Download Presentation

4 downloads 4245 Views 679KB Size Report
B2 2050. +24cm. No. B2_30y. B2_Max. I.B2.0_1. Extent of the floods caused by 30y storm rainfall (but without storm surge) and. 100y extreme upstream inflow ...
Scenario Modeling for Ho Chi Minh City: Future Climate Risk Communication Through Simulation and Visualization Anond Snidvongs Southeast Asia START Regional Center Chulalongkorn University Bangkok, Thailand

Nguyen Huu Nhan Southern Hydrometeorological Forecasting Center Ho Chi Minh, Viet Nam

Simulation and Modeling Tools Used

•Monsoon Driven Climate: PRECIS downscaled of ECHAM4 A2 and B2 GCM’s •Storms: Modified Linda •Sea Level: DIVA •Hydrodynamic: HydroGIS A total of 27 scenarios

INPUTS

SCENARIOS

PURPOSES

Seasonal Rainfall

Extreme Rainfall

Stor m Surge

Mean Sea Level

Upstream Inflow

Landuse

I.BL.0

Baseline _Max

No

No

Baseline

Baseline

Baseline

I.B2.0

B2_Max

No

No

B2 2050 +24cm

Baseline

Baseline

I.A2.0

A2_Max

No

No

A2 2050 +26cm

Baseline

Baseline

I.BL.1

Baseline _Max

No

No

No

Baseline

2050

I.B2.1

B2_Max

No

No

B2 2050 +24cm

Baseline

2050

I.A2.1

A2_Max

No

No

A2 2050 +26cm

Baseline

2050

I.BL.0_1

Baseline _Max

Baseline _30y

No

No

100y

2050

I.B2.0_1

B2_Max

B2_30y

No

B2 2050 +24cm

100y

2050

I.A2.0_1

A2_Max

A2_30y

No

A2 2050 +26cm

100y

2050

Extent and duration of the ‘regular’ seasonal monsoon floods with current landuse

Extent and duration of the ‘regular’ seasonal monsoon floods with planned future landuse and flood control system

Extent of the floods caused by 30y storm rainfall (but without storm surge) and 100y extreme upstream inflow; with planned future landuse and flood control system

INPUTS

SCENARIOS

PURPOSES

Seasonal Rainfall

Extreme Rainfall

Storm Surge

Mean Sea Level

Upstrea m Inflow

Landuse

II.BL.0

Baseline_ Max

Baseline_30y

Linda

No

100y

Baseline

II.B2.0

B2_Max

B2_30y

Linda

B2 2050 +24cm

100y

Baseline

II.A2.0

A2_Max

A2_30y

Linda

A2 2050 +26cm

100y

Baseline

II.BL.1

Baseline_ Max

Baseline_30y

Linda

No

100y

2050

II.B2.1

B2_Max

B2_30y

Linda

B2 2050 +24cm

100y

2050

II.A2.1

A2_Max

A2_30y

Linda

A2 2050 +26cm

100y

2050

II.BL.0_a

Baseline_ Max

No

Linda

No

Baseline

Baseline

II.B2.0_a

B2_Max

No

Linda

B2 2050 +24cm

Baseline

Baseline

II.A2.0_a

A2_Max

No

Linda

A2 2050 +26cm

Baseline

Baseline

II.BL.0_b

Baseline_ Max

Baseline_30y

No

No

100y

Baseline

II.B2.0_b

B2_Max

B2_30y

No

B2 2050 +24cm

100y

Baseline

II.A2.0_b

A2_Max

A2_30y

No

A2 2050

100y

Baseline

Extent of the ‘extreme’ floods driven by combination of tropical storms (typhoons) surge, mean sea level rise, 30y rainfall and 100y upstream inflow; with current landuse Extent of the ‘extreme’ floods driven by combination of storms surge, mean sea level rise, 30y rainfall and 100y upstream inflow; with planned future landuse and flood control system Extent of floods and saltwater intrusion caused by storm surge and sea level rise only in current landuse

Extent of the floods caused by 100 y extreme upstream inflow and 30y storm rainfall (without storm surge) in current landuse

INPUTS

SCENARIOS

PURPOSES

Seasonal Rainfall

Extreme Rainfall

Storm Surge

Mean Sea Level

Upstream Inflow

Landuse

III.bl.0

Baseline_ Min

No

No

No

Baseline

Baseline

III.B2.0

B2_Min

No

No

B2 2050 +24cm

Baseline

Baseline

III.A2.0

A2_Min

No

No

A2 2050 +26cm

Baseline

Baseline

I.BL.1_1

Baseline_ Max

Baselin e_30y

No

No

100y

2050

I.B2.1_1

B2_Max

B2_30y

No

B2 2050 +24cm

100y

2050

I.A2.1_1

A2_Max

A2_30y

No

A2 2050 +26cm

100y

2050

Extent of combination effect of drought and sea level rise on the water quality especially risk of salination under current land use

Extent of floods driven by 30y rainfall, 100y upstream inflow and mean sea level rise; with planned future landuse and flood control system

3 and 5-days Extreme Rainfalls with 30 and 100 y Return Periods 250

Basel

250

200

200

150

150

Basel

100

30-y

100

30-y

50

100y

50

100y

0

0 1

2

3

4

5

6

7

250

1

2050 A2

2

3

4

5

6

7

250

200

200

150

150

2050 A2

100

30-y r

100

30-y

50

100y

50

100y

0

0 1

2

3

4

5

6

7

250

1

2050 B2

2

3

4

5

6

7

250

200

200

150

150

2050 B2

100

30-y

100

30-y

50

100y

50

100y

0

0 1

2

3

4

5

6

7

1

2

3

4

5

6

7

DIVA Sea Level Projections

7 103 104

23 2 11 22 2 11

01 2 11 24 2 11

105

18 2 11

106 107 108

BEN RE

O C RANG

8

109

23 1 11

RAV H

212211111

CAN HO

24 1 11

G ANG

01 2 11

02 2 11

03 2 11

04 2 11

05 2 11

12

06 2 1

VNH O NG

07 2 11

P O CHM NH

08 2 11

11

09 2 11

NNH

10 2 11

E

14 2 11 13 2 11

KEN

16 2 11 15 2 11

17 2 11

O

12 2 11

CAM AU

20 2 11 19 2 11

DO NG HAP

11 2 11

03 3 11 02 3 11

9 21 2 11

08 3 11

10 07 3 11 06 3 11 05 3 11 04 3 11

13

DAC C

O NG E AM O NG

A DO G NAI

BARA BNH HU N

Storm Scenarios

NG ANG ANG VUNG AU

Linda PA2 Linda PA1

Linda 1997 110

Fig 1. The effect of flood control system of HCMC for points inside flood protection area (example: District 1 of HCMC)

Fig 2. The effect of flood control system of HCMC for points outside flood protection area (example: Sai Gon Main River)

With Dykes