Climate Change Adaptation in Water Sectorteacher.buet.ac.bd/diriwfm/climate/shortcourse/Awlad for...
Transcript of Climate Change Adaptation in Water Sectorteacher.buet.ac.bd/diriwfm/climate/shortcourse/Awlad for...
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Climate Change Adaptation in Water Sector
(Application of Modelling in Water Sector)
Mollah Md. Awlad HossainWater Resource Engineer
Head, GIS Division, CEGIS
11 February 2007
Dhaka
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Climate Change
Why it happens? Is it a new problem?How it affects Water System?What to consider in Modelling of WRS?
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Why it happens?Climate change may result from both natural and human causes.
– CO2 and Other Greenhouse Gas Variations – Ocean Circulation– Volcanic Eruptions– Solar Variations– Orbital Variations– Land Use Changes– Human Activity and Greenhouse Gas
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Climate Change Cycle
Based on ice cores drilled in Vostok, Antarctica. It shows temperature changes near the South Pole
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Recent Event•Since the 1900s global average temperature and atmospheric CO2 concentration have increased dramatically, particularly compared to their levels in the 900 preceeding years.
•The rapid rise in both surface temperature and CO2 is one of the indications that humans are responsible for some of this unusual warmth.
•This graph is based on data from tree rings, coral and ice cores, and historical records. It represents only the Northern Hemisphere.
• the modern temperatures are generally greater than during the past several hundred years.
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Effects of Climate ChangePrimary Effects: Global Warming which causes
-changes in Temperature and Precipitation
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Secondary Impact – Sea Level Rise, Coastal Inundation and Salinity Intrusion
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Relative vulnerability of coastal deltas as shown by the indicative population potentially displaced by current sea-level trends to 2050
Extreme = >1 million
High = 1 million to 50,000
Medium = 50,000 to 5,000 Source: IPCC 4th Assessment Report, 2007
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Year Temperature change (0C) Mean
Precipitation change (%) Mean
Monsoon Season
Dry Season
Monsoon Season
Dry Season
2020 0.8 1.1 +6.0 -2.02050 1.1 1.6 +8.0 -5.02100 1.9 2.7 +12.0 -10.0
National Adaptation Plan for Action (NAPA)
Bangladesh:Change in Temperature and Rainfall
Primary Impacts
Hot season will be more hot
Wet season will be more wet (2 floods in 2007)
Dry season will be more dry
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Secondary Impacts
• Flooding• Drainage congestion
• Droughts• Sea Level Rise
Changes in all above are happening in Bangladesh
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How it affects Water System?Increase in number and extent of floods and erosionLonger period of floods due to increased precipitation in monsoon and rising sea levelIncrease in period of drought due to reduced rainfall in winterIncrease in number and intensity of cyclones, tropical stormsSea Level Rise
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What is Modelling of Water System?
Representation of the behavior of water system under certain conditions
-Physically-Mathematically
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Climate Change Effect on FLOOD
Onset
Peak
DurationRecession
Recurrence
High peak, long duration flood is coming more frequently- huge impacts on lives, livelihoods, development, economy
1:30 yr 1:10yr
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Flood Complication due to CCHigh peak
Longer duratio
Early/delayed onset
Slow recession
More frequent
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More Complication
Flood + Drainage + Rainfall + Drought + Temp + Cyclone + SLR + Erosion +
+ CROP Calendar
Development Interventions
Policy/Politics…
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Secondary Impact – Floods
The onset and withdrawal of the peak flows are shifting. Flow records over past 50 years for the station Bahadurabad (Brahmaputra/Jamuna rivers) shows: peak discharge is increasing and is peaking earlier.
The estimated change in inundation categories under mean value of IPCC SRES scenarios in the year 2050s:
SRES scenario Flood free area Moderate flooded area
A2 57% decrease about 51% increase
B1 63% decrease about 82% increase
Bangladesh
Source: ORCHID, 2007
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Flooded Area in Bangladesh: Present & Future Scenario
Secondary Impact: Floods
Bangladesh
Spatial Distribution of Flood extent and depth for mean IPCC SRES A2 and B1 Scenarios for the year 2020s and 2050s excluding the coastal area of Bangladesh.
(a) SRES A2 (2020)(b) SRES A2 (2050)(c) SRES B1(2020)(d) SRES B1 (2050)
16Source: ORCHID, 2007
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Secondary Impact – Sea Level Rise, Coastal Inundationand Salinity Intrusion
Bangladesh
Effects of Sea level rise
Increase in inundated areas of up to 3% (2030s) and 6% (2050s): Primarily in coastal low lying areas (ORCHID, 2007)
Salinity intrusions along much of the coastline: Rates of intrusion vary with local conditions and are strongly influenced by dry season river flows and the rate of SLR.
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Secondary Impact – Sea Level Rise, Coastal Inundationand Salinity Intrusion
BangladeshInundation Due to Sea level Rise in coastal areas of Bangladesh
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Monsoon Season Dry SeasonScenarios
Inundated area, [ha]
Increase in inundation area
Inundated area, [ha]
Increase in inundation area
Base 1,720,200 [50%]
404,500 (12%) -
B1, Yr 2080 (SLR 15cm)
1,863,600 [54%]
4% Insignificant change -
A2, Yr 2050 (SLR 27cm)
1,972,200 [57%]
7% 559,100 (16%) 4%
A2, Yr 2080 (SLR 62cm)
2,189,200 [63%]
13% 768,600 (22%) 10%
A2, Yr 2080 (SLR 62cm+10% rainfall)
2,271,700 [66%]
16% Not Applicable
Source: CEGIS & IWM, 2006
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Secondary Impact – Cyclone and Storm Surge
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Bangladesh Bangladesh is hit by about 0.93% of the world’s total tropical stormsAbout 53% of the total world deaths due to tropical cyclones occurred in Bangladesh (Ali, 1999)
The cyclone High Risk Areas (HRAs) of 8900 sq km will increase by
35% in the 2020s40% in the 2050s
Population in cyclone HRAsCurrent - about 8.3 millionin the 2020s - 14.6 million in the 2050s 20.3 million
Source: ORCHID, 2007
Changes in cyclone High Risk Areas for current conditions, the 2020s and the 2050s. Only worst case examples included – highest warming
Source: NAPA, 2005
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An Example
• SEMP-UNDP conducted a study named “Impacts of Sea Level Rise on Land use Suitability and Adaptation Options” to develop land use zoning strategies to cope with different sea level rise scenarios for sustainable and equitable development in the SW region of Bangladesh
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Study Area
Total Study Area = 10,150 km2
Bagerhat = 3,426 km2
Khulna = 3,412 km2
Satkhira = 3,317 km2
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1. Gorai- Pasur- Rupsha System
2. Modhumoti- Baleshor System
3. Betna- Kobadakha-
Arpangashia-Kholpatura
System
4. Sibsha System
5. Ichamoti-Raimongal System
6. Kobadakha Subsystm
7. Rupsha-Sibsha Link
8. Shala-Gang System
9. Bhairab Sub-System
10. Chitra Subsystem
River System
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Polders• Polders
– 35 Nos– 4,760 km2 (47%)
• Length of embankment: 2,060 km
• Hundreds of Sluices
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Area inside/outside polders3,427 3,412 3,318
1,6301,305.30
1,823
0
500
1,000
1,500
2,000
2,500
3,000
3,500
4,000
Bagerhat Khulna Satkhira
Are
a (k
m2)
District area Protected area
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Base condition
• Flood season– Average year flow at Gorai: Yr 2000
• Dry season– Dry season flow at Gorai: Yr 1997
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Scenario for Hydrodynamic computation
• According to NAPA the Sea Level Rise is– 32cm in 2050– 88cm in 2100
Model run was planned for:- Base condition Yr 2000 flow situation
Yr 1997 flow situation- Scenarios: Yr 2000 + 32 cm SLR
Yr 2000 + 88 cm SLRYr 1997 + 32 cm SLRYr 1997 + 88 cm SLR
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Model River Network
D/S
U/S
-1.0
-0.5
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
4.0
24-Aug-00 26-Aug-00 28-Aug-00 30-Aug-00 01-Sep-00 03-Sep-00 05-Sep-00 07-Sep-00 09-Sep-00Time
Wat
er L
evel
(m,P
WD
)
SLR 0 cmSLR 14 cmSLR 32 cmSLR 88 cm
Source: IWM
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Flooding in Base Condition (Y2000)17
%
29%
30%
21%
3% 0%
32%
17%
18%
16%
16%
1%
32%
16%
30%
16%
6%
0%0%
5%
10%
15%
20%
25%
30%
35%
Dry 0 - 30 cm 30 – 90 90 – 180 180 – 300 >300
Bagerhat Khulna Satkhira
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Flooding in (Y2000 + 32 cm SLR)6%
9%
28%
36%
21%
0%
22%
15% 18
%
19% 23
%
4%
25%
13%
30%
21%
10%
0%0%
5%
10%
15%
20%
25%
30%
35%
40%
Dry 0 - 30 cm 30 – 90 90 – 180 180 – 300 >300
Bagerhat Khulna Satkhira
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Flooding in (Y2000 + 88 cm SLR)1% 3%
19%
34% 43
%
0%5% 7%
15% 23
%
34%
15%
16%
8%
27% 31
%
16%
2%
0%
5%
10%
15%
20%
25%
30%
35%
40%
45%
Dry 0 - 30 cm 30 – 90 90 – 180 180 – 300 >300
Bagerhat Khulna Satkhira
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Flood depth in Yr 2000
Flooding Total %Dry 2,757 27%0 - 30 cm 2,119 21%30 - 90 2,648 26%90 – 180 1,755 17%180 – 300 837 8%>300 39 0.4%
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Flood depth in Yr 2050
4 polder inundated
InundationArea
(km2)%
Dry 1,775 17%0 - 30 cm 1,252 12%30 – 90 2,604 26%90 – 180 2,593 26%180 – 300 1,804 18%>300 128 1.3%
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Flood depth in Yr 2100
13 polder inundated
InundationArea
(km2)%
Dry 756 7%0 - 30 cm 625 6%30 – 90 2,021 20%90 – 180 2,978 29%180 – 300 3,172 31%>300 604 5.9%
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Comparison of inundated area27
%
21% 26
%
17%
8%
17%
12%
26%
26%
18%
7% 6%
20%
29% 31%
6%0% 1%
0%
5%
10%
15%
20%
25%
30%
35%
Dry 0 - 30 cm 30 – 90 90 – 180 180 – 300 >300
Yr 2000 Yr 2050 Yr 2100
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Submergence of Embankments
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Adaptation OptionsOptions: • Long term measures – Ganges barrage
(OGDA option 8)• Mid term measure – Augmentation of Gorai
flow (OGDA option 7)• Construction of closures on main river
systems (Pussur, Shibsha and Kobadak rivers)
• Raising embankments to prevent overtopping
• Rehabilitation of drainage systems
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4 polder raised
Flood depth in Yr 2050 Area inundation (%) in Embankment raised condition (32 cm SLR)
26.8%
13.8%
66.3%
46.3%
6.8%
39.8%
41.5% 55.5%0.2%
0.4%
2.3%
0.00%
0.1%
0% 10% 20% 30% 40% 50% 60% 70% 80% 90% 100%
Bas
eEm
b.In
unda
ted
Emb.
Rai
sed
Area inundation (%) in Embankment raised condition (32 cm SLR)
26.8%
13.8%
66.3%
46.3%
6.8%
39.8%
41.5% 55.5%0.2%
0.4%
2.3%
0.00%
0.1%
0% 10% 20% 30% 40% 50% 60% 70% 80% 90% 100%
Bas
eEm
b.In
unda
ted
Emb.
Rai
sed
Dry 0 - 30 cm 30 - 90 cm90 - 180 cm 180 - 300 cm > 300 cmDry 0 - 30 cm 30 - 90 cm90 - 180 cm 180 - 300 cm > 300 cm
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13 polder raisedFlood depth in Yr 2100
Area inundation (%) in Embankment raised condition (88 cm SLR)
41.8%
17.3%
50.1%
18.7%
8.0%
57.3%
9.3%
6.6%
76.2%0.0%0.1%
0.5%
0% 10% 20% 30% 40% 50% 60% 70% 80% 90% 100%
Bas
eEm
b.In
unda
ted
Emb.
Rai
sed
Dry 0 - 30 cm 30 - 90 cm90 - 180 cm 180 - 300 cm > 300 cm
Area inundation (%) in Embankment raised condition (88 cm SLR)
41.8%
17.3%
50.1%
18.7%
8.0%
57.3%
9.3%
6.6%
76.2%0.0%0.1%
0.5%
0% 10% 20% 30% 40% 50% 60% 70% 80% 90% 100%
Bas
eEm
b.In
unda
ted
Emb.
Rai
sed
Dry 0 - 30 cm 30 - 90 cm90 - 180 cm 180 - 300 cm > 300 cm
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Emb. Raised: Comparison Land Class
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Example of SLR impact on drainagePolder 15
-1.0
-0.5
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
4.0
12:00 AM 2:24 AM 4:48 AM 7:12 AM 9:36 AM 12:00 PM 2:24 PM 4:48 PM 7:12 PM 9:36 PM 12:00 AM
Time
WL
(m+p
wd)
.
Polder WL_SLR88 cm River WL_SLR88 cm Polder WL_SLR32 cmRiver WL_SLR32 cm Polder WL_SLR00 cm River WL_SLR 00 cm
hBase = 2.19 m
hSLR32 cm = 2.1 hSLR88 cm = 1.73
TSLR88 cm = 6.5
TSLR32 cm = 6.8
TBase = 7 hrs
TSLR88 cm' = 7 hrs
TSLR32 cm' = 7.2 hrs
TBase' = 7.5 hrs
Drainage TimeTBase = 14.5 hrsTSLR32 cm = 14 hrsTSLR88 cm = 13.5 hrs
Head diffbase cond = 2.19 m 32 cm SLR = 2.1m88 cm SLR = 1.73 m
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Drainage under SLRWhat will happen with Increased Rainfall due to global worming??
h1h1
Additional volume of water to be drained
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Polder drainage improvement
priority
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Inundation in Sundarbans
44%
29% 27%26% 27%
47%
0%10%20%30%40%50%60%70%80%90%
0-50 cm 50 - 100 cm > 100 cm
Base Y2050 (32cm SLR) Y2100 (88cm SLR)
Sundarban area = 4,080 km2
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Salinity
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Salinity Propagation
0
2
4
6
8
10
12
14
16
30 50 70 90 110 130 150
Distance (km)
Salin
ity (p
pt)
Base condition SLR 32 cm SLR 88 cm
Gorai-Passur-Rupsha is 1.8 km and 9.0 km towards the inlands
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Salinity condition with adaptation
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Conclusions of the study
SLR will cause inundation of Polders
Drainage will be slower resulting longer drainage period
SLR should be included as a design parameter
Estimation of openings ( Sluices) should consider elongated drainage period
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Adaptation options in modelling of WRM
Increase Emb. Height – considering SLR
Increase Drainage opening –considering longer drainage period due to wetter wet season and higher d/s water level
Estimate Frequency considering trend due CC
Estimate Salinity propagation considering SLR and lower upstream flow due dryer dry season
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Thank You
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50
Major impacts of climate change on water resourcesIntensification of the hydrological cycle
Dryer dry seasons and wetter rainy seasons
Heightened risks of more extreme and frequent floods
and drought
Reduced availability of water
Deterioration of the quality and quantity of available
and accessible water
Melting of glaciers which will increase flood risk during
the rainy season, and strongly reduce dry-season water
supplies to one-sixth of the World’s population
Melting of ice in mountains and Polar Regions resulting
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Changes in Temperature and Precipitation
BangladeshAccording to ORCHID, 2007 report,
Rise in temperature By the 2020s: - 0.9 (A2) and 1.0°C (B1) - 2.0°C (A2) and 1.6°C (B1)Changes in annual rainfall by the 2020s is 0% (A2)and -1% (B1) Seasonal changes by the 2020s:- slightly wetter winters (+3% A2, 0% B1) - slightly wetter monsoon summers (+1% A2, +4% B1). By the 2050s average changes are slightly larger, with - winter drying (-3% A2, -4% B1)- summer wetting (+2% A2, +7% B1).
51SRES: Special Report on Emissions Scenarios
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26.8
%
66.3
%
6.8%
0.1%
0.0%
0.0%
0.2%
0.4% 2.3%
41.5
%
55.5
%
0.1%
13.8
%
46.3
%
39.8
%
0.1%
0.0%
0.0%
0.0%
10.0%
20.0%
30.0%
40.0%
50.0%
60.0%
70.0%
Dry 0 – 30 cm 30 - 90 cm 90 - 180 cm 180 - 300 cm > 300 cm
Base Y 2050 Y 2050 + embank. Raised
41.8
%
50.1
%
8.0%
0.1%
0.0%
0.0%
0.0%
0.1%
0.5% 9.
3%
76.2
%
13.9
%
17.3
%
18.7
%
57.3
%
6.6%
0.0%
0.0%
0.0%10.0%20.0%30.0%40.0%50.0%60.0%70.0%80.0%90.0%
Dry 0 - 30 cm 30 - 90 cm 90 - 180 cm 180 – 300cm
> 300 cm
Base Y 2050 Y 2050 + embank. Raised