154
J. Xia, G.H. Huang, Z. Chen, and X. Rong
the related modeling results under projected scenarios for
regional development (Simonovic, 1996). The DSS helps
users to assess geological conditions and natural hazards,
and provides extensive technical bases and supports for
decisions related to sustainable management of flood-
threatened or affected areas. The study contributes to new
methodologies for flood management, with an emphasis
on: (1) uncovering the complexities of and reasons for a
variety of contradictions and conflicts existing in the flood-
endangered regions, including factitious and natural fac-
tors; (2) systematically integrating the proposed approaches
within a general framework in order to provide a compre-
hensive decision-support tool for directly conducting sce-
nario analyses; this should lead to desired alternatives for
resolving various contradictions and conflicts in flood-en-
dangered regions; and (3) providing re-education and train-
ing for decision makers and the public on the importance
of the sustainability in the flood-endangered regions.
A number of models, tools, and approaches are con-
sidered under a general framework, which can be used to:
(1) develop a supporting system for long-term regional
socio-economic development and flood-prevention plan-
ning; (2) provide effective management on population
mobilization and disaster reduction during the flooding pe-
riod; and (3) conduct optimal planning on the rehabilitation
of flooded areas. The DSS will be applied to the flood-
endangered regions in the Yangtze River Basin.
Figure 1. The Yangtze River basin in China.
from June to September in 1998. This flood has broken
many historical records. It was characterized by extended
periods of heavy rainstorms, high flooding stages, and enor-
mous flood damages, as described in detail below.
The Heavy Rainstorms Covering a Large Area
Within a Long Period
Since entering the monsoon season on June 11, 1998,
heavy rainstorms were frequent in the Yangtze River Ba-
sin. If the daily rainfall in a rainstorm-covered region is
over 50 mm, then this day is named a rainstorm day (RD).
Table 1 shows a total of 74 RDs during a span of 82 days
from June to August 1998. The number of days with daily
rainfall in excess of 100 mm totaled 64, and that in excess of
200 mm was 18 days. Thus, only eight days out of the 82
days from June 11 to August 31 were without rainstorm
events.
The heavy rainfalls during the flooding period covered
a vast area. In regions around the Boyang Lake and the
Dongting Lake, for instance, the total rainstorm area with
daily rainfalls over 50 mm reached 150,000 km on June
23, 1998. On June 13, the area of heavy rainstorm over
2
100 mm was about 51,000 km . Moreover, the intensity of
Major Flooding Disasters
in the Yangtze River Basin
The Yangtze River (also called the Changjiang River)
originates from Mountain Tanggula in the Qinghai-Tibet
Plateau and meanders over a distance of 6,300 km. It is
the largest river in China (Figure 1). The Yangtze River
flows across China’s mainland from the west to the east,
and discharges its water into the Pacific Ocean with a
2
3
yearly flow of 10,000 billion m . The river basin has 3,600
2
tributaries with a total drainage area of 1.8 million km .
the rains during the flooding period was very high. For
example, the precipitation over Wuhan City within 48 hours
on July 20 and 21, 1998, reached 457 mm, with a maxi-
mum intensity of 95 mm/hr. In the Yuanshui Watershed of
the Dongting Lake region, accumulated rainfall in three
days from July 20 to 22 was over 655 mm, with all three
days having daily rainfalls over 100 mm.
The Yangtze River Basin is a densely populated and eco-
nomically prosperous area of China, with many large cit-
ies such as Chongqing, Wuhan, Nanjing, and Shanghai.
However, as a freely flowing river, it may naturally bring
floods. Historically, several great flooding disasters along
the Yangtze caused tremendous damages to human lives
and properties. During the past 2,100 years, from the be-
ginning of the Han Dynasty (202 B.C. to A.D. 220) to the
end of the Qing Dynasty (1644 to 1911), there were a
total of 214 flooding events, with an average frequency of
once every ten years. In the early 20th century, five se-
vere floods occurred in the Yangtze. The great flood in
1931 drowned 145,000 people and inundated 1.8 million
houses. The biggest flood struck in 1954. It claimed 20,000
lives, inundated 3.2 million hectares of cultivated land, and
made more than 18 million people homeless. A major flood-
ing disaster occurred again in the Yangtze River Basin
Table 1. Rainstorm Days Occurred in the Yangtze River
from June 11 to August 31 of 1998
Date During
June
July
August
Total
P > 50 mm
P > 100 mm
P > 200 mm
19 d
17 d
6 d
30 d
26 d
8 d
25 d
24 d
4 d
74 d
64 d
18 d
P - Daily rainfall amount in a rainstorm region in the Yangtze.
IWRA, Water International, Volume 26, Number 2, June 2001