Climate changes susceptibility in agriculture: A high extent of food and nutrition insecurity in Coastal area of rural Bangladesh
Preface:
The concept of
global warming should not receive the amount of attention that is currently
determined on this issue because the earth continuously goes through spells of
warming and cooling. On the other hand the increasing temperature of the world
is but a part of this natural cycle and out of human control. Food and safe life is a social right of human being
but this changes of climate, now days the life of coastal areas people of
developing world is in high risk especially in Bangladesh and South Asian coastal
belt. We most of the people know climate change and greenhouse gas emission by
the industrial countries and particularly western region and some eastern
countries (Alam, M., 2003). Consequence results are sea level raising and
frequent natural calamities and ultimate outputs are food insecurity and
vulnerability to the rural people of coastal area in developing world. In this
paper I would like to dig out the root causes of climate change and its
consequences impact in rural coastal area of Bangladesh, where people are
living in hardcore poverty and natural vulnerability, particularly high level
of food insecurity. National and international social and political dilemmas
are the major reasons for these uneven and unexpected situations ever being.
Key words: Food insecurity, vulnerability, climate
change, natural disaster, hardcore poverty
1. Introduction:
Climate
variability is critical development issues for current world same as to Bangladesh.
The country is ranked as the most vulnerable to natural disasters due to
frequent cyclones, storm surges and floods, coupled with a high population
density and growth, and low climate resilience. In most years between 30-50% of
the country is affected by floods (BER, 2009, BBS, 2008). Climate change is
projected to change the intensity and frequency of natural disasters, worsen
the extent of flooding and negatively impact agricultural productivity,
infrastructure and development prospects (FAO, 1994, 1999, IFRI, 2010). Bangladesh has already taken
action to face the climate challenge by adopting various policies to address
climate change and investing heavily in adaption measures (IPCC, 2007). The
recently prepared Climate Change policy and Action Plan coherent evidently how Bangladesh
intends to scale up its effort to become resilient to climate change (NAPA, 2001,
GOB, 2006). In this paper I am exploring the possible complex underlying
reason to decreasing rice and other agriculture production which is
determined by Ministry of Agriculture report as well as my regular field
visit as a local inhabitant on the other hand to adapt the local community
especially the farmer group for continuing their rice and other agriculture
production in saline water in coastal area of Bangladesh (Brammer, et al., 1993).
Soil salinity is a worldwide problem. Bangladesh is no exception to it. In Bangladesh, salinization is one of the major natural hazards hampering crop production. Coastal area in Bangladesh constitutes 20% of the country of which about 53% are affected by different degrees of salinity (Islam, et al., 1999, Lokman Hoassin and et al., 2012). Agricultural land use in these areas is very poor. Declining land productivity with shift towards negative nutrient balance is among the main concerns with food security problem in the country. Salinity problem received very little attention in the past but now it is becoming emerging problems due to rapid climate change (Lokman Hoassin and et al., 2012). Nevertheless, symptoms of such land degradation with salinization are becoming too pronounced in recent years to be ignored. It has become imperative to explore the possibilities of increasing potential of these (saline) lands for increased production of food crops (Frihy, 2003). Thus combating land salinization problem is vital for food security in the country through adoption of long-term land management strategy (GEC, 2008, GIZ, 2010).
Figure-1: Bangladesh Map: General and natural soil structure.
Source: Soil Resources and
Development Institution (SRDI), Dhaka, Bangladesh
On the other hand, Bangladesh
is the world most climate change vulnerable country. Its economy draws the main
strength from agriculture sector. The sector contributes 19.10% to GDP (at
current prices 2008) and employs 50.28% of the labour force (BBS, 2008). Even
though increase in the shares of fisheries, livestock, and forestry, crop
sub-sector alone accounts for 60.83% share of agricultural GDP (BBS, 2008).
Crop agriculture in Bangladesh is, nevertheless, constrained by a number of
challenges almost every year (Lokman Hoassin and et al., 2012) due to diverse
structure of soil in Bangladesh (figure-1) and climate change. Major constraint
include loss of arable (cultivable) land, population growth, climate changes,
insufficient managing practices (fertilizer, water, and pests & diseases),
lack of quality seeds, and inadequate credit support to farmers, unfair price
of produces, and insufficient investment in research. Bangladesh has lost about
l million ha of arable land from 1983 to 1996 (BARC, 2007-08). Virtually, no
step has been taken by the government to arrest this loss. The land use policy
prepared by the government several years back has not yet been implemented.
Population growth poses an extra great risk to yield efficiency. Besides, crop
agriculture in Bangladesh has become regularly vulnerable to the hazards of
climate change–flood, drought, and salinity in particular (Islam, M.R., 2004, Islam, M.S., 2001, 2003). In addition, underprivileged
management practices, particularly those of pests and diseases, fertilizer,
water and irrigation have largely contributed to vital decline in crop production
(FAO, 2006). Small and marginal farmers that represent preponderance of farm
population are inhibited by poor monetary assets and cannot, consequently,
afford high administration expenses of high input technology (UNFCC, 2013).
That’s why we commencing this project to mitigate the local marginalized small
farmer as well as climate change vulnerable community may sustain their
livelihood to producing their main food rice in slain soil (UNFCC, 2013).
According to IPCC (2001), most
of the coastal area of Bangladesh go under saline water by 2050 or earlier. In
this issue and its consequences are mainly emerging impact on agriculture and
decreasing the yield of boro about 55-62% and wheat 61% by 2050 in Bangladesh
(FAO, 2006). Randomly cutting of the green trees by the local influential
particularly in the coastal zone for building shipyard and others activities (Agrawala,
S, et al., 2003). Bangladesh facing challenges every year for crop agriculture due
to reduce of cultivate land, population growth, rapid climate change, bad or inadequate
management practice or absent of good governance, unethical or unfair price of agriculture
product. On the other hand, after liberation each and every government has been
facing different challenges and high level absent of research initiatives in different
sectors and in particularly in agriculture sector therefore agriculture production
increasing rate is low comparatively neighbor countries (GEC, 2008). Asib Ahmed
(2011) argued, Bangladesh each year losing about 80,000 ha of cultivate land due
to growth of population and different housing plants. The land use policy of Bangladesh
should be reconstructed immediately for saving more agriculture land from the land
terror. Country’s commodities (food) production
is hampering by flood, drought, salinity and other natural hazard (Islam, M.S.,
2001, 2003, Islam, M.R, 2004)
1.
Objective:
To ensure food security through
increasing rice production in coastal saline area of Bangladesh as well as to
reduce climate change vulnerability by building awareness. It’s a goal or objective but without works together (Local, National and
International cooperation) this goal may not possible to achieve. Since long from
my childhood I have been seen the local people still has been fighting against
natural calamity. Every year they have lost their lives and assets including
domestic animals by natural disaster and its most and major underlying reason
is climate change and its related impacts. Therefore we feel to do something by
finding the realistic reasons and generalist cope up capacity for saving their
life and assets.
2.
Methodology:
Mainly secondary data are the main sources of information
including web searching. Based on that secondary data has been analysis in
STATA, where was following by econometrics formula and statistical rules. But more or less may be a little error has
been occurred due to time series and liner data time to time shifted, that’s
why further inclusive researches are important for get more intensive result in
this issue.
3. Literature review:
For getting in-depth information regarding the
climate change and its impact in agriculture and food security in rural costal
region of Bangladesh and its contemporary literature review. I am trying to
collect different writing such as article, books and reports, web publication.
3.1. Climate change (Definition):
“…a change in global climate
patterns apparent from the mid to late 20th century onwards, attributed largely to the
increased levels of atmospheric carbon dioxide produced by the use of fossil
fuels”. (Source: www.google.it)
3.2. UN Framework of Climate Change
Based on UN framework of
climate change, only purposes are affirmed as bellow:
“For the purposes of this convention:
1. "Adverse effects of
climate change" means changes in the physical environment or biota
resulting from climate change which have significant deleterious effects on the
composition, resilience or productivity of natural and managed ecosystems or on
the operation of socio-economic systems or on human health and welfare.
2. "Climate change"
means a change of climate which is attributed directly or indirectly to human
activity that alters the composition of the global atmosphere and which is in
addition to natural climate variability observed over comparable time periods.
3. "Climate system"
means the totality of the atmosphere, hydrosphere, biosphere and geo-sphere and
their interactions.
4. "Emissions" means
the release of greenhouse gases and/or their precursors into the atmosphere
over a specified area and period of time.
5. "Greenhouse
gases" means those gaseous constituents of the atmosphere, both natural
and anthropogenic, that absorbs and re-emits infrared radiation.
6. "Regional economic
integration organization" means an organization constituted by sovereign
States of a given region which has competence in respect of matters governed by
this Convention or its protocols and has been duly authorized, in accordance
with its internal procedures, to sign, ratify, accept, approve or accede to the
instruments concerned.
7. "Reservoir" means
a component or components of the climate system where a greenhouse gas or a
precursor of a greenhouse gas is stored.
8. "Sink" means any
process, activity or mechanism which removes a greenhouse gas, an aerosol or a
precursor of a greenhouse gas from the atmosphere.
9. "Source" means
any process or activity which releases a greenhouse gas, an aerosol or a
precursor of a greenhouse gas into the atmosphere.”
3.3. The Universal warming debates
among the different groups and nations:
In effect all scientists or
specialist agree that the globe has warmed a small amount since the year 1000
or earlier than, if we choose, since 1800-1850, when instrumented temperature
records became rationally precise and disseminated in enter areas of the world
(climate change facts, 2013). A large number of people which is increasing,
believe that any warming is too little that is interchangeable from the noise
in the environmental statistics (UNFCCC, 1997, Wigley and et al., 1987) and that the data have not been properly
adjusted for such things as urban heat island effects, and mechanism
calibration (UNFCCC, 1997, WB,
2000). This is particularly true of
the global data set, even though "urbanization has caused regional
increases in temperature that exceed those measured on a global scale (Figure-2), leading to urban heat islands as
much as 12°c hotter than their surroundings" (NCBI, 2013). Most scientists agree that
warming is better than cooling and many believe CO2 provides important
enhancements for forests and agriculture, even while also believing we should
not be fouling our nest (Hossain, 2001).
Figure-2: Global average
temperature 1850-2011
Source: Met Office Hadley Centre (web: www.metoffice.gov.uk/hadobs)
The grounds of the temperature increase, and therefore the future way, is matured
only within the harmony group of scientists. This is based on work of computer
modelers, believing their increasingly complex models show the cause is due to
man's activities and that there will be increasing temperatures according to
how much additional greenhouse gases are emitted (UNFCCC, 1997). There are many other scientists who are non-modelers, many with
backgrounds as atmospheric physicists, climatologists, engineers,
meteorologists, and paleo-climatologists (Wigley and et al., 1987), who do not believe the primary cause is
mankind, although this could be part of it. These scientists and the people who
follow them are often called climate change skeptics. Most of these scientists
believe that the sun is at the root of the warming (if any), but that other
factors are also at work (UNEP, 1989). To help
separate fact from fiction, an explanation of these thoughts is included here,
along with links to these materials.
The Hadley prediction chart and the observation chart below are from
the Climatic
Research Unit (CRU) at the University
of East Anglia, which is well respected for its historical databases maintained
at the global level, and which is used in IPCC assessments. See (figure-2, 3 & 4) the Hadley
composite charts for 1880 to present by month, year and quarter by
hemisphere.
Figure-4: Global land and ocean temperature
index:
3.4. IPCC climate change forecast
and recent study:
The IPCC 2007 climate change forecast for this
century was as follows:
“CO2 has risen from 280ppm to 379 ………. for 7 assumptions about future
temperatures.
Temperature increase. For the next 2 decades,
0.2 deg. C (0.4 F) ………….in high northern latitudes.
Sea level rise: For 6 sets of assumptions, the
mid-points are about 0.3 meters ( 1 ft.) Since 1850 sea level has risen about
200 mm (9 in.), ……………. and with no acceleration.
Other attributes: Ocean acidity should
rise with reduced ph units of 0.14 to 0.35; ……………. less in sub-tropics inland
areas.”
According the figure 3 and 4 we find the increasing picture of global temperature and out
most consequences of climate change.
The IPCC
in its most recent report in 2007 stated:
“Warming of the climate system is unequivocal, as is
now evident from observations of increases in global average air and ocean temperatures,
widespread melting of snow and ice, and rising global average sea level.'
'Most of the observed increase in globally averaged
temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic
greenhouse gas concentrations. This is an advance since the TAR's conclusion
that "most of the observed warming over the last 50 years is likely to have been due to the
increase in greenhouse gas concentrations". Discernible human influences
now extend to other aspects of climate, including ocean warming,
continental-average temperatures, temperature extremes and wind patterns”.
3.5.
Center of Excellence for Geospatial Information Science (CEGIS) Study:
Impact of
Sea-Level Rise (SLR) in Bangladesh on coastal communities and their Livelihoods
CEGIS study regularly find out real picture. Where CEGIS has tried to find out
“Investigating the impact of relative sea level rise on coastal communities and
their livelihoods in Bangladesh” in partnership with IWM and funded by UK
Department of Environment Food and Rural Affairs (DEFRA). The study considered
the climate change induced global sea level rise (GSLR), changes in concentration
of cyclones and precipitation for both low and high greenhouse gas emission
(GGE) scenarios according to the 3rd IPCC predictions. The impact analysis of
coastal communities and their livelihoods has been done for the projected year
2020, 2050 and 2080 by application of state of the art mathematical model
(Pfeffer, W.T. and et al. 2008, Pirazzoli, P.A., 1993).
3.6.
Other similar studies:
There are more
or less 2.5 billion world people’s livelihoods depend on agriculture (FAO, 2011),
of these, one billionaire family farmers working small farms. The other 1.5 billion
include farm laborers, fishers, migrant workers and pluralists (GOB,
IUCN, BCAS, 2003). Family farms are more than
just businesses. They also contribute to local, regional and national food
security and to economic development (UNDP, 2010). For the farmers themselves,
their farms are the basis for secure livelihoods and their well-being. World
agriculture will undergo far-reaching economic and corporeal change in the
coming 50 years (Ali, A.K.M.T., 2006). Population
increase, urbanization and income growth will drive the demand for food while
high energy prices, stress on natural resources, and climate change may act to
constrain supply. To feed the world’s growing population – projected to exceed
9 billion in 2050 (UN, 2009) – it will be necessary to boost the production of
food and to do so sustainably. Most important barrier to sustainable
agriculture is genetically modified organ (GMO) as well as high rate of
population growth. A sustainable agriculture is a system of agriculture that
will last. It is an agriculture that maintains its productivity over the long
run. Sustainable agriculture is both a philosophy and a system of farming. It
has its roots in a set of values that reflects an awareness of both ecological
and social realities (Ali, A.K.M.T., 2006, Ali,
A.M.S., 2005). Working with natural soil processes is of particular
importance. Sustainable agriculture systems are designed to take maximizes
advantage of existing soil nutrient and water cycles, energy flows, and soil
organisms for food production (Mondal, 2005).
These substances are rejected on the basis of their dependence on non-renewable
resources, disruption potential within the environment, and their potential
impacts on wildlife, livestock and human health (Karim,
Z., and et al., 1990). Instead, sustainable agriculture systems rely on
crop rotations, crop residues, animal manures, legumes, green manures, off-farm
organic wastes, appropriate mechanical cultivation, and mineral bearing rocks
to maximize soil biological activity (UNFCCC, 1997,
WB, 2000) and to maintain soil fertility and productivity (UNEP, 1989, UNFCCC, 1997, WB, 2000). Natural,
biological, and cultural controls are used to manage pests, weeds and diseases
(GIZ, 2010).
Due to various human
activities (mainly burning of fossil fuel), carbon dioxide (CO2) and other
greenhouse gases (methane, nitrous oxide, ozone, chlorofluorocarbons and water
vapor) are accumulated in the earth’s atmosphere, resulting in climate change.
Rising temperature expand the ocean volume in two ways. Primarily it melts mass
volume of ice of the polar region and secondly, causes thermal expansion of
water of the sea (figure 3 and 4). The relative contributions of thermal
expansion and ice melting to this sea level rise are uncertain and estimates
vary widely, from a small expansion effect through roughly equal roles for
expansion and ice melting to a dominant expansion effect (Sarkar and et al., 2003). These two factors increase
volume of ocean water of the earth and rise in the sea level (figure-5). The
human factor that is mainly responsible for global warming and sea level rise
is burning of fossil fuels. Deforestation is another human activity,
responsible for decreasing the CO2 sink. Miller (2004) states that, 75% of the
human caused emissions of CO2 since 1980 are due to fossil fuel burning and the
remainder is the result of deforestation, agriculture, and other human changes
in the land use. Emissions of CO2 from U.S. coal burning power and industrial
plants alone exceeded the combined CO2 emissions of 146 nations, which contain
75% of the world’s people (Miller, 2004). As a small nation, Bangladesh plays
an ignorable role for greenhouse gas emission (Sarwar, 2005). According to
National Adaptation Programs of Action (NAPA, 2002) dialogue, per capita CO2
emission in Bangladesh is 0.2 ton per year. But, statistic for developing
countries is 1.6, world average is 4.0, industrial world is 6.0 and the value
for United State of America (USA) is 20.0 ton. The developing countries,
representing nearly three-quarters of the world population, are responsible for
less than one-quarter of the fossil-fuel carbon emissions. The OECD countries,
with about 15% of the world population, account for around 44% of the total
emission and individually USA is solely responsible for 23% of the total yearly
fossil fuel carbon emission to the atmosphere (Singh,
2002). In contrast, Bangladesh contributes a microscopic 0.06% (Warrick
at el., 1993). Besides, ice melting, thermal expansion and also some local
factors like subsidence and siltation play role in the sea level rise process
(more detail in next heading no. 5).
4. Challenges and underlying reason of climate change vulnerabilities:
Rise in sea level, predicted 88 and 89 cm along the
coastline of Bangladesh roughly 25% of landmass is likely to be inundated
permanently if sea level rises by 89 cm which might create 18 million climate
refugees (UNFCC, 2013, Titus, J. G., and et al., 1991). With rising sea surface temperature, it
is very likely that the intensity and the frequency of the storm will increase saltwater
intrusion could further compound the problem by crippling the agriculture
sector. Loss of cultivable land and most of the land newly created coastline
would be useless and riverbank erosion will increase the southern region are
most horizontal to frequent flood, the north western regions are likely to
experience a slow desertification. The impact of climate change will radically
affect crop productivity, food security and livelihood (GIZ, 2010, IFPRI, 2010).
Due to chronic malnutrition caused by shrinking food grain supply will create
more vulnerable the health care and nutrition initiatives of Bangladesh (IFPRI,
2010). Water related impacts of climate change will likely be the most critical
for Bangladesh– largely related to coastal and riverine flooding, but also
enhanced possibility of winter (dry season) drought in certain areas. The
effects of increased flooding resulting from climate change will be the
greatest problem faced by Bangladesh. Both coastal flooding (from sea and river
water), and inland flooding (river/rain water) are expected to increase.
Flooding in
Bangladesh is a regular feature and has numerous adverse effects, including
loss of life through drowning, increased prevalence of disease, and destruction
of property. This is because much of the Bangladesh is located on a floodplain
of three major rivers and their numerous tributaries. One-fifth of the country
is flooded every year, and in extreme years, two-thirds of the country can be
inundated (Mirza, 2002). This vulnerability to flooding is exacerbated by the
fact that Bangladesh is also a low-lying deltaic nation exposed to storm surges
from the Bay of Bengal. There has been a trend in recent decades of much higher
inter-annual variation in area flooded (Pfeffer and
et al. 2008, Pirazzoli, 1993). Since the
late 1970s flooding events have tended to cover significantly lower or
significantly higher areas than what was observed in prior decades. This trend
in edges cannot be simply attributed to climate change. Rather several other
factors are at play. Better flood monitoring and control measures have probably
contributed to significant reduction in areal coverage of moderate flooding
events, which now cover much lower area (Lokman, 2012). According to figure-5
we find some projected scenario those are really significant responsible for
future enchantment of development and food and nutrition security in
Bangladesh. With regard to extremes at the upper end such as the 1988 and 1998
flooding events, climatic variability as well as long term climatic change
could certainly be contributing factors (Pfeffer and
et al. 2008).
Figure-5: Projected scenarios due to climate change in Bangladesh (six elements):
Parameters |
Worst
Scenario (predictable)
|
|
2050
|
2100
|
|
Relative Sea Level Rise |
153cm |
460cm |
Land Subsidence |
140cm |
240cm |
Shore Line Erosion |
1.5km |
3 Km |
Loss of Habitable Land |
16 km2 |
34 km2 |
Displace Population |
13% |
40% |
Reduction of Mangrove Area |
79 km2 |
95 km2 |
4.1. Increased
Chilly Melt:
Higher temperatures will result in chillier melt,
increasing runoff from the neighboring Himalayas into the Ganges and
Brahmaputra rivers. Given the altitude of the mountains and the enormous size
of the glaciers, this problem will most likely continue over the century (EPI, 2004, Elliott, L., 2004, Hossain, 2001, Iqbal,
2012).
The problem could be of even greater concern as there is evidence to show that
temperatures in the Himalayas are rising at higher rates, thereby contributing to
enhanced snow melt (Karim and et al.,
1990).
4.2. Increased
Rainfall:
While this is not certain,
the climate models tend to show increased precipitation, particularly during
the monsoon season. This will contribute to increased runoff. For example,
Mirza and Dixit (1997) found that a 2°C warming with a 10% increase in
precipitation would increase runoff in
the main three river of Bangladesh (Ganges, Brahmaputra, and Meghna) by 19%,
13%, and 11%, respectively (Lokman and et al., 2012).
4.3. Sea Level Rise
(SLR):
Sea level
rise will result in coastal flooding both under ambient conditions (given the
low elevations of the coast), and even more so in the event of storm surges (Pirazzoli,
1993, Lokman, 2012). It will also
indirectly cause riverine flooding by causing more backing up of the
Ganges-Brahmaputra-Meghna Rivers along the delta. The below figure-6 where a
collection of different six data set on SLR, shown from 1850 with an arbitrary
vertical offset for clear understand. Variances of these data sets are very
reasonable but its significance level is very important for policymaker and
decision makers for next course of action in climate change issues.
Figure-6: Global Sea level raising variance (Six
Datasets).
5.1. Sea Level Rise (SLR) and Salinity Intrusion:
5 5.3. An example of salinity intrusion:
5.4. Further action should taken:
6. Probably impacts of climate change to Bangladesh:
Figure-8: Kernel Density: Total commodities (food) production trends normal and estimated.
8. Role of Micro Loan/Credit for adapting and to ensure food security:
9. Recommendations and sustainability analysis:
9.1. Sustainable agriculture in global perspective:
9.2. Objectives of sustainable agriculture
9.3. Steps to a sustainable agriculture:
9.4. Approaches of sustainable agriculture (according to Elyas Khan, 2011)
Source:
Jevrejeva et al. 2006 (http://www1.ncdc.noaa.gov/pub/data/cmb/bams-sotc/2009/global-data-sets/SEALEVEL_sveta.txt)
5. Increased intensity
of cyclone winds and precipitation:
On the other hand, it is also possible – though
considerably more uncertain - that drought could increase under climate change.
Drought is a recurring problem in Bangladesh: 19 occurred between 1960 and 1991
(Lokman, 2012). Drought is typically caused when the
monsoon rains, which normally produce 80% of Bangladesh’s annual precipitation,
are significantly reduced (Miller, 2008). The southwest and northwest regions
of the country are most vulnerable to drought. The estimates from the climate
models do not yield a clear picture of how droughts will change. The estimated
changes in precipitation are not significant (EPI, 2004, Elliott, 2004). The models tend to show increased
monsoon precipitation and annual precipitation, which could mean fewer
droughts. But, a number of climate models estimate decreased annual
precipitation (Karim and et al.,
1990),
and the models tend to show reduced precipitation in the winter months. So the
possibility of increased drought cannot be ruled out.
5.1. Sea Level Rise (SLR) and Salinity Intrusion:
A direct
consequence of sea level rise would be intrusion of salinity with tide through
the rivers and estuaries. It would be more acute in the dry season, especially
when freshwater flows from rivers would diminish (Sarwar, M. G. M., 2005).
According to an estimate of the Master Plan Organization, about 14,000 sq km of
coastal and offshore areas have saline soils and are susceptible to tidal
flooding (BBS, 2008, See Figure-6). If some 16,000 sq km of coastal land is
lost due to a 45 cm rise in sea level, the salinity front would be pushed
further inland (Pfeffer, and et al. 2008).
Figure-7: Map of Bangladesh (Selected Area): Salinity
Concentration in Groundwater
Source: Soil Resources and Development Institution (SRDI), Dhaka,
Bangladesh
The present
interface between freshwater and saline water lies around 120 to 160 area, will
cause reduction in fish production. Pond culture in the coastal area will be
affected by intrusion of salt water into ponds, unless embankments are made
around them. Shrimp farming in the coastal area is a lucrative business.
Increase in salinity is likely to jeopardize the shrimp farming. For the last
few decades, more and more attention is being given to sea fish and brackish
water fisheries.
In the southwest as well as in the estuary, salinity levels are likely
to change in the polders due to sea level rise and increased rainfall. The
construction of these polders has been started in the 1960s under the Coastal
Embankment Project with the expressed objective of flood protection and
prevention of saline water intrusion. Since sea level rise would enhance saline
incursion, while increased rainfall would dilute the water to reduce salinity,
the net effect on polders and other associated croplands is uncertain (Mondal, 2005). Therefore, several studies indicate that the coastal zone
vulnerability would be acute due to the combined effects of climate change, sea
level rise, subsidence, and changes of upstream river discharge, cyclone and
coastal embankments area, will cause reduction in fish production (Lokman Hossain and et al., 2012, Mondal, 2005, Rashid,
and Islam, 2007). Pond
culture in the coastal area will be affected by intrusion of salt water into
ponds, unless embankments are made around them. Shrimp farming in the coastal
area is a lucrative business. Increase in salinity is likely to jeopardize the
shrimp farming (Mondal, 2005). For the last few decades, more and more attention
is being given to sea fish and brackish water fisheries.
5 5.2. Threat to agriculture production:
Effect of saline
water intrusion in the estuaries and into the groundwater would be enhanced by
low river flow, sea level rise and subsidence. The adverse effects of saline
water intrusion will be significant on coastal agriculture and the availability
of fresh water for public and industrial water supply will fall. Agriculture is
a major sector of Bangladesh's economy and the coastal area of Bangladesh is
very fertile for growing rice. Increase in salinity intrusion and increase in
soil salinity will have serious negative impacts on agriculture. The presently
practised rice varieties may not be able to endure increased salinity. The food
production does not seem to have a better future in the incident of a climate
change. In Bangladesh, rice production may fall by 10 % and wheat by 30 % by
2050 (Climate change in Asia 'too alarming to contemplate'-report, IPCC, 2007).
5 5.3. An example of salinity intrusion:
There is clear evidence of increased saline intrusion in the coastal
zones. For example in the coastal city of Khulna the main power station needs
to collect fresh water to cools its boilers by sending a barge upstream to get
freshwater. Over the last one decade the barge has to go further and further
upstream to get suitably fresh water for the purpose. While there is other
divert water flows to Calcutta), the trend towards salinization in the coastal
zone is very clear. (NAPA, 2005). Of the several factors that affect rice
production, a biotic stresses limit rice yields in 9 million hectares in
central and inland areas of the country (Lokman and et al., 2012). In India, water available for agriculture has
fallen by nearly 10% during the last decade (Lokman and et al., 2012). While in Bangladesh, about 2.8 million hectares of
coastal soil has become saline due to heavy withdrawal of surface and
groundwater for irrigation and intrusion of seawater (SRDI, 1998, Sing, 2002, Sarkar, M.A.R and et al., 2003). The total saline area forms a third of the 9
million hectares of total national cultivated area in Bangladesh. In addition,
drought has adversely affected rice in all three cropping seasons and ultimate
result is food insecurity of its population particularly rural poor.
5.4. Further action should taken:
Ø
Emphasize
salinity issue in Integrated Coastal Zone Management (ICZM) Plan and early
action should taken for early result;
Ø
More
study/ scientific research for innovating introducing salinity tolerant crop varieties;
Ø
Incorporate
drinking water crisis due to salinity in the National Water Policy Raise global
awareness of the need to address vulnerability to salinity as sea-level is
rising upstream flow must be increased.
6. Probably impacts of climate change to Bangladesh:
The impacts
of climate change including rising temperatures, changing rainfall and an
increase in the frequency and intensity of extreme weather events are already
being felt in many parts of the world. The consequences of these changes are
particularly serious in developing countries where livelihoods and ecosystems
are highly sensitive to changes in climate; the majority of people rely on the
natural resource base for their livelihoods; and the capacity to adapt is
limited by poverty, poor governance and inequitable distribution of resources
and power. The observed and predicted changes in climate have significant
implications for food and income security, health and access to water and other
natural resources. This is particularly true for poor rural people who are
dependent on agriculture for their livelihoods, and for poor women and other
marginalized groups who often lack access to the resources and services which
would allow them to adapt (Agrawala, S. and et al.,
2003). The impacts of climate change pretense a serious risk to the achievement
of social justice and an end to poverty (IFPRI, 2010). It is
clear that adaptation to climate change will be critical to achieving
sustainable development, and that this will require action across sectors and
at multiple levels. The international community must organize resources for
adaptation, and support capacity development in susceptible countries to tackle
the challenge of climate change. Otherwise high level food and nutrition
insecurity will be occurred in coastal area of Bangladesh.
7.
Climate
Change Impact in Agriculture and Food:
The
challenge for Bangladesh agriculture, to put simply, is to increase production,
while minimizing environmental impact. This includes conserving and protecting
the quality of the resources that determine the performance of agriculture like
land, water and air. Reductions in yield, although determined by many factors,
may be partially a consequence of land and water exploitation (FAO,
1994).
Figure-7:
Regression result of total demand of rice, rice production, white production
and net production of both commodities in Bangladesh over the time (using
STATA).
Figure-8: Kernel Density: Total commodities (food) production trends normal and estimated.
By the early
1980s approx. 53 percent of Bangladesh’s geographical area had been considered
degraded. The major process of land degradation is soil erosion (due to water
and wind erosion) contributing to over 75 percent of the land degradation. One
third of this land was degraded by human activities, while nearly one half was
degraded by a combination of human and natural causes. IUCN
and BCAS found a negative and significant negative relationship between
land degradation and food grain productivity in both the 1980s and 1990s. The future challenge
are very significant for sustainable agriculture.
8. Role of Micro Loan/Credit for adapting and to ensure food security:
Principal goal
of this study is to examine the impact of climate change on the food security
of rural poor and what Microfinance Institutions (MFIs) are doing to enhance
their food security in the context of climate change. Further, by identifying
the problems and expectations related to present forms of MFIs it intends to
explore the expected model of MFIs, which would ensure food security for the
rural poor.
In order to overcome food and nutrition vulnerability through
applying the following objectives of MFIs
o
To
identity the impacts of climate change on food security of rural poor.
o
To
investigate the changes in life style to ensure household food security in the
climate change context.
o
To
examine the role of Microfinance Institutions to address the changes in the
lives of rural poor due to climate change and to ensure their food security.
o
To
inspect the problems, constraints and expectations related to present forms of
Microfinance Institutions to enhance food security of rural poor in the climate
change context
o
To
explore a new and expected model of Microfinance Institution to enhance food
security of rural poor in the climate change context
9. Recommendations and sustainability analysis:
Based on experience to date
with poverty-environment mainstreaming as well as climate change adaptation, a
number of challenges can be anticipated for mainstreaming climate change
adaptation: Climate change is a complex issue with many links to development
issues. To make it relevant to decision makers across the government, it is
important to understand the linkages with broader poverty reduction and
pro-poor economic growth. This entails identifying the potential economic costs
of climate change as well as the benefits of taking action to enhance adaptive
capacity. Just as environmental
sustainability requires the involvement of key sectors (e.g. agriculture, land
use, water) and sub national bodies, climate change adaptation calls for the
active participation of most sectors of the economy, as well as of sub-national
authorities. Climate change impacts manifest themselves at the local level,
affecting the livelihoods, health and vulnerability of the population,
especially the poorest. It is thus important that the responses put forward at
the national level be rooted in local conditions, recognizing the great damage
that climate change can cause to livelihoods. Climate change is a long-term issue
whose consequences are not yet fully visible. It is also an issue that requires
managing risks and taking decisions in an environment of considerable
uncertainty.
On the other hand poverty-environment
mainstreaming and mainstreaming climate change adaptation countenance common
challenges and thus can advantage from a common approach. The
poverty-environment mainstreaming approach provides a credible platform to
assist countries in mainstreaming climate change adaptation into development
planning processes. While the proposed set of activities or modules and their
sequence are not fixed, a certain number will likely be needed to produce
lasting results. This ambiguity is not encouraging to decision-making on the
part of political leaders or government officials whose mandates and terms are
shorter, and who are concerned with political cycles. Essentially,
mainstreaming can be seen from two points of view, this standpoint of actors
inside institutions with a mandate to lead on an issue to be mainstreamed, and
the perception of development actors seeking to improve perform in a wide variety
of areas. Ultimately, the goal is full integration of climate change adaptation
as standard development practice. The idea of sustainable agriculture has been
around a long time. Since the very first crop was sown and animal was penned,
farmers have tried to ensure that their land produces a similar or increasing
yield of products year after back-breaking year; recent attempts to popularize
the concept build on this tradition. Sustainable agriculture is the use of
farming systems and practices which maintain or enhance (FACTA, 1990).
9.1. Sustainable agriculture in global perspective:
Agriculture
is sustainable when it is ecologically sound, economically viable, socially
just, culturally appropriate and based on a holistic scientific approach (GIZ,
2010). Low-External-Input and Sustainable Agriculture (LEISA) is agriculture
which makes optimal use of locally available natural and human resources (such
as soil, water, vegetation, local plants and animals, and human labor,
knowledge and skill) and which is economically feasible, ecologically sound,
culturally adapted and socially just (GIZ, 2010). Sustainable development is
the management and conservation of the natural resource base and the
orientation of technological and institutional change in such a manner as to
ensure the attainment and continued satisfaction of human needs for present and
future generations. Such sustainable development (in the agriculture, forestry
and fisheries sectors) conserves land, water, plant and animal genetic
resources, is environmentally non-degrading, technically appropriate,
economically viable and socially acceptable.
9.2. Objectives of sustainable agriculture
ü Make best use of the resources available;
ü Minimize use of non-renewable resources;
ü Protect the health and safety of farm workers, local communities and
society;
ü Protect and enhance the environment and natural resources;
ü Protect the economic viability of farming operations;
ü Provide sufficient financial reward to the farmer to enable continued
production and contribute to the well-being of the community; Produce
sufficient high-quality and safe food;
ü Build on available technology, knowledge and skills in ways that suit local
conditions and capacity.
ü Sustainable agriculture’s benefit to farm and community economies is
grounded in four well-established economic development principles and a fifth,
concern for the community (giz, 2010).
9.3. Steps to a sustainable agriculture:
The
agro-ecosystem is made up of many interacting components with multiple goals
(GIZ, 2010). Nurtures natural resources and maintains ecological balance is
driven by market demand and economically viable, ensures local replicability,
gender equity, and social acceptability, generates predictable income (Lokman,
2012) and considers availability of household labor and seasonality of labor
demand.
9.4. Approaches of sustainable agriculture (according to Elyas Khan, 2011)
Ø
“Sustainable agriculture has been practiced for many decades and
encompasses a tremendous number of different approaches described by many
different names. To this point, most of these approaches have largely been
limited to the substitution of environmentally.
Ø
More significant advances can be expected, however, as a result of
developments in the science and art of agro-ecosystem design and management.
Ø
Many of the approaches in conventional agriculture (minimum tillage,
chemical banding) would fall into the "efficiency" category.
Ø
Efforts to substitute safe products and practices (botanical pesticides,
bio-control agents, imported manures, rock powders and mechanical weed control)
are also gaining popularity.
Ø
The systems that focus on redesign of the farm are the most sophisticated,
generally the most environmentally and economically sustainable, over the long
term.
Ø
The approaches of sustainable agriculture are very variable, and are
dependent on the physical resources of the farmer, and the degree deficiencies
in support farm, the talents and commitment of the support available.”
9.5. Policies for sustainable agriculture:
9.5. Policies for sustainable agriculture:
The
Bangladesh govt. policies have always emphasized food grain self-sufficiency,
which has not necessarily coincided with agricultural sustainability. The
growth of agricultural production and productivity, which had risen
significantly during 1970s and 1980s, declined during 1990s. These slowdowns
have worsened since 2000, both overall agricultural production and food grains
production have shown negative growth rates in 2000-01 to 2002-03 periods (Figure-7
& 8). Decline in the growth rates
of agricultural production and productivity is a serious issue considering the
questions of food security, livelihood, and environment. This examination must
be framed not only by Bangladesh’s ongoing need to ensure food self-sufficiency
but also by the consequences of access to international markets. But the main
food of Bangladesh rice is also in vulnerable situation to increase production
and feeding the nation due to complex climate and its changes. Figure 9 shown
the productivity of rice over the period in Bangladesh and its increasing
significantly since millennium but upcoming climate change and SLR will be
building a barriers to its continuation.
Figure-9: Rice production in Bangladesh on areas
(Aus, Aman and Boro) FYs: 1971-2010 and 2010-12
10.
Conclusion:
This paper has argued the vulnerability of
Coastal Area’s people in Bangladesh to climate change with particular reference
to tropical cyclone occurrences and intensity, storm surges, coastal erosion,
and particularly slain water effect in agriculture. The analysis has been both
qualitative and quantitative. The vulnerability assessments may have many
shortcomings in terms of analytical procedures, and more research is needed to
arrive at a more reliable assessment so that a better response mechanism can be
developed. A few adaptation options have also been identified. These options
will pay a favorable return even if the climate change does not occur (Singh, O.P., 2002).
Bangladesh is dangerously susceptible to climate change
persuaded vulnerability (Sayma and Salehin, 2012), but the core elements of its vulnerability are fundamentally contextual.
May be Bangladesh is the only country in the world that lying on the deltaic
flood-plain of three major rivers and their numerous branches. Each year about
35- 75% of the country is normally flooded or flash flooded (S.N. Alam et. al. 2008). We should use our water resource
properly. As a result of climate change our water resource will face great
trouble.
High density of population (800/skm) in coastal area
of Bangladesh as well as higher percentages of poverty has shown in this region.
Many
projected climate change impacts including sea level rise, higher temperatures and
enhanced monsoon precipitation and run-off, potentially reduced dry season precipitation,
and increase in cyclone intensity would in fact reinforce many of these
baseline stresses that already pose a serious impediment to the economic
development of Bangladesh (Z. Karim. 1997). There is therefore a need to
clearly address whether climate change impacts are simply one more reason to
lower contextual vulnerability via business as usual economic development
activity, or whether adaptation to climate change might require suitable adjustment
in such projects or highlight the need for entirely new activities.
Thus far there has been no clear articulation on this
important issue, despite the disproportionately high number of conferences and
donor funded projects on climate change that have taken place in Bangladesh
over the past decade. New climate oriented projects in Bangladesh might
therefore require a higher doorsill of importance in the light of the
considerable body of knowledge and past experience that has already been gathered.
Nevertheless, climate change
and sea level rise are on the edge of a slanting position for Bangladesh. The cost
of climate change and sea level rise are terrible and they are by now taking
place. Floods are getting more common, storms are getting tougher, and land
droughts are getting longer. The melting of the ice caps in Greenland and the
Arctic is picking up pace and sea levels are rising. The habitats of plants and
animals are threatened, and food production is under pressure.
Climate change
and sea level rise and salinity impacts are really high for Bangladesh, though
the country plays very little role in greenhouse gas emissions, leading to
climate change and sea level rise. By affecting different livelihood activities
and important ecosystem of the country, sea level rise imposes a great threat
to the existence of Bangladesh. Therefore, Bangladesh government need to pay
keen attention to the issue and should develop strategy to combat sea level
rise impacts and thus safe its citizen. It will not be wise to think that sea
level will not rise at all, or to wait to see what happen in future. So,
development and implementation of adaptation policies and taking initiatives
for mitigation measures are the right ways to respond to sea level rise
impacts. It deserves research to find the solutions of the potential problems,
in practice and to develop salinity tolerant species for agriculture and
fisheries sectors (NGOF, 2013).
The coastal
protection activities should be done with sufficient drainage facilities.
Adaptation cost should be recovered from coastal resources using economic
instruments. I think researches also need to find out the way to save the
country’s broad range of biodiversity, threatened by the further experience.
For surviving adaptation and mitigation are two options for Bangladesh. Between
the two, the first one is local specific and second one is mitigation demands through
collective efforts of global communities. So, finally we can finish concluding
remark by a sentence “if OECD set their mind with considering way to developing
world than it could reduce a larger portion of climate change impact”.
11. Bibliography:
1. Agrawala, S., Ota, T., Ahmed, A.U., Smoth, J., Aalst,
M.V., 2003. Development and Climate Change in Bangladesh: Focus on Coastal
Flooding and the Sundarbans, Organisation for Economic Co-operation and
Development (OECD), Paris.
2. Alam, M., 2003. Bangladesh Country Case Study,
National Adaptation Programme of Action (NAPA) Workshop, 9-11 September 2003,
Bhutan.
3. Ali, A., 2000. Vulnerability of Bangladesh Coastal
Region to Climate Change with Adaptation Option. Bangladesh Space Research and
Remote Sensing Organization (SPARRSO), Dhaka.
4. Ali, A.K.M.T., 2006. Assessment of sea level
variations using climate and physiographic data of Chittagong coastal region.
M.S. Thesis, Institute of Forestry and Environmental Sciences, University of
Chittagong, Bangladesh.
5. Ali, A.M.S., 2005. Rice to shrimp: Land use/ land
cover changes and soil degradation in Southwestern Bangladesh, Land Use Policy.
6.
Asib Ahmed,2011.
Some of the major environmental problems relating to land use changes in the
coastal areas of Bangladesh: A review, Journal of Geography and Regional
Planning Vol. 4(1), pp. 1-8, January 2011
7.
BBS, 1999.
Statistical Yearbook of Bangladesh. 1999. Bangladesh Bureau of Statistics
(BBS).
8.
BBS, 2007.
Statistical Yearbook of Bangladesh. 2007. Bangladesh Bureau of Statistics
(BBS).
9.
BBS, 2008.
Statistical Yearbook of Bangladesh. 2008. Bangladesh Bureau of Statistics
(BBS).
10.
BCAS/RA/Approtech,
1994. Vulnerability of Bangladesh to climate change and sea level rise:
concepts and tools for calculating risk in integrated coastal zone management.
BCAS, Dhaka.
11.
Bennett, S.L.,
Rahman, A., Huq, S., 1991. Climate Change and Asian Farming Systems. In:
Proceedings, Asian Farming Systems Research/ Extension Symposium. Asian
Institute of Technology, Bangkok.
12.
Brammer,
H., Asaduzzaman M., Sultana, P., 1993. Effects of Climate and Sea level Changes on the Natural Resources of
Bangladesh. Briefing Document No. 3, Bangladesh Unnayan Parishad (BUP), Dhaka.
13.
Broadus, J.M.,
1993. Possible impacts of, and adjustment to, sea level rise: the cases of
Bangladesh and Egypt, In: Warrick, R.A., Barrow, E.M. and Wighley, M.L. (Ed.).
Climate and Sea Level Change: Observation, Projection and Implication,
Cambridge University press, Cambridge.
14.
Chanratchakool,
P., 2003. Problems in Penaeus monodon culture in low salinity areas,
Aquaculture Asia VIII (1), pp.54-56.
15.
Church JA,
Gregory JM, Huybrechts P., 2001. Changes in sea level. In: Houghton JT, Ding Y,
Griggs DJ et al (eds) Climate change 2001, the scientific basis. Cambridge
University Press, Cambridge, pp 639–693.
16.
CZPo, 2005.
Coastal Zone Policy, Ministry of Water Resources, Government of the People’s
Republic of Bangladesh, Dhaka.
17.
Climate Change
Facts web link, 2013. http://www.climatechangefacts.info/, 02 December, 2013 at 16.00 Roman Time.
18.
Cook RJ (2000).
Science-based risk assessment for approval and use of plants in agricultural
and other environments In: Persley GJ, Lantin MM (eds): Agricultural
Biotechnology and the Poor. Consultative Group on International Agriculture
Research, Washington, D.C. pp.123-130.
19.
Dalby, S., 2002.
Environmental Change and Human Security, ISUMA, pp. 71-79.
20. Earth policy Institute, 2004. Increased flows of
environmental refugees, EDC News, (Retrieved from
http://www.edcnews.se/cases/EnvRefugeesBrown.html., on October 14, 2004).
21. Elliott, L., 2004. The Global Politics of the
Environment, Palgrave Macmillan, New York.
22. F. Wambugu (2003), Biotechnology for sustainable
agricultural development in Africa: opportunities and challenges
23. FACTA (1990). “Food, Agriculture, Conservation and
Trade Act of 1990.Public Law 101-624, Title XVI, Subtitle A, Section 1603. The
National Agricultural Law Center.
24. FAO (1994) Development and Education Exchange
Papers (DEEP): Sustainable Agriculture and Rural Development: Part
1: Latin America and Asia, Rome, p. 5.
25. FAO, 1996. Technical Background Document of World Food
Summit. 1996. FAO.
26. FAO (1999). The state of food insecurity in the world.
Food and Agriculture Organization of the United Nations, Rome.
27. Elyas, KHAN, 2011. “Bangladesh: Challenges in
Sustainable Agriculture”, Master of development Studies (Course: Sustainable
Development Policy and Tools), East West University, Dhaka, Bangladesh, 2012.
Web link: http://elyaskhan.blogspot.it/2013/01/bangladesh-challenges-in-sustainable.html
28. Faisal, I.M., Parveen, S., 2004. Food Security in the
Face of Climate Change, Population Growth and Resource Constraints:
Implications for Bangladesh, Environmental Management 34(4), pp. 487-498.
29. Frihy, O.E., 2003. The Nile Delta-Alexandria Coast:
Vulnerability to Sea-Level Rise; Consequences and Adaptation, Mitigation and
Adaptation Strategies for Global Change 8, pp. 115–138.
30. GEC, 2008. Assessment on Peatlands, Biodiversity and
Climate change-Main Report, Global Environment Centre, Kuala Lumpur &
Wetlands International, Wageningen
31. GIZ (2010), Sustainable Agriculture – a Challenge for
the 21st Century, Conference report, Bonn, 23-24 November 2010.
32. GoB, IUCN, BCAS, 2003. Bangladesh: National Programme
of Action for Protection of the Coastal and Marine Environment from Land-Based
Activities, Department of Environment, Ministry of Environment and Forests,
Government of the People’s Republic of Bangladesh, Collaboration With IUCN –
The World Conservation Union, Bangladesh Country Office, and Bangladesh Center
for Advance Studies (BCAS)
33. GoB, MoWR, 2006. Coastal Development Strategy. Dhaka,
Ministry of Water Resources, Government of the People’s Republic of Bangladesh.
34. GoB, 1999. National Agricultural Policy-1999. Ministry
of Agriculture (GOB). Government of Bangladesh.
35. Golam Rahman. 2004. Windows of Agriculture in
Bangladesh.
37. Government of Bangladesh, 1993. Assessment of the
vulnerability of coastal areas to sea level rise and other effects of global
climate change. Department of the Environment, Dhaka.
38. GoB, 2005. National adaptation program of action.
Ministry of Environment and Forest, Dhaka, Bangladesh
39. GoB., UN, 2005. Millennium Development Goals:
Bangladesh Progress Report, Jointly prepared by Government of Bangladesh and
the United Nations Country Team in Bangladesh, Dhaka.
40. Hossain, M.S., 2001. Biological aspects of the coastal
and marine environment of Bangladesh, Ocean & Coastal Management 44, pp.
261-282.
41. Iftekhar, M.S., Islam, M.R., 2004. Managing mangroves
in Bangladesh: A strategy analysis, Journal of Coastal Conservation 10, pp.
139-146.
42. IFPRI, 2010. Food Security, Farming, and Climate Change to
2050: Scenarios, Results, Policy Options, International Food Policy Research
Institute, 2033 K Street, NW Washington, D.C. 20006-1002, U.S.A, 2010
43. IPCC, 2001a. Climate Change 2001: Mitigation,
Contribution of Working Group III to the Third Assessment Report of the
Intergovernmental Panel on Climate Change (IPCC), Cambridge University Press,
UK.
44. IPCC, 2001b, Climate Change 2001: Synthesis Report,
Contribution of Working Group III to the Third Assessment Report of the
Intergovernmental Panel on Climate Change (IPCC), Cambridge University Press,
UK.
45. IPCC, 2007a. Climate change 2007: The physical science
basis, Summary for Policymakers. IPCC, Geneva, 1–18.
46. IPCC, 2007b. Climate Change 2007: the Physical Science
Basis, Contribution of Working Group I to the Fourth Assessment Report of the
Intergovernmental Panel on Climate Change, edited By: Solomon, S., Qin, D.,
Manning, M., Chen, Z., Marquis, M., Averyt, K. B., Tignor, M., and Miller,
H.L., Cambridge University Press, Cambridge, UK and New York, NY, USA, 996 PP.,
2007.
47. IRRC, 2003. Hybrid rice in Bangladesh, Irrigated Rice
Research Consortium, International Rice Research Institute, Manila, the
Philippines, (Retrieved from http://www.irri.org/irrc/hybridrice/Bangladesh1.asp
on 20 November 2005).
48. Islam, M.R. (ed.), 2004. Where Land Meets the Sea: A
Profile of the Coastal Zone of Bangladesh, The University Press Limited, Dhaka.
49. Islam, M.S., 2001. Sea-level Changes in Bangladesh:
The Last Ten Thousand Years. Asiatic Society of Bangladesh, Dhaka.
50. Islam, S., Huda, A.U., 1999. Proper utilization of
solar energy in Bangladesh: effect on the environment, food supply and the
standard of living, Renewable Energy 17, pp. 255-263.
51. IPCC, 2007c. IPCC-2007: Impacts, adaptation and
vulnerability. Report of the working group-II. Intergovernmental Panel on
Climate Change (IPCC).
52. Karim, Z., Hussain, S.G. and Ahmed, M., 1990. Salinity
Problems and Crop Intensification in the Coastal Regions of Bangladesh. Soils
Publication No. 33, Soils and Irrigation Division, BARC, Farmgate, Dhaka,
Bangladesh, pp. 1–20.
53. Kausher, A., Kay, R.C., Asaduzzaman, M., Paul, S.,
1993. Climate Change and Sea-level Rise: the Case of the Coast. Briefing
Ducument No. 6, Bangladesh Unnayan Parishad (BUP), Dhaka.
54. Khan, M. Elyas, 2011. “Bangladesh: Challenges in
Sustainable Agriculture”, Sustainable Development: Policies and Tools, Masters
of Development Studies (MDS), East West University, Dhaka, Bangladesh, June,
2011. (Unpublished but academically accepted).
55. Md. Hafiz Iqbal, 2012. Impacts of Salinity on Rice
Production of Southwest Coastal Region of Bangladesh, Graduate School for
Development and Cooperation (IDEC), Hiroshima University.
56. Md. Lokman Hossain, Mohammed Kamal Hossain, Mohammed Abdus
Salam and Ashik Rubaiyat, 2012. SEASONAL
VARIATION OF SOIL SALINITY IN COASTAL AREAS OF BANGLADESH, International
Journal of Environmental Science, Management and Engineering Research Vol. 1
(4), pp. 172-178, Jul-Aug., 2012.
57. Md. Tajuddin Sikder, 2010. The Impacts of Climate
Change on the Coastal Belt of Bangladesh: An Investigation of Risks &
Adaptations on Agricultural Sector, Proc. of International Conference on
Environmental Aspects of Bangladesh (ICEAB10), Japan, Sept. 2010.
58. Miller, G.T., 2004. Living in the Environment. Brooks/
Cole-Thomson Learning, USA.
59. Mondal, M.H. 2005. Challenges and Opportunities of
sustainable crop production in Bangladesh. Eighth Biennial Agronomy Convention.
Bangladesh Society of Agronomy.
60. Mondal, M.K., 1997. Management of soil and water
resources for higher productivity of the coastal saline rice lands of
Bangladesh. PhD thesis. University of the Philippines, Los Baños, Philippines.
61. NAPA, 2002. Interactive Dialogue on Climate Change,
Bangladesh and the LDC Expert Group (LEG), Workshop on National Adaptation
Programs of Action (NAPAs), Held on 18-21 September 2002, Dhaka.
62. NEWSECURITYBEAT.org, 2013. Web link: http://www.newsecuritybeat.org/2013/10/perfect-storm-climate-challenges-aquaculture-net-food-security-gains-bangladesh/#.Uo4tydL0C6w, December, 2013, Rome, Italy.
64. Nicholls, R.J., Hoozemans, F.M.J., Marchand, M., 1999.
Increasing flood risk and wetland losses due to global sea-level rise: regional
and global analyses, Global Environmental Change 9, pp. S69-S87.
65. Pfeffer, W.T., Harper, J.T., O’Neel, S., 2008.
Kinematic constraints on glacier contributions to 21stcentury sea-level rise.
Science 321:1340 1343
66. Pirazzoli, P.A., 1993, Global sea level change and
their measurement. Global and planetary change, 8, 135-148.
67. Nagy, J. G. et. al. 2000. Impact of agriculture
research in Bangladesh, estimating returns to agricultural research. Bangladesh
Agricultural Research Management Project (ARMP), BARC and IFDC.
68. Nazmul Huda et. al. 2004. National Seed Management.
Agricultural Employees Conference and Technology Fair. Ministry of Agriculture.
69. OECD, 2003. ENVIRONMENT DIRECTORATE DEVELOPMENT
CO-OPERATION DIRECTORATE, Working Party on Global and Structural Policies,
Working Party on Development Co-operation and Environment, DEVELOPMENT AND
CLIMATE CHANGE IN BANGLADESH: FOCUS ON COASTAL FLOODING AND THE SUNDARBANS, By
Shardul Agrawala, Tomoko Ota, Ahsan Uddin Ahmed, Joel Smith and Maarten van
Aalst, COM/ENV/EPOC/DCD/DAC(2003)3/FINAL.
70. PATHIKRIT, 2012. Role of Microfinance Institutions to
Enhance Food Security in the Climate
Change Context: Gender based analysis of rural poor community of Bangladesh,
Technical Progress Report # 1, April, 2012, by Gulsan Ara Parvin.
71. PRDI , 2013. Climate Campaign Brief-6, Increasing
Salinity Threatens Productivity of Bangladesh, Participatory Research and
Development Initiative-PRDI, House 106/7, Monipuri Para, Tejgoan, Dhaka 1215.
Bangladesh
72. Rashid, M.H., Islam, M.S., 2007. Adaptation climate
change for sustainable development of Bangladesh agriculture. Bangladesh
country paper. p. 8.
74. Shamsuddoha, Md and Chowdhury, R. K., 2007. Climate
Change Impact and Disaster Vulnerabilities in the Coastal Areas of Bangladesh.
75. Sarkar, M.A.R., Ehsan, M., Islam, M.A., 2003. Issues
relating to energy conservation and renewable energy in Bangladesh, Energy for
Sustainable Development VII (2).
76. S. Jevrejeva, A. Grinsted, J. C. Moore, and S. Holgate,
2006. Nonlinear trends and multiyear cycles in sea level records, JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111,
C09012, doi:10.1029/2005JC003229, 2006, published 12 September 2006.
77. Sarwar, M. G. M., 2005. Impacts of sea level rise on
coastal zone of Bangladesh. Master’s thesis of Environmental Science Programme.
Lund University, Sweden.
78. SDNP, 2004. Climate Change & Bangladesh: Sea level
rise, Bulletin published on World Environment Day, 05 June 2004, Sustainable
Development Networking Programme (SDNP), Dhaka, Bangladesh, http://www.bdix.net/sdnbd_org/world_env_day/2004/bangladesh/climate_change_sealevel.htm.
79. Singh, O.P., 2002. Spatial Variation of Sea Level
Trend along the Bangladesh Coast, Marine Geodesy 25, pp. 205–212.
80. SMRC, 2003. The vulnerability assessment of the SAARC
Coastal Region due to sea level rise: Bangladesh case study. SAARC
Meteorological Research Center, Dhaka
81. SRDI, 1998a. Coastal area and water salinity map of
Bangladesh (1967 and 1997), Soil Resources Development Institute (SRDI), Dhaka,
Bangladesh.
82. SRDI, 1998b. Soil salinity map of Bangladesh (1973),
Soil Resources Development Institute (SRDI), Dhaka.
83. SRDI, 1998c. Soil salinity map of Bangladesh (1997),
Soil Resources Development Institute (SRDI), Dhaka.
84. Sayma Khanom and Mashriqurs Salehin, 2012. Salinity
Constraints to different water uses in coastal are of Bangladesh: A case study,
Bangladesh J.Sci. Res.25(1), 33-42, June, 2012
85. Syed Nural Alam et. al. 2008. Control of pests and
diseases in vegetables through integrated pest management. Agricultural
Technology Manual. BARI.
86. Titus, J. G., Park, R. A., Leatherman, S., Weggel, R.,
Greene, M. S., Treehan, M., 1991. Greenhouse effect and sea level rise: The
coast of holding back the sea. Coastal management, 19(3), 171-204.
88. UN, 2005. Retrieved from the United Nations website,
http://www.un.org/millenniumgoals/, during May 2005
89. UNDP, 2007: Human Development Report-2007/08.
90. UNEP, 1989. Retrieved from http://www.grida.no on 18
September 2004.
91. UNFCCC, 1997. Kyoto Protocol to the United Nations
Framework Convention on Climate Change, 11 December, Kyoto, Japan.
92. Wigley, T.M.L., Raper, S.C.B., 1987. Thermal expansion
of sea water associated with global warming, Nature 357, pp. 293-300.
93. WB, 2000. Bangladesh: Climate Change & Sustainable
Development. Report No. 21104, World Bank, Dhaka.
94. Z. Karim. 1997. Accelerated Agricultural Growth in
Bangladesh. Seminar on Agricultural Research on Development in Bangladesh. BARC,
Dhaka, Bangladesh.
7. Acronyms:
BBS
BCAS
BMD
CC
CCA
CCSLR
CEGIS
CNG
CO2
cm
CZPo
dS/cm
DoE
EPI
FAO
GBM
GHGs
GoB
GCC
GMO
GW
GLT
GST
IPCC
km2.
m
mm
MT
OECD
SLR
SMRC
SPARRSO
SRDI
SST
UN
UNDP
UNFCCC
WB
|
Bangladesh Bureau of Statistics
Bangladesh Centre for Advanced Studies
Bangladesh Meteorological Department
Climate Change
Climate Change and Adaptation
Climate Change and Sea Level Rise
Centre for Environment and Geographic Information System
Compressed Natural Gas
Carbon dioxide
Centimeter
Coastal Zone
Policy
Deci-simens
per centimeter
Department of Environment
Earth policy Institute
Food and Agriculture Organization (UN)
Ganges-Brahmputra-Meghna
Green House Gases
Government of Bangladesh
Global
Climate Change
Genetically
modified organ
Global Warming
Global Land Temperature
Global Sea Temperature
Intergovernmental Panel on Climate Change
Square Kilometer
Meter
Millimeter
Metric ton
Organization for Economic Co-operation and Development
Sea Level Rise
SAARC Meteorology Research Centre
Space Research and Remote Sensing Organization
Soil Resources Development Institute
Sea Surface Temperature
United Nations
United Nations Development Programme
United Nations Framework Convention on Climate Change
World Bank
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