Extratropical Highlights
– December 2012
1. Northern Hemisphere
The 500-hPa circulation during December
featured above-average heights near the Aleutian Islands, across eastern Canada,
Greenland and Scandinavia. Below-average heights were present over western
North America, across the east-central North Atlantic and Europe, and over the
middle latitudes of central and eastern Asia (Fig. E9). This overall pattern projected
onto a strong positive phase of the Scandinavia teleconnection pattern (Fig. E7, Table E1). It also projected onto continuing negative
phases (three months) of the West Pacific and Pacific/ North America teleconnection
patterns, and onto the negative phase of the Tropical/ Northern Hemisphere
pattern.
The main land-surface temperature signals
during December included above-average temperatures across central and eastern
North America, and below-average temperatures in Alaska and much of Eurasia (Fig. E1). The
main precipitation signals included above-average totals in the northwestern and
eastern U.S., northwestern and southeastern Europe, and eastern China, and below-average
totals in the south-central U.S. (Fig. E3).
a. North America
The mean 500-hPa circulation during
December featured above-average heights south of the Aleutian Islands and over
eastern Canada, and below-average heights over western Canada (Figs. E9, E11). This pattern projected onto a continuing
negative phase (three months) of the Pacific/ North America teleconnection pattern,
and also onto the negative phase of the Tropical/ Northern Hemisphere pattern (Fig. E7, Table E1). These conditions reflected a nearly complete
disappearance of the mean ridge normally located over western North America.
They were also associated with a westward shift of the mean Hudson Bay trough
axis to central North America. The resulting upper-level wind pattern reflected
anomalous northwesterly flow into Alaska and anomalous southwesterly flow into
the western U.S (Fig. E10).
These conditions were associated
with above-average surface temperatures across the eastern half of North
America, with most regions recording departures in the upper 70th
percentile of occurrences (Fig. E1). In contrast, southwestern and eastern Alaska
and northwestern Canada recorded below-average temperatures, with many areas
recording departures in the lowest 30th percentile of occurrences.
Areas downstream of the mean trough
axes recorded well above-average precipitation during December, including the
U.S. Pacific Northwest and eastern U.S. (Fig.
E3). Area-averaged totals in the Pacific
Northwest reached the 90th percentile of occurrences, and were above
average for a third straight month (Fig.
E5).
In contrast, the south-central U.S.
again recorded below-average monthly precipitation (Fig. E3), with large areas of Kansas,
Oklahoma, and Texas recording totals less than 25% of normal (Fig. E6).
This marks the eighth straight month of below-average precipitation in the
Great Plains region (Fig. E5). As a result, much of the region continued to be
impacted by extreme or exceptional drought. At the end of December, the “U.S. Drought
Monitor” indicated exceptional drought from northern Texas northward to central
South Dakota, including portions of eastern Wyoming and southeastern Colorado.
Extreme drought persisted in northwestern Arkansas, northwestern Iowa, and southwestern
Minnesota.
b. North Atlantic/ Europe
The mean 500-hPa circulation during
December featured a north-south dipole pattern of height anomalies, with above-average
heights across eastern Canada, Greenland, and Scandinavia, and below-average
heights over the east-central North Atlantic and Europe (Figs. E9). This pattern was associated
with a complete disappearance of the Icelandic Low for a second straight month,
and with a strong positive phase (+2.0) of the Scandinavia teleconnection
pattern (Fig. E7,
Table E1). It was also associated in northern
Europe with enhanced jet stream winds, increased storminess (Fig. E13) and above-average
precipitation (Fig. E3).
c. Asia
The 500-hPa height pattern during
December featured an extensive area of negative height anomalies across central
and eastern Asia (Fig. E9). Similar conditions were also present in
November. In combination with the strong blocking ridge over Scandinavia, this
pattern during December contributed to well below-average temperatures across
central Asia, with many areas recording departures in the lowest 10th
percentile of occurrences (Fig. E1). Also, eastern China recorded well above-average
precipitation for a second straight month (Fig.
E3),
with area-averaged totals again reaching the 99th percentile of
occurrences (Fig. E5).
2. Southern Hemisphere
The mean 500-hPa circulation during
December featured above-average heights over the southeastern South Pacific
Ocean and in the areas south of both Australia and South Africa, and generally
below-average heights in the middle latitudes (Fig. E15)
Much of eastern Australia recorded anomalously
warm (Fig. E1)
and dry (Fig. E3)
conditions in December, with portions of the northeast recording temperature
departures in the upper 90th percentile of occurrences (Fig. E1).
The South African rainy season
lasts from October to April. During December 2012, rainfall for the region as a
whole was near average, with above-average totals in interior portions of
southern Africa and below-average totals in extreme southern South Africa and
Madagascar (Fig. E3).
To date, the 2012-13 rainy season has been variable,
with above-average totals in October, below-average totals in November, and
near-average totals in December (Fig. E4).