Seasonal Highlights
1. Climate in China
During the winter (Dec. 2010-Feb. 2011), seasonal mean surface
air temperature of China
was 0.3℃ below
normal (-4.3℃), being the
coldest winter since 1987. Temperatures were observed near or below normal in
most of China, except Qinghai, central-western Southwest China, parts of
Central China, parts of western North China, northern Heilongjiang, and parts
of western Xinjiang, where temperatures were more than 0.5℃
above normal, with 1-2℃ above
normal in parts of above regions. Temperatures were 1-2℃
below normal in central-northern Xinjiang, western and eastern Inner Mongolia,
western Northeast China, and southwestern South China, with over 2℃
below normal in parts of northern North Xinjiang and parts of western Northeast China.
For the season, averaged precipitation over China was near normal, while
precipitation distribution was extremely uneven. Precipitations were observed
30%-100% more than normal in most of Inner Mongolia, most of Northeast China,
northern and western Xinjiang, locations of western Qinghai, southwestern
Tibet, locations of eastern Sichuan, and central-southern Yunnan, with over
100% more than normal in locations. Meanwhile, precipitations were observed 30-80%
less than normal in western Liaoning, locations
of western Inner Mongolia, central-southern Xinjiang, central-eastern Tibet, central Sichuan,
Jiang-Huai areas, Jiang-Han areas, and southern South China, with over 80% less
than normal in central-southern Xinjiang and central Tibet.
2. World Climate
During the boreal winter(Dec.
2010-.Feb. 2011), seasonal mean surface air temperatures were observed more
than 0.5℃ below
normal in most of Europe, central-western Russia, northern Central Asia, most
of East Asia, Afghanistan, most of Pakistan, most of Australia, central and
northwestern North America, with values over 4℃ below normal in northern Europe and central-southern
Russia. Meanwhile, temperatures were observed significantly higher than normal in eastern North America, most of the Far
East of Russia, most of West Asia, the Qinghai-Tibet Plateau, the western Indo-China
Peninsula, most of North Africa, locations of northern and central-eastern
South America, with at least 4℃
above normal in parts of above regions.
For the winter,
precipitations were observed 30%-100% more than normal in parts of the East
Europe Plain, northern coast and parts of the Far East of Russia, northern East
Asia, southeastern India, the western Indo-China Peninsula, southeastern West
Africa, most of Australia, parts of central and northern North America,
northern and central-eastern South America, with over 200% above normal in parts
of above regions. Meanwhile, precipitations were observed 30-80% less than
normal in northern Europe, central Russia, most of Central Asia, most of West
Asia, the Qinghai-Tibet Plateau, most of West Africa, southern North America,
and locations of northwestern South America, with precipitations over 80% less
than normal in parts of above regions.
3. General Circulation
Features
Northern Hemisphere: During the boreal winter(Dec.
2010-.Feb. 2011), in the field of 500hPa geopotential height
anomaly, positive anomalies above 4 dam covered regions from northeastern
North America to northwestern Russia through the Arctic Ocean, and northern
North Pacific, with central values above 16 dam over northern North Pacific. Negative
anomalies of -4~-8 dam covered regions from eastern United
States to the northern North
Atlantic Ocean, and the middle latitudes of the Northwest Pacific.
Southern Hemisphere: During the boreal winter, in the
field of 500hPa geopotential height anomaly, positive anomalies above 4 dam covered
the South Indian Ocean and the South Atlantic Ocean between 40oS-60oS,
and the middle latitudes of the South Pacific, with central values above 8 dam over
the South Indian Ocean and the South Atlantic Ocean.
Meanwhile, negative anomalies below -4 dam covered the southeastern South Pacific
in the high latitudes.