

Administration. In that way, the end user and policy-
maker can make effective use of climate information.
Perspective
The warming climate is accompanied by changes in the
mean and extreme climates, and both have large impacts
on the society and economy of China.
2
Statistically,
annual meteorological disasters account for 3-6 per cent
of China’s gross domestic product during the 1990s,
with a larger percentage in the years featuring signifi-
cant climate anomalies. In recent years, those disasters
tend to intensify and lead to more severe losses to the
national economy, human life and property, resulting in
a variety of key social and environmental problems. In
particular, to a great extent, meteorological disasters are
directly caused by extreme climates. For example, the
freezing rain in southern China in January 2008 caused
economic losses of about CNY151 billion and the death
of 129 people, and the torrential rain and landslide in
Zhouqu County of Northwest China in 2010 resulted
in the death of 1,501 people. Climate change studies
and their services are at a preliminary stage. In future
works, there is an urgent need to further examine the
nature and cause of climate change over a wide range
of time and spatial scales in China. Understanding the
observed changes in various kinds of mean and extreme
climates, improving the ability of climate models in
reproducing observed changes, and improving the tech-
niques of projecting future changes in both dynamical
and statistical approaches are equally important tasks.
Finally, climate products such as seasonal and decadal
predictions and long-term climate change projections
can better serve Chinese society.
around CNY145 billion. In this situation, it is important to perform
seasonal climate prediction to meet the needs of defence against
meteorological disasters. Accordingly, seasonal climate prediction
is always emphasized in the field of climate change. In that area,
both statistical and dynamical approaches have been applied in
seasonal precipitation prediction by the Chinese Meteorological
Administration. A statistical approach, such as the year-to-year
increment approach, is based on a comprehensive study of the rela-
tionship between regional precipitation and the preceding climate
conditions such as snow cover on the Eurasian continent, the El
Niño–Southern Oscillation, soil moisture, Arctic Oscillation and
Antarctic Oscillation, after which a regression equation for predic-
tion is established. The dynamical approach is based on numerical
experiments of climate models. For the two-tiered method, global
sea surface temperatures are first predicted by an oceanic or atmos-
phere-ocean general circulation model, and then used to force an
atmospheric general circulation model to forecast atmospheric
elements. For the one-tier method, the seasonal prediction system
is generally composed of an atmosphere-ocean general circula-
tion model and a data assimilation system. Since China and East
Asia are areas with low prediction skill on seasonal precipitation,
statistical downscaling and dynamical downscaling have also been
used to perform seasonal prediction. In addition, error correction
schemes have also been applied in practice.
The aforementioned effort has improved China’s regional
climate prediction skills on the seasonal scale. The related climate
prediction product has also served society. For example, seasonal
precipitation prediction has been carried out by several research
centres and universities, and their results are collected by the
National Climate Center. All experts in that field are organized
together to discuss the forthcoming climate change at regional
and national scales. The final prediction products for key climatic
variables will be publicly issued by the Chinese Meteorological
[
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C
apacity
D
evelopment
Others
8%
Agriculture,
forestry,
biology
6%
Ocean
7%
Meteorology
71%
Earthquake
8%
(a)
(a) Mean percentage of economy losses caused by different disasters, and (b) mean percentage of economy losses caused by
different meteorology disasters in China in recent decades
Source: Huang, 1999
3
27%
Typhoon,
hail
11%
Others
7%
Droughts
55%
Floods
27%
(b)