Extratropical Highlights –October 2016
1. Northern Hemisphere
The 500-hPa circulation during October
featured above-average heights over much of the high latitudes and across eastern
North America, and below-average heights over central and eastern Asia, and
over the Gulf of Alaska (Fig. E9). In the subtropics, the 200-hPa circulation
featured a pronounced westward retraction of the mean subtropical ridge over
Australasia, along with amplified mid-Pacific troughs in both hemispheres (Fig. T22).
This pattern is consistent with the La Niña-related pattern of enhanced
convection over Indonesia and suppressed convection across the central
equatorial Pacific (Fig. T25).
The main land-surface temperature signals
during October included above-average temperatures in eastern North America,
the southern half of the United States, and China, and below-average
temperatures in western Canada and large portions of south-central and
southeastern Russia (Fig. E1). The main precipitation signals included above-average
totals in the northwestern U.S., western Canada, eastern
Europe, and eastern China, and below-average totals in the central and
southeastern U.S., Scandinavia, and northern Russia (Fig. E3).
a. North America
The 500-hPa circulation during October
featured above-average heights across the eastern half of North America and a strong
trough over the eastern Gulf of Alaska (Fig.
E9). This pattern was associated with well above-average
surface temperature across much of the U.S. and the eastern Canada,
with much of the central and southern U.S. recording departures exceeding the
90th percentile of occurrences (Fig. E1). It was
also associated with above-average precipitation in the northwestern U.S. and
western Canada (downstream of the trough axis), and with below-average
precipitation across the central and southeastern U.S. (Fig. E3). Precipitation totals in the
U.S. Gulf Coast states were generally in the lowest 10th percentile
of occurrences, which acted to intensify and expand drought conditions from
central Mississippi to western South Carolina.
According to the U.S. Drought
Monitor, exceptional or extreme drought continued during October across central
and southern California, and expanded to cover the area from central
Mississippi to southeastern Tennessee and western South Carolina. Severe or
extreme drought persisted in New York, northern New Jersey and much of New
England. Conversely, long-term drought conditions lessened considerably in the
northwestern U.S.
b. China
The 500-hPa circulation during October
featured above-average heights over northeastern China and a broad, amplified
trough over central Asia (Fig. E9). This overall pattern was associated with an
anomalous low-level southerly flow of moist subtropical air into central and
eastern China (Fig. T20). These conditions were associated
with well above-average surface temperatures across much of China, with many
locations recording departures in the upper 90th percentile of
occurrences (Fig. E3).
They were also associated with above-average precipitation in eastern China,
with portions of the northeast recording totals in the upper 90th
percentile of occurrences (Fig. E3).
2. Southern Hemisphere
The mean 500-hPa circulation during
October featured an anomalous zonal wave-3 pattern in the middle latitudes, which
included an amplified trough south of Australia (Fig. E15). This trough contributed to a continuation of below-average
surface temperatures in portions of the southwest (Fig. E1).
The Antarctic ozone hole typically
develops during August and reaches peak size in late September (Fig. S8). It
then typically decreases in size during October and November, and dissipates in
early December. During October 2016, the size of the ozone hole was below the
average of the 2006-2015 period, with a rapid drop in
size seen in mid-October.