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North America
Summary:
A negative phase of the Pacific/North American (PNA) pattern is
forecast, which translates into an anomalously cold winter over much of
the western part of North America. Anomalously mild winter is expected
for the southeastern and (with less confidence) southwestern United
States.

Fig.
1. The forecast of surface air temperature
anomalies in North America in the winter (DJF) of 2008. The
blue (red) contours and the letter C (W) indicate colder (warmer) than
normal temperatures. CL means near normal. The base period for
calculating anomalies is 1971-2000. The numbers at the contours
are confidence
factors of the forecast.
Discussion
The
atmospheric circulation over North America
will resemble a negative phase of the Pacific/North
American (PNA) pattern. This phase of the PNA pattern is characterized
by a frequent upper atmospheric troughing in the west and ridging in
the
east of the continent. This leads to relatively more frequent outbreaks
of cold air
in the west and less frequent in the east. See more information about
the PNA
at the CPC
website.
Two major contributors to this state of the PNA
pattern
are: 1) the La Niña event in the equatorial Pacific and 2)
the
negative phase of the Pacific Decadal Oscillation (PDO) (see the latest forecasts
for the ENSO and PDO). An analysis of a cumulative effect of other
factors (briefly discussed below) also suggests that the negative phase
of the PNA is more likely.
One of the rules that were used in this forecast
represents a tree-structured statistical model that links the
quasi-biennial oscillation (QBO) in the stratospheric winds and
year-to-year changes in the PNA index (Rule 202). This model suggests a
high probability of a decrease in the PNA index compared to the last
winter. A similar conclusion can be made based on an extrapolation,
which makes use of an internal structure of the PNA time series. When
the index decreases, there is an almost 80% chance that it will become
negative.
A number of rules, however, point to a possibility of a positive PNA
index in 2008. One of those rules describes a statistically significant
correlation found between the PNA and the North Atlantic Oscillation
(NAO) indices, with the latter leading the former by 3 years (Rule 35).
In 1995, the NAO index was positive, and this suggests the PNA index
may be positive in 2008. Two other factors, surface air temperature
(SAT) in Greenland (Rule 199) and the Gulf of Mexico (Rule 200), act in
favor of a positive PNA index as well. Due to the low confidence
factors for these rules, however, their effect of the PNA forecast is
relatively weak, and the evidence remains quite solid that the negative
PNA index is more likely in 2008.
This PNA forecast is consistent with the forecast of winter SAT
anomalies in the southeastern US. The latter forecast takes
into
account the state of the NAO, which is expected to be positive (see the
winter 2008
forecast for the North Atlantic).
Also, a quite strong relationship for the winter temperature in the
Southwest was found with the QBO (Rule 31) and a weaker relationship
with the Eurasian snow cover (Rule 27). Both rules suggest an
anomalously mild winter for the region.
In the early fall of 2007, the distribution of sea surface temperature
(SST) anomalies in the North Atlantic will be reviewed, which may
correct the outlook for the winter of 2008. Currently, the so-called
“horseshoe” pattern is forming there, and if this
pattern
remains unchanged through the summer and early fall, a warmer than
normal winter can be expected in the southwestern US.
Significant uncertainty exists in the forecast for the Midwest and Ohio
Valley region. The Climate
Prediction Center (CPC) outlook
calls for positive SAT anomalies in these regions calculated as
departures from the 1971-2000 climatology. This is a relatively safe
forecast given a strong positive temperature trend since the late
1970s. For example, in the central climatological region (click here
to see the region map), only 4 out of 19 winters since 1989 were colder
than the average temperature for the period 1971-2000. Our forecast
predicts some cooling in this region, with SAT anomalies below the
average for the past ten years and probably close to the average for
the period 1971-2000.
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Season: |
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Winter (DJF) 2008
Forecast
issued: June 7, 2007
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