A Preliminary Assessment of the Sources of Hydrological Services in the Coastal Mangrove Forest of...

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29/09/2014 1 NRG BESS Early Career Researcher Conference on Biodiversity, Ecosystem Services and Sustainability Presenting Author : Ali Mohammad Rezaie Research Associate & Graduate Student Co-Authors : Dr. Munsur Rahman, Dr. Anisul Haque, Shah Alam , Ishtiaq Ahmed, Hafez Ahmed, Sumaiya, Md. Nurul Kadir, Muhammad Khalid Bin Siddique, Mansur Ali Jisan A Preliminary Assessment of the Sources of Hydrological Services in the Coastal Mangrove Forest of the Sunderbans Using Delft 3D And 1D HEC-RAS Models

Transcript of A Preliminary Assessment of the Sources of Hydrological Services in the Coastal Mangrove Forest of...

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NRG BESS Early Career Researcher Conferenceon

Biodiversity, Ecosystem Services and Sustainability

Presenting Author : Ali Mohammad RezaieResearch Associate & Graduate Student

Co-Authors : Dr. Munsur Rahman, Dr. Anisul Haque, Shah Alam , Ishtiaq Ahmed, Hafez Ahmed, Sumaiya, Md. NurulKadir, Muhammad Khalid Bin Siddique, Mansur Ali Jisan

A Preliminary Assessment of the Sources of Hydrological Services in the Coastal Mangrove Forest of the Sunderbans

Using Delft 3D And 1D HEC-RAS Models

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Background of the Study

• The Ganges–Brahmaputra–Meghna (GBM) the third largest freshwater outlet to the world’s oceans

• The Brahmaputra, after travelling about 1800 km through Tibet and India-the Ganges flows for about 2000 km through India, and enters through the western side of Bangladesh.

• The Ganges, Brahmaputra and Upper Meghna rivers join and flow into the Bay of Bengal as the Lower MeghnaEstuary.

Background of the Study

- Almost NO Primary data available

- The unique habitat of Sunderbandepends on the Hydrological regime

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Objective of the study

• Sources of the freshwater and saline water in the ?

• Dependence of the ecosystem services of the Sundarbanon the freshwater flows of the Lower Meghna estuary or Gorai River ?

• Change in salty to fresh environment inside Sundarban depending on the seasonality and flooding scenarios ?

Models Descriptions

• Model boundary contains the River Lower Meghna, Arial khan & Gorai in the up and Bay of Bengal near Sri-Lankan coast in the down.

• All major rivers in the southern part of Bangladesh is fitted by relatively finer grids.

• Minimum Grid Size: 400m x 400m (River)

• Maximum Grid Size: 5000 m x 5000 m (Ocean)

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Models Descriptions _Data Sources

• River Bathymetry Data-Bangladesh Water Development Board; ESPA DELTAS Bathymetry Survey

• Ocean Bathymetry Data - General Bathymetric Chart of the Oceans (GEBCO); 30 sec resolution

• Land elevation Data – Ministry of Water Recourses, CEGIS; 50m resolution

• Boundary Data – Bangladesh Inland Water Transport Authority, Bangladesh Water Development Board, NAOTIDE ocean tide generator

Model Validation_Delft3D

Calibration: Buriswar SW 20; Central Estuarine System

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-0.50

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4/29/2000 5/4/2000 5/9/2000 5/14/2000 5/19/2000 5/24/2000 5/29/2000 6/3/2000

MeasuredData

Model Data

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Model Validation

Calibration: Meghna Bhola SW 279; Eastern Estuarine System

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25-Jan-2000 4-Feb-2000 14-Feb-2000 24-Feb-2000 5-Mar-2000 15-Mar-2000 25-Mar-2000 4-Apr-2000

Measured

Model

Model Validation

Calibration: Rupsa SW 288.4; Western Estuarine System

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12-May-2000 14-May-2000 16-May-2000 18-May-2000 20-May-2000 22-May-2000 24-May-2000 26-May-2000 28-May-2000

Measured

New

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HEC-RAS Model Validation

20.00

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0.008 0.01 0.012 0.014 0.016 0.018 0.02

NR

MSE

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Roughness

Whole Year

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Wet Season

Model Performance for different roughness

HEC-RAS Model Validation

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NM

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(%)

Roughness

Whole Year

Dry Season

Wet Season

Model Performance for different roughness

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Results & Discussions

The discharge, total water volume and percentage of flow distribution among the estuarine systems

Results & Discussions

total water volume and percentage of flow distribution among the estuarine systems

Estuarine Systems Estuary

Total Dry Season Flow m3 (Nov-

April)

Total Wet Season

Flow m3 (May-

Oct)

Eastern Estuarine System

(EES) Meghna 66471(59%) 377285 (87%)

Central Estuarine System

(CES)

Arail Khan 930 (1%) 3897(1%)

Bishkhali 149 (0.5%) 211(<1%)

Baleshwar 19572 (20%) 22761 (6%)

Western Estuarine System

(WES)

Rupsa 3701(4.5%) 3021 (1%)

Shibsa 14023 (15%) 13823 (4%)

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Discharge distribution in the estuarine systems on an average

flooding conditions

79%

7.5% 0.5% 1%

3% 3%

6%

Results & Discussions

The model results show that the freshwater source of Sunderban is from Lower

Meghna; from eastern estuarine system to western !

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Tidal characteristics

0

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Velo

cit

y (

m/s

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Distance from upstream (km)

Meghna ( Ebb dominating)Flood

Ebb

Meghna (Eastern Estuary)

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cit

y (

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Distance from upstream (km)

Rupsha pasur (Flood dominating) Flood

Ebb

Rupsha- Sibsa

(Western Estuary; Sunderban)

Tidal Excursion

Tidal Excursion for all estuarine Systems for an average Year (Dry season)

Flooding Condition/ Season

Dry Season

Wet Season

Average

Extreme Dry

ExtremeWet

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Tidal Excursion

Tidal Excursion for all estuarine Systems for an average Year (Wet season)

Tidal Excursion

Tidal Excursion for all estuarine Systems for an extreme wet Year (Dry season)

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Tidal Excursion

Tidal Excursion for all estuarine Systems for an extreme wet Year (Wet season)

Tidal Excursion

Tidal Excursion for all estuarine Systems for an extreme dry Year (Dry season)

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Tidal Excursion

Tidal Excursion for all estuarine Systems for an extreme dry Year (Wet season)

Tidal Prism for all estuarine systems for an Extreme Wet year

0.000E+00

5.000E+11

1.000E+12

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MEGHNA TENTULIA BURISHWAR BISKHALI BALESHWAR RUPSA SIBSA

Wet Season

Flood Volume Ebb Volume

0.000E+00

5.000E+11

1.000E+12

1.500E+12

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MEGHNA TENTULIA BURISHWAR BISKHALI BALESHWAR RUPSA SIBSA

Dry Season

Flood Volume Ebb Volume

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Tidal Prism for all estuarine systems for an Extreme Dry year

0.000E+00

5.000E+11

1.000E+12

1.500E+12

2.000E+12

2.500E+12

3.000E+12

3.500E+12

MEGHNA TENTULIA BURISHWAR BISKHALI BALESHWAR RUPSA SIBSA

Wet Season

Flood Volume Ebb Volume

0.000E+00

5.000E+11

1.000E+12

1.500E+12

2.000E+12

2.500E+12

3.000E+12

3.500E+12

MEGHNA TENTULIA BURISHWAR BISKHALI BALESHWAR RUPSA SIBSA

Dry Season

Flood Volume Ebb Volume

Tidal Prism for all estuarine systems for an average year

0.000E+00

5.000E+11

1.000E+12

1.500E+12

2.000E+12

2.500E+12

3.000E+12

3.500E+12

MEGHNA TENTULIA BURISHWAR BISKHALI BALESHWAR RUPSA SIBSA

Wet Season

Flood Volume Ebb Volume

0.000E+00

5.000E+11

1.000E+12

1.500E+12

2.000E+12

2.500E+12

3.000E+12

3.500E+12

MEGHNA TENTULIA BURISHWAR BISKHALI BALESHWAR RUPSA SIBSA

Dry Season

Flood Volume Ebb Volume

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Tidal Prism at Discrete Estuarine System

Tidal Prism/ Flood-Ebb dominance for all estuarine Systems for an Average/

Representative Year

Preliminary Findings

• More than 80% of the total flow volume and discharge are draining out

through Lower Meghna in almost every conditions ( Average; Dry; Wet)

• the ecosystem services of the Sundarban depend on the freshwater

flows of the Lower Meghna estuary entering from the ocean side

• The computed tidal excursions and tidal prisms shows that the strength

of ebb and flood tides are almost same for the Sundarban system.

• So, the freshwater entering through the ocean during the flood tide are

completely drained during the ebb tide that results a rhythmic change of

salty to fresh environment inside Sundarban depending on the

seasonality and flooding scenarios.

• This will support co-existence of both freshwater and saline water

fisheries and other fluvial and marine habitats in Sundarban.

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Implications for ecosystem services

• Mangroves are key source of income for poor rural populations

• Mangroves also offer a range of supporting services, especially

protection against cyclones, erosion etc.

• Mangroves are dependent on a delicate salinity balance

• Sea level rise and upstream dams will reduce freshwater

availability

• Understanding current interactions between saline and fresh

water will help protect these already threatened resources.

• Change in the dynamic equilibrium due to either natural or man-

made will adversely affect the services of these particular

ecosystem resources of Sundarban.

Present Research Gap

Data:• Availability of accurate and time series data• Open access data

Design: • Interdisciplinary research designs are rare but required

Research:• Numerical quantification of river-sea flow dynamics,

morphological changes, hydrological regime dynamics• Affect of physical processes on ecosystem services• Impact of coastal hazards on biodiversity

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On-going work and Future Plan

- Upload results for open access

- Further analyse links between ecosystem resources, coastal morphological changes and extreme events.

- Further investigate the links between natural hazards and ecosystem services

Acknowledgements

• BUET IWFM research team who have had direct and indirect input to this study.

• Espa Deltas project (part of the ESPA programme)for funding this study.

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Thank You All !

“The scientist is not a person who gives the right answers, he's one who asks the right questions.”

― Claude Lévi-Strauss

For further Query : [email protected]