Fulco Ludwig: salt intrusion and water supply

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Climate change impacts on Salt water intrusion in Coastal Bangladesh Dr. Fulco Ludwig Earth System Science Group Wageningen University 27 January 2016

Transcript of Fulco Ludwig: salt intrusion and water supply

Page 1: Fulco Ludwig: salt intrusion and water supply

Climate change impacts on Salt water intrusion in Coastal Bangladesh

Dr. Fulco Ludwig Earth System Science Group

Wageningen University 27 January 2016

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Ganges

Brahmaputra

Meghna

GBM BASINS The GBM Basins drain 1.72 Mi km2 area 93% of the area outside Bangladesh 75-80% of flow in 5 months of monsoon

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Saltwater intrusion is caused by a combination of sea level rise and reduction of dry season river flows

Dis

char

ge

(m2/

s)

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Water Supply for the city of Khulna

§ Khulna is the 3rd largest of Bangladesh § Local water is saline during the dry season § Only deep groundwater can be used for drinking water § Large parts of the Khulna residents drink saline water

during part of the year § ADB and Japanese gvt wanted to invest 250 million US$

in a new drinking water plant § The question is where to build to plant and where to get

the water from and will this be affected by climate change

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Salt intrusion in May in Southwest Bangladesh

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Modelling framework to assess future salt intrusion

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Future Sea Level Rise – end of 21st Century – From IPCC AR5

IPCC 2013

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0 SLR 32 cm SLR 88 cm SLR

Impact of SLR on Salinity Intrusion

Hiron Point

Bay of Bengal

Mongla

Khulna

Movement of 5 ppt Salinity line

Source: IWM

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Climate change impact on flow of the Ganges under 2 degree warming

-­‐60%

-­‐40%

-­‐20%

0%

20%

40%

60%

80%

100%

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

Change  in  Ganges  Flow

 Com

pared  to  

1985

-­‐200

5  (%

)

CNRM  RCP8.5  (2035-­‐2055) SMHI  RCP8.5  (2029-­‐2049)

Reduction in flow in May when salt intrusion is highest

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Climate change impact on salt water intrusion

0.0

0.5

1.0

1.5

2.0

2.5

3.0

3.5

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

Salinity

 (PPT)

Atharobanki  R:  Avge.  Salinity  in  RCP  8.5  Scenario  RCP  8.5  (2029-­‐2049) Base  (1985-­‐2005) RCP  8.5  +  Gorai  Dredging2 degree warming Gorai dreding + 2 degree warming

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Where to develop the drinking water plant

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Conclusions

§ Combined reduced dry season river flows and sea level rise result in large scale increases in salt water intrusion

§ Salt intrusion is likely to increase in the future in Southwest Bangladesh unless dramatic infrastructure measures are taken

§ Water intake for drinking water supply near Khulna is not suitable due to increasing salt water intrusion

§ This study recommends Mollarhat as intake point due to low salinity

§ In addition a reservoir can be developed