Extratropical Highlights
– January 2015
1. Northern Hemisphere
The mean 500-hPa circulation during
January featured an extensive anomalous wave pattern extending from eastern
Asia to Europe. Regional aspects of this pattern included above-average heights
across the high latitudes of the North Pacific, Alaska, western North America,
the central North Atlantic, and eastern Asia (Fig. E9). The pattern also featured
below-average heights over the central subtropical north Pacific, and across
the high latitudes of the North Atlantic from eastern Canada to Scandinavia. This
pattern projected onto the positive phases of the North Atlantic Oscillation
(NAO, (+1.57) and the East-Atlantic teleconnection pattern (+1.11) (Table E1, Fig. E7).
The main land-surface temperature signals
during January included above-average temperatures across eastern Alaska, western
Canada, the western U.S., western Russia and east-central Asia (Fig. E1). The
main precipitation signals included above-average totals in eastern
Europe and western Russia, and below-average totals in the western and
southeastern portions of the U.S. (Fig. E3).
a. North Pacific/ North America
The mean 500-hPa circulation during
January featured a north-south dipole pattern of height anomalies over the
North Pacific, and an anomalous ridge-trough pattern across North America (Fig. E9).
Over North America, this anomaly pattern reflected an amplified ridge in the
west and an amplified trough in the east. This pattern was associated with above
average surface temperatures across western North America, with the largest
departures (exceeding +4oC) observed in western Canada and eastern
Alaska (Fig. E1).
It was also associated with exceptionally warm and dry (Fig. E3) conditions in the western U.S.,
with many areas recording temperature departures in the upper 70th
percentile of occurrences and precipitation totals in the lowest 10th
percentile of occurrences.
Consistent with these conditions, the
U.S. Drought Monitor indicated a continuation of exceptional drought in central/
southern California and western Nevada, with extreme drought extending
northward into Oregon. Exceptional or extreme drought also continued in north-central
Texas and western Oklahoma.
b. North Atlantic/ Europe
The 500-hPa circulation featured a
north-south dipole pattern of height anomalies across the North Atlantic, with
above-average heights in the middle latitudes and below-average heights
extending from eastern Canada to Scandinavia. This pattern projected onto the
positive phase of the NAO (+1.57) and the east Atlantic teleconnection pattern
(+1.11) (Table E1,
Fig. E7). It was associated with amplified
Icelandic Low, an enhanced ridge over the east-central North Atlantic, and a
split flow pattern centered over western Europe (Fig. E10). It
was also associated with an enhanced transport of milder, marine air into
Europe, which contributed to anomalously warm (Fig. E1) and wet (Fig. E3) conditions in eastern
Europe and western Russia.
c.
East-central Asia
Exceptionally
warm surface temperatures were observed across east-central Asia during
January, with many locations recording departures in the upper 90th
percentile of occurrences (Fig. E1). This warmth was related to a weakening of the
climatological mean trough over northeastern Asia, which typically brings cold
air into northern China and Mongolia (Figs.
E9, T23).
2. Southern Hemisphere
The mean 500-hPa circulation during
January featured above-average heights over the high latitudes of the South
Pacific, and below-average heights over the central South Atlantic Ocean (Fig. E15). The
South African rainy season lasts from October to April. Rainfall during January
for was below average the region as a whole (Fig. E4), with the main deficits recorded
in the south and the main surpluses recorded in northern Mozambique and
Madagascar (Fig. E3).
To date, the South African rainy season was below average during October, November,
and January, and above average in December (Fig. E4).