FLOOD MONITORING and FORECASTING IN THE CENTRAL VIET NAM - PowerPoint PPT Presentation

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FLOOD MONITORING and FORECASTING IN THE CENTRAL VIET NAM

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Most plains are with low elevation, easy to be flooded or inundated. 1. Introduction ... Flood and inundation in the Central Viet Nam is ranged as the most severe. ... – PowerPoint PPT presentation

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Title: FLOOD MONITORING and FORECASTING IN THE CENTRAL VIET NAM


1
FLOOD MONITORING and FORECASTING IN THE
CENTRAL VIET NAM
Dr. Nguyen Thi Tan Thanh, National
Hydro-Meteorological Service (NHMS) of the
Ministry of National Resources and Environment
(MONRE) E-mail ktcaokhong_at_hn.vnn.vn
nttanthanh_at_yahoo.com
2
1. Introduction
  • Viet Nam has around 331,000 km2 of natural land.
  • Located in monsoon humid tropics, Viet Nam is
    affected by both oceanic and continental
    climates, especially flood and inundation.
  • There are 2,360 rivers and streams that have
    lengths longer than 10 km, in the central of
    VietNam 740.
  • The coastal plains are not large but densely
    populated (60 of population) with many important
    and rather developed political, socio-economic
    centers. Most plains are with low elevation, easy
    to be flooded or inundated.

3
Introduction
  • Rainfall is unevenly distributed in time and
    space. More than 70 of annual rainfall occurs in
    wet season.
  • Total flow of rivers in Viet Nam reaches 650
    km3/year, equivalent to a flow depth of 960 mm.
  • Ratio of flood and low flow varies from 1.5 to
    30.
  • Severe floods were recorded in 1945, 1969, 1971,
    1978, 1983, 1993, 1990, 1996, 1998, 1999 and
    2003.
  • In period of 1971 - 2001, death toll of 13,300
    people.
  • Flood rising rate, amplitude and peaks are high.
    Flood rising intensity in mountainous rivers may
    reach 2-5m/hour downstream plains 20-50cm/hour.
    Flood amplitude in mountainous areas may reach
    10-20m, higher than 25m in some places.

4
1. Introduction
  • High Flood and inundation last for about 2- 7
    days in the Central Viet Nam, 7-15 days in the
    North Viet Nam, and 3-4 months in the Mekong
    River delta.
  • Depth of inundation is about 2-4m, in some places
    it would reach 5-8m.
  • Combination of typhoon, storm surge, heavy rain
    and high tidal level would cause the flood more
    severe.

5
2. FLOOD IN THE CENTRAL VIET NAM
  • Often associated with heavy rains, typhoons,
    tropical depressions, occur in a large area
    covering some provinces or almost the whole
    region.
  • Rivers are steep, times of concentration are
    short, and downstream areas have low drainage
    capacity.
  • Somehow can be classified as flash floods.
  • Tide and storm surge play a certain role in
    increasing inundation.
  • Flood and inundation in the Central Viet Nam is
    ranged as the most severe. It occurs with high
    frequency causing prolonged inundation in small,
    narrow coastal areas where socio-economic centers
    and densely populated areas are located.

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  • 2.1. Data information collection, processing for
    operational forecast
  • -International Station Network
  • National Telegraphic Station Network consisting
    of
  • 127 synoptic stations.
  • 76 rainfall stations.
  • 182 hydrologic stations
  • 21 ocean-meteorological stations.

8

5 weather radar stations. 3 low
resolution satellite stations 1 high resolution
GMS and NOOA satellite stations.
9
  • 2.2. RAINFALL
  • Large amount of rainfall with high intensity.
  • Maximum daily rainfall 500 - 1000 mm.
  • 24 hours max rainfall reached the highest value
    in Vietnam
  • 1,384 mm at Hue, and
  • 1,009 mm at Son Giang.

10
Rainfall 7 hr 2nd to 7 h 3rd /11/1999
11
rainfall isohyetal map (from 19h 30.X to 7h
6.XI.1999)
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2.3. Flood season on main rivers in the Central
VietNam

13
FLOOD IN 1999
14
FLOOD IN 1999
15
3. INUNDATIONin the Central Vietnam
16
Inundation In historical floods in 1999 in the
Central Vietnam
17
Inundation Map September 1978 flood in Nghe An -
Ha Tinh Plain
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Inundation Map November 1987 flood in Kon River
Plain (Binh Dinh Province)
31
Inundation Map October 1983 flood in Da Rang
River Plain (Phu Yen Province)
32
Inundation Map XI.1978 flood in Cai Nha Trang
River Plain (Khanh Hoa Province)
33
Flood Warning Tower
34
  • 4. Hydrological Forecasting
  • Forecasting is made year-round in form of three
    types short-term, medium-term, and long-term
    forecast.
  • 4.1. Short-range forecast
  • -Rainfall forecasts with lead time of 2-3 days
    are made and used as inputs for hydrological
    forecasts
  • During rainy season from June to December river
    flow and stage of main rivers are made daily with
    lead time of 24 to 48 hrs for rivers in the
    North, 6 to 24 hrs for rivers in central part.

35
4.1. Short-range forecast (cont.)
  • - In case river stage exceeds the alert level II,
    information on flood situation and flood
    forecasting bulletins are disseminated twice a
    day and three times per day if it exceeds the
    alert level III
  • In emergency 8 to 24 forecasts are made within a
    day

36
4.2- Medium and long-range forecasting
  • Medium-range hydro-meteorological forecasting
    bulletin is regularly disseminated 5 times per
    day during rainy season and 10 times per day
    during dry months
  • Long-range HM forecasting bulletin is released
    monthly or every three month in a year
  • - Forecasting parameters are water discharge and
    stage as well as possible drought and water
    shortage in main river systems

37
  • 4.3. Dissemination of forecasting bulletin
  • - Flood - forecasting is provided to the TV and
    Radio broadcasting agencies, some central daily
    newspapers as well as posted on the website of
    www.nchmf.gov.vn
  • RHMC and PHMFC daily provide the forecasting to
    the Provincial Flood and Storm Control Committees
    (PFSCCs), the local TV and radio broadcasting
    agencies with the hydromet forecasting bulletin.
  • Information bulletin on flooding is delivered
    directly to the Leading Communist Party Bodies,
    National Assembly, Government and relief
    providing organizations

38
5. Forecasting techniques
  • - Rainfall-runoff models, method of corresponding
    stage and multivariable regression have been used
    to produce short-term river forecasts.
  • - In recent years, different models like SSARR,
    TANK, NAM have been applied in flood forecasting
    of small and medium size rivers. Hydrological and
    Hydraulic models have also been used in
    forecasting storm for central part and lower
    parts of the big river basins like Hong and
    Mekong

39
5. Forecasting techniques (cont.)
  • - Medium-term and long-term hydromet forecasts
    are made mainly using statistical methods like
    time series analysis, multivariable regression,
    analogue etc. methods.
  • - Forecasting operation has been automated in
    term of data/information collection, processing,
    updating and inputting to models as well as
    preparation of forecasting bulletin.
  • - Forecasting accuracy is 75-85 for short-term,
    and 65-70 medium term and long- term forecasts
    respectively

40
6. Recommendations
  • Establishment of flood and flash flood warning
    and forecasting system on the Thu Bon river
    system (Quang Nam Province) or in Quang Ngai
    Provice (Tra Khuc and Song Ve rivers), where
    flood and flash flood frequently occur
  • Improvement of the hydromet station network
    (automatical stations)
  • Rainfall estimation conventional method,
    Satellite, Rada.

41
6. Recommendations
  • More efficient use of hydrologic and hydraulic
    models (e.g. DEM based distributed models)
  • Research on flood mapping and flash flood
    occurrence areas
  • - Seting up Flood Warning Tower
  • Training
  • Community awareness on flood and flash flood.

42
Map Thu Bon river system (Area10,350km2)
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Thu Bon river system
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Map rivers of Quang Ngai Province (Area Trµ
Khóc 3,240km2, sng VÖ 1,250km2)
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6 h
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48
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