U.S., including long-term trends and computer models used for long-range forecasting.
The outlook calls for below-average precipitation in the Southwest, where many states have been suffering from a multi-year drought, as well as below-average precipitation in the Southeast. In addition to California, the winter outlook is especially unwelcome news in Texas, where a
3-year drought has led to unprecedented
water restrictions in the state capital of Austin and many other communities. After the drought eased somewhat during the fall, the winter outlook forecast calls for the re-expansion and intensification of drought during the winter.
The only areas of the country that NOAA outlined for above-average precipitation this winter are in Montana, Wyoming, and Hawaii.
Forecasters are expecting a colder-than-average winter in the Northern Plains, with milder-than-average conditions in the Southwest, South Central states, Southeast, New England, and Western Alaska. The forecast also calls for a warmer-than-average winter in the Northeast, and a separate drought outlook also issued on Thursday shows drought conditions
will persist in a small but highly populated area from New York City to Boston to Portland, Maine.
Precipitation outlook for the winter of 2013-14.
Click image to enlarge. Credit: NOAA.
The rest of the country, though, falls into the “equal chances” category for precipitation and temperature, which means that there are equal probabilities for above-average, average, or below-average temperatures. This isn’t the same thing as projecting an “average” winter, but rather an indication that there was not enough evidence to tilt the odds in favor of a particular outcome.
The forecast covers meteorological winter, which runs from December through February. Based on more accurate short-range forecast techniques, meteorologists at NOAA and in the private sector are convinced that the winter will start off
colder-than-average from the Central U.S. to the East, but that after mid-December, it may warm again in at least parts of those areas.
“Our methods indicate a higher probability that cold might linger into mid-December, but then all bets are off after that,” said Stephen Bennett, the president and founder of
EarthRisk Technologies in San Diego, which forecasts the likelihood of extreme weather events up to a month in advance.
The Arctic Oscillation: Emerging Research Left Out of Official Outlook
In making its winter outlook, there is some information that NOAA did not take into account that could potentially improve its forecast accuracy and reduce the area of “equal chances” on the map.
In addition to El Niño and La Niña, a weather pattern known as the
Arctic Oscillation, or AO, also influences winter weather in the eastern U.S. When the AO is in a “negative” phase, cold air more readily spills out of the Arctic and into the eastern states. Most of the Mid-Atlantic and Northeast’s snowiest winters have taken place when the AO was negative.
Boston's North End neighborhood amid the snow drifts after a historic blizzard struck in February 2013.
Credit: Twitter via Matt Meister.
When the AO is in a positive phase, however, cold air tends to get bottled up in the Arctic, resulting in milder and drier-than-average conditions along the East Coast.
While NOAA maintains that the AO cannot reliably be predicted more than a week or two in advance, a private forecasting firm,
Atmospheric and Environmental Research (AER), has been using a novel forecast technique during the past several years that has shown considerable success in predicting the tendency of the AO months in advance.
AER’s Judah Cohen and several colleagues developed an index based on the extent and rate of increase in October snow cover in Siberia. That index has shown a promising link to the wintertime AO through a complex series of interactions with the upper atmosphere, particularly the polar vortex, which is a corridor of fast-moving high altitude winds that forms a ring around the frigid Arctic region.
A rapidly advancing and unusually extensive October snow cover, Cohen has found, tends to foretell a winter with a predominantly negative AO, which usually means a colder and snowier-than-average winter in the Northeast and Mid-Atlantic states.
This year, though, while Siberian snow cover wound up being more widespread than usual, it advanced more slowly than normal during October, Cohen said in an interview. Siberian snowfall cover came in at its third highest since 1976, Cohen said, while the snow advance index came in below average, a rare split decision.
Such mixed signals complicated his seasonal forecast, which Cohen has already distributed to clients in the energy sector and other weather-dependent industries. His forecast, like NOAA’s, calls for the likelihood of a milder-than-average winter in the Mid-Atlantic and Northeast.
The correlation between an index capturing the rate of expansion in Siberian Fall snow cover and the phase of the Arctic Oscillation.
Click image to enlarge. Credit: Judah Cohen.
“It looks like the (Northern) Hemisphere wants to go into a positive AO mode, and that would favor warm temps in the Eastern U.S.,” Cohen said, noting the forecast is far from a slam dunk. “The seasonal forecast business is good for humbling (you) and for making you realize what you don’t know,” Cohen said.
NOAA has been reluctant to implement Cohen's methods as a way of improving its winter forecasts, choosing instead to continue to rely almost solely on the tropical Pacific conditions as a forecast basis. That leads to problems during years like this one when there is no El Nino or La Nina present or forecast to develop.
“I certainly think they have been slow — whether it’s justified or not I can’t speak to — in bringing aboard some of the new ideas in the scientific research community,” Cohen said of the Climate Prediction Center.
“No tool is perfect, but there is information there that they’re leaving on the table by just focusing on ENSO,” he said, using the acronym for the larger climate cycle that El Niño and La Niña are a part of, known as the
El-Niño-Southern-Oscillation.
NOAA’s Halpert told reporters on Thursday that NOAA is still researching the potential usefulness of Cohen’s methods. “It is something that we’re still looking at in a research mode. It does look like there is potentially some predictability in the AO,” he said, noting that the forecast issued on Thursday did not include the Siberian snowfall index that Cohen helped develop.
Cohen has also started to incorporate Arctic sea ice extent into his forecasts, given recent research showing that the sharp reduction in sea ice in recent years may be leading to extreme behavior of the AO, with potential links to
blizzards in the Mid-Atlantic and Northeast. During the winter of 2009-2010, for example, the AO was extremely negative, with an unusually mild Arctic but an unusually cold and snowy eastern U.S. and Europe.
This
Warm Arctic/Cold continents pattern is a focus of ongoing research
http://www.climatecentral.org/news/...-role-in-causing-cold-snowy-winters-study-sa/ as Arctic sea ice continues to decline due primarily to manmade global warming.
“Everyone and their grandmother is doing sea ice research (now),” Cohen said.
