Monthly Highlights
1. Climate in
During September 2012, the surface air temperature
averaged over China was 16.6℃, which was equal to the
normal. Monthly mean surface air temperatures were 1-2℃ above normal in
northern and southwestern Xinjiang, northwestern Tibet, northeastern Inner
Mongolia, northeastern Northeast China. Meanwhile, temperatures were below
normal in eastern Northwest China, southern Northeast China, North China,
Huanghuai, Jianghuai, Jiangnan, Jianghan, eastern Southwest China and South
China, with 1-2℃ below normal in western North China, southern Jianghuai,
western Jiangnan, eastern Jianghan and eastern Southwest China.
In September, average precipitation over
In September, extremes of
Daily Precipitation (DP), Consecutive Precipitation (CP) and Consecutive
Precipitation Days (CPD) were sporadically observed in
DP
extreme events occurred in Baoqing and
2. World Climate
During September 2012, monthly mean temperatures were
1-4℃ above normal in
mid-eastern Europe, mid-northern Asia,most North America and
mid-southern South America, with temperatures 2-4℃ above normal in locations
of southern Middle Europe, mid-northern Russia, northwestern Canada, central
South America. Meanwhile, monthly mean temperatures were 1-2℃ below normal in
the Russian Far East, parts of northern South America, central North Africa and
southern South Africa, with temperatures at least 2℃ below
normal in locations.
For the month, precipitations were at least 50% above
normal in mid-northern
3. General Circulation Features
Northern Hemisphere: During September
2012, the field of mean 500hPa geopotential height exhibited a three-wave
pattern over the mid-high latitudes. In the field of height anomaly, positive
anomalies above 4 dam covered northwestern
Southern Hemisphere: For the month, in the
field of mean 500hPa geopotential height zonal circulation dominated the
mid-high latitudes. In the field of height anomaly, positive anomalies above 4
dam covered locations of Antarctic, the
4. Tropical Features
Sea Surface Temperatures
(SSTs): During September 2012, SSTs were above normal over most of the central and eastern equatorial Pacific with
central anomaly values above 0.5℃. NINO 1+2 index
was 0.5℃, with an increase of 0.3℃, NINO 3, NINO 3.4 and NINO Z indices were 0.4℃, 0.5℃ and 0.4℃, with a drop of 0.3℃, 0.2℃ and 0.2℃, respectively, and NINO 4 index was 0.4℃, the same as in August.
Subsurface
Temperatures: During September 2012, anomalously warm subsurface water maintained in
the eastern and western equatorial Pacific. Anomalously
warm subsurface water in the central equatorial Pacific weakened and shrank,
while anomalously cold subsurface water below -0.5℃ controlled a part of
the central equatorial Pacific.
Warm Pools: During September 2012, the areas of the
Wind Field: During September 2012, at lower troposphere (850hPa), zonal winds were near normal over the eastern equatorial Pacific, while westerly anomalies
dominated the central and western equatorial Pacific. At upper troposphere
(200hPa), zonal winds were near
normal over the central and
western equatorial western Pacific, while westerly anomalies controlled the eastern
equatorial Pacific with central
value above 12m/s.
Southern
Oscillation: For the month, the
Southern Oscillation Index (SOI) was 0.4, with an increase of 0.8 from last
month.
Convections over
the Tropics: During September 2012,
the anomalous outgoing long wave radiation (OLRa) showed that enhanced
convection was observed over the western Pacific west of the international dateline,
while convection was near normal over the central and eastern Pacific. At lower
troposphere (850hPa) divergent wind field, a convergent center was around 125ºE, 17.5ºN, and a
divergent center was near 105ºW, 15ºS. At upper troposphere (200hPa), the corresponding divergent
center was near 135ºE, 10ºN, and the
convergent center was around 100ºW, 25ºS.
5. ENSO
Monitoring and Outlook
During the recent period, positive anomalies weakened in the
east-central and eastern equatorial Pacific. Based on models’ prediction and
trend diagnoses of the oceanic variations, the ENSO-neutral conditions are
expected to persist through the coming autumn and winter.
Therefore, we will closely monitor the development of ENSO conditions and update our ENSO wrap-up in time.