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Gorai River
Impact of Upstream Interventions
on the Morphology of the
Ganges-Gorai
2
M Shahriar Sonet
ID-34
DHSM-2016
Ganges is the 2nd longest
river in the GBM basin
Sources of Ganges
Information on
Ganges & Gorai
River
Sources of Gorai
Discharge
Ganges Gorai
7,000 cumec
3
Gorai (Gorai-Madhumati: 261miles)
is one of the longest river in
Bangladesh
RIVER MAP
Figure 1: The Ganges & Gorai Rivers on map,
source: The Ganges water diversion: environmental effects and implications, Maminul Haque
Figure 2: Ganges river basin
source: Encyclopedia, Britannica
Flow volume
Natural & Human Interventions
&
their Impacts on the Ganges
1 2 3 4 Figure
Reference : The basics you can find anywhere 5 Steps To Successful Storytelling Published on April 5, 2014 Featured in: Marketing & Advertising
Changes in the Ganges River
&
its impact on the Gorai River
Erosion/acceleration
(ha)
Bangladesh India Total Change
(1980-1999)
Erosion 18,250 13,350 31,600
Acceleration 5,600 8,500 14,100
Net erosion 12,650 4,850 17,500
Continue..
Figure 4: Mean daily discharges of the
Gorai River at different periods
source: http://a-a-r-s.org/aars/proceeding/ACRS1999/Papers/WR99-8.htm
Changes in the planform of the Ganges River around
the Gorai off-take
Figure 5: Landsat TM images of dry season showing the
planform of the Ganges river around the Gorai off-take
source: The Ganges water diversion: environmental effects and implications
Changes in the Hydraulic regime of the Ganges
Post-Farakka period
When there was no treaty, i.e. during 1988-1996,
water levels in dry period were lower than when a
treaty was in effect i.e. , during 1975 to 1987
the morphological changes are noticed where the
river banks are composed of highly erodible
materials, i.e., at the downstream reach of the Gorai
in the immediate upstream of Borida.
Morphological change
Future of the Gorai River and Disaster
management perception
Aspects Period Effects
Planform 1975-1985
1986-1998
+
-
Severe upstream bank erosion along the right bank 1987-1992 +
Existence of water-sharing treaty 1975-1987(except
1976)
+
Absence of water-sharing treaty 1988-1996 -
Different aspects that have influenced the Gorai River flow
(1975-1996) in addition to the Farakka Barrage
*‘+/-‘representsanuncertainsituations
**Existingwater-sharingtreatywillexpirein2026
Different aspects that will influence the Gorai River flow
(2003-2030) in addition to the Farakka Barrage
Aspects Period Effects
Planform 2003-2010
2011-2030
-
+/-*
Severe upstream bank erosion along the
right bank
2003-2030 +/-
Existence of water-sharing treaty** 2003-2026 +
Existence /Absence of water-sharing
treaty**
2026-2030 +/-
* ‘+/-‘represents an uncertain situations
** Existing water-sharing treaty will expire in 2026
When a large scale human
interventions occurs it can modify the
system as rapidly as natural hazard.
This is what is probably happening to
Gorai River.
—Maminul Haque Sarker
13
THANK YOU

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Impact of Upstream Interventions on the Morphology of the Ganges-Gorai River_M Shahriar Sonet-BUP_DHSM

  • 2. Gorai River Impact of Upstream Interventions on the Morphology of the Ganges-Gorai 2 M Shahriar Sonet ID-34 DHSM-2016
  • 3. Ganges is the 2nd longest river in the GBM basin Sources of Ganges Information on Ganges & Gorai River Sources of Gorai Discharge Ganges Gorai 7,000 cumec 3 Gorai (Gorai-Madhumati: 261miles) is one of the longest river in Bangladesh
  • 4. RIVER MAP Figure 1: The Ganges & Gorai Rivers on map, source: The Ganges water diversion: environmental effects and implications, Maminul Haque Figure 2: Ganges river basin source: Encyclopedia, Britannica
  • 5. Flow volume Natural & Human Interventions & their Impacts on the Ganges 1 2 3 4 Figure Reference : The basics you can find anywhere 5 Steps To Successful Storytelling Published on April 5, 2014 Featured in: Marketing & Advertising
  • 6. Changes in the Ganges River & its impact on the Gorai River Erosion/acceleration (ha) Bangladesh India Total Change (1980-1999) Erosion 18,250 13,350 31,600 Acceleration 5,600 8,500 14,100 Net erosion 12,650 4,850 17,500
  • 7. Continue.. Figure 4: Mean daily discharges of the Gorai River at different periods source: http://a-a-r-s.org/aars/proceeding/ACRS1999/Papers/WR99-8.htm
  • 8. Changes in the planform of the Ganges River around the Gorai off-take Figure 5: Landsat TM images of dry season showing the planform of the Ganges river around the Gorai off-take source: The Ganges water diversion: environmental effects and implications
  • 9. Changes in the Hydraulic regime of the Ganges Post-Farakka period When there was no treaty, i.e. during 1988-1996, water levels in dry period were lower than when a treaty was in effect i.e. , during 1975 to 1987 the morphological changes are noticed where the river banks are composed of highly erodible materials, i.e., at the downstream reach of the Gorai in the immediate upstream of Borida. Morphological change
  • 10. Future of the Gorai River and Disaster management perception Aspects Period Effects Planform 1975-1985 1986-1998 + - Severe upstream bank erosion along the right bank 1987-1992 + Existence of water-sharing treaty 1975-1987(except 1976) + Absence of water-sharing treaty 1988-1996 - Different aspects that have influenced the Gorai River flow (1975-1996) in addition to the Farakka Barrage *‘+/-‘representsanuncertainsituations **Existingwater-sharingtreatywillexpirein2026
  • 11. Different aspects that will influence the Gorai River flow (2003-2030) in addition to the Farakka Barrage Aspects Period Effects Planform 2003-2010 2011-2030 - +/-* Severe upstream bank erosion along the right bank 2003-2030 +/- Existence of water-sharing treaty** 2003-2026 + Existence /Absence of water-sharing treaty** 2026-2030 +/- * ‘+/-‘represents an uncertain situations ** Existing water-sharing treaty will expire in 2026
  • 12. When a large scale human interventions occurs it can modify the system as rapidly as natural hazard. This is what is probably happening to Gorai River. —Maminul Haque Sarker

Editor's Notes

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