Extratropical Highlights
– November 2012
1. Northern Hemisphere
The 500-hPa circulation during November
featured a persistent anomalous zonal wave-4 pattern (Figs. E9, E11).
Aspects of this pattern included above-average heights across the high
latitudes of the North Pacific Ocean, the central U.S., and southwestern
Russia, and below-average heights over the Gulf of Alaska, the southeastern
U.S., the eastern North Atlantic, central Asia, and the western North Pacific (Fig. E9). The
pronounced north-south dipole of height anomalies over the western Pacific
reflected a strong negative phase (-2.0) of the West Pacific teleconnection pattern (Fig. E7, Table E1).
The main land-surface temperature signals
during November included above-average temperatures in the western U.S., across
Europe, and western Russia, and below-average temperatures in Alaska, the
eastern U.S., and central Siberia (Fig. E1). The main precipitation signals included above-average
totals in eastern China, and below-average totals over
the eastern half of the U.S. and the Plains states (Fig. E3) where ongoing precipitation deficits (Fig. E5) have led to a continuation of exceptional
drought conditions.
a. North America
The mean 500-hPa circulation during
November featured a persistent anomalous wave pattern characterized by
above-average heights over the high latitudes of the North Pacific and the
western U.S., and below-average heights over the Gulf of Alaska and the
southeastern U.S. (Figs. E9, E11). This pattern strongly
influenced the temperature and rainfall patterns across North America, with
anomalously cold and dry conditions observed downstream of the mean ridge axes
(across southern Alaska and the eastern U.S.), and well above-average
temperatures observed across the western U.S. (Figs. E1, E3).
Precipitation totals across the
eastern U.S. were generally in the lowest 10th percentile of
occurrences, with many areas recording the lowest monthly totals for November in
the record dating back to 1979 (Fig. E5). Similar deficits were observed in the central
U.S., with the Great Plains region recording well below-average totals for the
seventh straight month. As a result, large
portions of the central U.S. continued to be impacted by extreme or exceptional
drought. At the end of November, the “U.S. Drought Monitor” indicated
exceptional drought from Texas northward to central South Dakota, including
portions of eastern Wyoming and eastern Colorado. Extreme drought persisted in portions
of Arkansas, Iowa, and southern Minnesota.
b. Europe/ Asia
The mean 500-hPa circulation during
November featured an anomalous wave pattern with above-average heights over
southwestern Russia and below-average heights over the eastern North Atlantic
and central Asia (Fig. E9). This pattern contributed to above-average
temperatures across Europe, and to below-average
temperatures over central Siberia (Fig. E1). It also contributed to below-average
precipitation over southeastern Europe and southwestern Russia (Fig. E3).
A strong negative
phase of the West Pacific teleconnection pattern (Fig. E7, Table E1)
was also present during November, as indicated by a large area of above-average
heights at 500-hPa over the high latitudes of the central North Pacific and
eastern Siberia, and below-average heights extending from central Asia eastward
to the date line. This pattern was associated with enhanced westerly jet stream
winds across southern China and the low latitudes of the western North Pacific
(Figs. T21, E10), and with a southward shift of the entrance region
for the East Asian jet. This shift included an anomalous
southerly flow of moist air at 850-hPa into eastern China (Fig. T20), and anomalous ascending motion across that region (Fig. T24). These conditions were
associated with well above-average precipitation in eastern China, where
monthly totals exceeded the 90th percentile of occurrences (Figs. E3, E4).
2. Southern Hemisphere
The mean 500-hPa circulation during
November featured above-average heights over Antarctica and below-average
heights centered over the three ocean basins (Fig. E15). Much of Australia again
recorded above-average temperatures during November, while exceptionally dry
conditions were present in the northeast (Fig.
E3).
The South African rainy season
lasts from October to April. During November 2012, rainfall for the region as a
whole was below average, with much of southeastern Africa recording totals in
the lowest 30th percentile of occurrences (Figs.
E3, E4). Previously,
the region recorded above-average precipitation during both September and
October.
The Antarctic
ozone hole typically develops during August, reaches peak aerial extent in September
and early October, and dissipates rapidly during November. The 2012 ozone hole had
dissipated by early November, after being smaller than average during
August-October (Fig. S8)
Overall, the size
of the 2012 ozone hole was comparable to the smallest seen during the 2002-2011
period. This reduced size coincided with a below-average
aerial coverage of polar stratospheric clouds throughout July- October, along
with a below-average size of the SH polar vortex during October and November (Fig. S8).