19
Aspects CNMC LNMC TNMC VNMC
75% of labour force; about
80% of poverty remains in this
sector;
80% of cultivated areas are
subsistence rain fed rice with
very low yield levels
stakeholders to built water
storage infrastructures system
for expanding irrigated
agriculture aiming at boosting
rice production to reach 3.3
million tones as targeted in
year 2010
CLD It contributes nearly
50% of the total rice and
aquaculture production
Average population density in
the CLD: 423 people/km
2
Flood characteristics
Downstream of Kratie, flood
discharge is regulated through
extended floodplains, and
outflow into three main
channels – Lower Mekong and
Bassac rivers, and Tonle Sap
River and Great Lake
Dominant influence on the
incidence and severity of
flooding in the Cambodian
floodplain and the delta in
Vietnam from left bank
tributaries downstream of
Vientiane (Nam Ngum and
Nam Theun, and the Se Kong,
Se San and Sre Pok Rivers
entering the Mekong
mainstream at Stung Treng)
Reversal flow of the Tonle Sap
forms a key feature for
Cambodia’s floodplain
hydrology
The flow patterns is also
determined by downstream
hydraulic conditions, tidal
influences and backwater
effects particularly upstream
Last 37 years ( 1966-2002 ) 27
floods
Among of 27 historic floods, 6
were large floods: 1966, 1971,
1978, 1995, 1996 and 2002,
Agriculture in the Mekong
river flood plain is particularly
prone to flood damage not
only due to over bank flows
inundation from the
mainstream, but also from the
back water effects in the
tributaries when the
mainstream is full;
1995 flood (Storm Lois)
caused tributary backwater
effects and inundation of
103,000 ha of the Vientiane
Plain; with the depth of
between 0.5 to 0.8 m for
period up to 2 months.
Year 2002 of Vongfong-14
storm from Southeast
Monsoon affected in 12
provinces; 43 Districts; 1,000
villages; 30,000 families;
Flood is considered as one of
the most dangerous disaster
for human life and socio-
economic development
The Mekong flow is naturally
regulated by the Great Lake in
Cambodia before entering to
the CLD; floods are governed
by flat topography, the regime
of the flow from up stream,
the regulation of Great Lake,
regimes of East and West tide,
local rainfall and hydraulic
infrastructure (control) system
Low flow season from
December to June with
average discharge of about
3000 m3/sec; the flood season
from July to November with
average discharge of about
25,400 m3/sec.
Annually, an area of 1.2 - 1.9
million hectares of the CLD
are inundated for from 2 - 5
months and water depth from
0.5 m to 4.0 m and more;