Highlights
General
Circulation Features
Northern
Hemisphere
During
October, the mean 500hPa geopotential height field exhibited a 4-wave pattern at
mid-high latitudes. The polar vortex was stronger than normal. Correspondingly,
negative anomalies below –4 dam covered the regions of Europe, offshore of
Taymyr Peninsula, northeastern North Pacific and eastern North America.
Meanwhile, positive anomalies above 4 dam controlled the regions between the
northern North Atlantic to Greenland and northern Canada, western North America
and western Siberia, with center values above 12 dam over the northern North
Atlantic. In this month, Northern Hemisphere subtropical high was obviously
stronger than normal. The Northwest Pacific subtropical high was also stronger
than normal and extended westward remarkably.
Southern Hemisphere
In the mean 500hPa geopotential height field during October, a 3-wave
pattern dominated the mid-high latitudes.
Positive anomalies dominated the Antarctica and the
south-central Pacific, the southwestern Atlantic, and the south-central India
Ocean. Meanwhile, negative anomalies covered the southeastern Australia and
southwest to South America.
During
October, the mean surface air temperatures were 1℃~2℃higher
than normal in the north-central Northeast China, west-central Southwest China,
most of Tibet and Qinghai, northern Xinjiang. The monthly mean surface air
temperatures were near or above normal in the rest regions. During October,
rainfall totals of 50% more than normal received in the regions such as
south-central Northeast China, North China, most of the regions between the
Yellow River and the Huaihe River, central Shanxi, northeastern Gansu, southern
Ningxia and southwestern Xinjiang. Meanwhile, rainfall totals were 50% below
normal in the regions south to the Yangtze River and most of South China, with
80% below normal in central Northwest China, Hainan, southern Zhejiang, southern
Jiangxi, southern Hunan, southeastern Guangxi and southwestern Guangdong.
Sea Surface
Temperatures(SSTs)
During
October, most of the equatorial Pacific were controlled by the positive SST
anomalies above 0.5℃. Positive SST anomalies above 1.0℃
were observed in part of the eastern equatorial Pacific. Negative SST anomalies
in the offshore of South America were weaker than that in September.
Correspondingly, the SST indices of NINO 4, NINO 3 and NINO 1+2 regions were 0.8℃,
0.4℃
and 0.1℃,
respectively. In addition, positive anomalies around 0.5°C
remained in the equatorial India Ocean.
In this month, at the lower troposphere (850hPa),
weak westerly anomalies about 2m/s covered the central and eastern equatorial
Pacific and the equatorial India Ocean. At the upper troposphere (200hPa), zonal
wind anomalies were near normal.
Southern Oscillation
Convection
over the Tropics
During October, the anomalous outgoing longwave radiation (OLR)
distribution exhibited that slightly enhanced convections were nearby the
dateline over the equatorial Pacific and suppressed convections were over the
equatorial western Pacific. In the lower troposphere (850hPa) divergent wind
field, the convergent center was over 150°E,
7°N,
and the divergent center was around 110°W,
15°S.
Correspondingly, the divergent and the convergent centers at the upper
troposphere (200hPa) were over 150°E,
10°N
and around 95°W,
25°S,
respectively.