General Circulation Features
Northern Hemisphere
During April, the mean 500hPa geopotential height field exhibited a 4-wave
pattern in mid-high latitudes. In the anomaly field, negative anomalies
dominated the region from eastern Europe to the Northwest Pacific, with center
values below –8 dam. Positive anomalies above 4 dam were observed in Polar
region, North Europe and northwestern North America, with center values above 16
dam. In this month, both the Northern Hemisphere subtropical high and the Northwest
Pacific subtropical high were stronger than normal.
Southern Hemisphere
In the mean 500-hPa geopotential height field during April,zonal circulation dominated the mid-high latitudes. In the height anomaly
field, below-normal heights were observed over the southeastern Pacific, the
southeastern Atlantic and the east-central India Ocean. Above-normal heights
were observed over most of Antarctica and the region around.
During April, the
mean surface air temperatures were above average in much of China. The positive
anomalies above 2℃ were observed in much of Northwest China and North China,
Central China and western Tibet, with the maximum values above 4℃. In this
month, rainfall totals were above 50% more than normal in Yunan, southern
Tibet, southwestern Xinjiang, western Hainan and parts of North China. Rainfall
totals in the other regions of China were near or below normal. The monthly
precipitation totals were 50~90% less than normal in central and eastern
Northwest China, the western regions between the Yellow River and the Huaihe
River and middle of Northeast China.
Sea
Surface Temperatures (SSTs)
During April, the
negative SST anomalies below -0.5℃ were observed
over the equatorial Pacific east to 120°W. The negative anomalies near South America
weakened. The positive anomalies above 0.5℃ maintained in the western
equatorial Pacific. Sea surface temperatures were near normal in the central
equatorial Pacific. Correspondingly, the SST indices of NINO 4, NINO 3 and NINO
1+2 regions were 0.3℃, 0℃ and -0.3℃, respectively.
In addition, positive anomalies above 0.5℃ dominated much of the
equatorial India Ocean.
In April, the
zonal wind anomalies at the lower troposphere (850hPa) over the equatorial
Pacific changed little compared with that in March. The weak easterly anomalies
covered the region around the dateline. Westerly anomalies about 2m/s remained
in the rest regions of the equatorial Pacific. Easterly anomalies about 2~4m/s controlled
the equatorial India Ocean. At the upper troposphere (200hPa), weak westerly anomalies
were observed in the central and eastern equatorial Pacific and the equatorial
India Ocean. Weak easterly anomalies were observed over the western equatorial
Pacific.
Southern Oscillation
Convection over the Tropics
During April, the anomalous outgoing longwave radiation (OLR)
distribution exhibited that convections enhanced over the region around the
dateline and were suppressed obviously over Indonesia. In the lower troposphere
(850hPa) divergent wind field, the convergent center was over equator 155°E, and the divergent center
was around 85°W, 20°S. Correspondingly, the
divergent and the convergent centers at the upper troposphere (200hPa) were
over equator 155°E and around 90°W, 25°S, respectively.