Climate change impact on the Sundarbans Nandan Mukherjee Center for Climate Change and Environmental Research (C3ER) BRAC University
Climate change impact on the Sundarbans
Nandan MukherjeeCenter for Climate Change and Environmental Research (C3ER)
BRAC University
Physical setting
The Sundarbans appears deep greenAgricultural lands are lighter greenTowns appear as tanStreams are blue
• Part of GBM delta, spanning about 350 km in width in Southern Bangladesh and the state of West Bengal in India
• Within this geographical area, forests cover nearly 10,000 sq km, of which about 6,000 sq km are in Bangladesh:• Total land area is 4,143 km² • Water area of 1,874 km²
• Home to a large human population: 4.5 million in India, 7.5 million in Bangladesh
(Source: WWF, 2010)
Sundarbans: The Eco-region is both Unique and Uniquely Fragile!
Unique because:• Most extensive mangrove forests
exposed to freshwater and seawater mix.
• Most significant strongholds of the Royal Bengal Tiger, an endangered species.
• The flora of the Sundarbans, the mangrove, presents a natural buffer, a bulwark against coastal erosion and seawater ingress into one of the most densely populated regions of the world.
Sundarbans: The Eco-region is both Unique and Uniquely Fragile!
Sundarbans' fragility stems from its uniqueness. • Fragility due to rich ecological diversity, unique biota
comprising :– 334 species of plants, 49 species of mammals, 400
species of fish, 320 species of birds, 53 species of reptiles, 11 amphibian species
– Numerous invertebrates, phytoplankton, fungi, bacteria, zooplankton, benthic invertebrates, mollusks.
• Human induced climate change threatens the delicate balance between land, air, and sea (WWF, 2010)
Fragility due to rich ecological diversity, unique biota comprising :
OBSERVED EVIDENCES OF CLIMATE CHANGE
• Temperature is showing an increasing trend, as well as precipitation
• Variability in the climatic parameters has been increased
Variability in Temperature• Annual count of summer days
(>25°C) is increasing (J,S,K)• Monthly maximum value of daily
minimum temperature is increasing(S)
• Monthly minimum value of dailyminimum temperature is decreasing(K)
• Percentage of cool night and daysare decreasing (J)
• Percentage of warm days and warmspell duration is increasing (J)
• Cold spell duration is decreasing (J)• Diurnal temperature variability
(range) is increasing (J)
Variability in Rainfall• Annual total wet-day
precipitation is increasing(J,K)
• Number of heavy (>10 mm)precipitation days increasing(J,K)
• Number of very heavyprecipitation (>20 mm) daysincreasing (J,S)
• Annual count of days whenRainfall>5mm is increasing (K)
• Consecutive dry days aredecreasing (K)
Relationship between climate change and hydro-meterologyand hydro
GHG increases
Increases in radiative forcings
Increases in temperature
Changes in precipitation and
ET
Changes in soil moisture
Changes in soil groundwater
Changes in drought
Changes in runoff
Snow and ice melt
Sea level rise Backwater effect by tidal flow
Changes in floodChanges in river flow
Increases in
Increases in
Changes in
ET
Changes in soil
Changes in soil
drought
Salinity intrusion
Storm surge
Snow and ice melt
Sea level rise
EFFECTS OF CLIMATE CHANGE
•Increased occurrence of storm surge in the Bay of Bengal•Increased tidal flooding and permanent inundation•Increase in salinity, and change in water quality
EFFECTS OF CLIMATE CHANGE
Tropical Cyclone : some facts
Although science is not conclusive, IWTC (2006) noted that:
• If projected rise in sea level due to global warming occurs, then the vulnerability to tropical cyclone storm surge flooding would increase
• Some increase in cyclone peak wind speed and rainfall will occur if climate continues to warm
• Model studies and theory project a 3-5% increase in wind speed per degree Celsius increase of sea surface temperature.
Cyclone Sidr-It was never anticipated before
Source:http://cimss.ssec.wisc.edu/goes/blog/wp-content/uploads/2007/11/071115_sidr_mimic_anim.gif
Damage done by SIDR: A Preliminary Assessment
• Cyclone Sidr struck Bangladesh with winds of over 220 km/h (150mph) and a tidal surge of > 6m
• The authorities confirmed at least 2,3001 deaths.
• An estimated one million families are thought to have been affected.
NDVI, Satellite Aqua, 20th November 2007Resolution is 250 m
Forest Area Affected by cyclone SIDR
Affected area is 21% Of total Sundarbans area
Forest affected areas in the Sundarbans
Damage done by SIDR: A Preliminary Assessment
Effects on Fauna:• 40 species of mammals, • 400 species of birds and• More than 200 species of fishes fell victim to
the calamity.
Situation of Gorai• After the construction of
Farakka, dry seasonal flow in the Gorai River has reduced drastically.
• Mean dry seasonal flow decreased 72% and it has increase by 23% after the GWT
• Mean 1-day low flow has been decreased from 146 cumec to to 51 cumec
Line of equal salinity (5 ppt) for different sea level rise in dry season
0 SLR32 cm SLR88 cm SLR
0 SLR32 cm SLR88 cm SLR
0 SLR0 SLR0 SLR32 cm SLR32 cm SLR32 cm SLR88 cm SLR88 cm SLR88 cm SLR
0 SLR32 cm SLR88 cm SLR
0 SLR32 cm SLR88 cm SLR
in base condition with SLR 32 cm with SLR 88 cm
Condition Salinity (ppt)
0-1 ppt 1-5 ppt 5-10 ppt 10-15 ppt 15-20 ppt 20-25 ppt > 25 ppt
Base condition 10.8% 16.2% 19.1% 20.9% 15.9% 12.6% 4.5%
SLR 32 cm 9.2% 17.8% 18.0% 18.6% 15.6% 15.7% 5.0%
SLR 88 cm 4.0% 21.0% 17.8% 15.6% 14.9% 17.9% 8.8%
Salinity distribution in different scenario
Plant Type – Sundari – Health Index Under Different SLR Scenarios
Suitability of Sundri in SLR Base scenario
0
20
40
60
80
100
Block_A Block_B Block_C
Block in Sundarban
Perc
enta
ge o
f Sui
tabi
lity
Very Good Good Poor
Suitability of Sundri in SLR 32 cm scenario
0
20
40
60
80
100
Block_A Block_B Block_C
Block in Sundarban
Perc
enta
ge o
f Sui
tabi
lity
Very Good Good Poor
Suitability of Sundri in SLR 88 cm scenario
0
20
40
60
80
100
Block_A Block_B Block_C
Block in Sundarban
Perc
enta
ge o
f Sui
tabi
lity
Very Good Good Poor
31
Impact on tigers
Sea level rise (cm) (baseline is year 2000)
High tiger abundance habitat (km2)
Medium tiger abundance habitat (km2)
Low tiger abundance habitat (km2)
Total tiger habitat (km2)
0 574 1,445 2,155 4,1754 574 1,442 2,153 4,1698 551 1,352 2,117 4,021
12 527 1,229 1,941 3,69716 458 1,011 1,477 2,94620 309 622 840 1,77124 142 236 296 67428 37 74 48 159
Importance of Ganges-Gorai System
• Due to a drastic fall in the flow of the Gorai River, at least seven of the 15 rivers dependent on it, are now nearly dead while eight others are flowing timidly.
• The Gorai River normally has about 15 per cent of the Padma River’s annual flow volume. To keep the GoraiRiver bankful about 5 000 cum/sec flow will be required (BWDB 2000).
• So a minimum flow of about 2 000 cum/sec in the Gorai River and 13 334 cum/sec in the Ganges River, is necessary for fresh water inflows to the Sundarbans.
Proposed Ganges Barrage
Diversion flows down the Gorai River during the dry season could be made at 4 500 cum/s
How to combat the situation
• Integrated coastal and marine management• Monitoring the impact of climate change on
coral reef, Royal Bengal Tiger, crocodiles and Sundari tree
• Coastal vulnerability and risk assessment• Economic valuation of Sundarbans' resources • Afforestation and reforestation by salt tolerant
species
How to combat the situation
• Facilitating natural regeneration and natural succession of native tree species
• Creating public awareness through mass media• Initiating community based coastal forestation• Protecting existing mangroves against encroachment
and cutting• Establishing mechanisms to harness benefit from
Global Carbon Market