Climate variation refers to the seasonal and annual variation in temperature and rainfall patterns and their distribution within and between regions or countries. Climate change on the other hand refers to long term changes in global weather patterns resulting from changes in the composition of the atmosphere, brought about by emission of greenhouse gases (GHG) primarily carbon dioxide, Methane and nitrous oxide. Since the beginning of the industrial revolution, atmospheric concentrations of carbon dioxide have increased nearly 30%, Methane concentration have more doubled and nitrous oxide concentration have risen by about 15% (AEO, 2002). Those increases have enhanced the heat trapping capacity of the earth atmosphere. Increasing concentration of green house gases are likely to accelerate the rate of climate change.
Scientists expect that the average global surface temperature could rise 1-4.5oF (0.6-2.5oC) in the next fifty years and 2.2-10oF (1.4-5.8oC) in the next century with significant regional variations. Evaporation will increase as the climate warms, which will increase average global precipitation. Soil moisture is likely to become more frequent. Sea level is likely to rise along most of the U.S Coast. Scientists generally believe that the combustion of the fossil fuels and other human activities are the primary reasons for the increased concentration of carbon dioxide. Fossil fuel burned to run cars and trucks, heat homes and businesses, and power factories are responsible for about 98% of U.S carbon dioxide emissions, 24% of Methane emission, and 18% of nitrous oxide emission. Increased agriculture, deforestation, landfills industrial production, and mining also contribute a significant share of emission.
For Africa, climate variability is determined by prevailing patterns of sea surface temperature, atmospheric winds, regional climate fluctuations in the India and Atlantic Oceans, and by the El Nino Southern Oscillation (ENSO) phenomenon-the natural shift in ocean currents and winds off the Coast of South America, which occur every two to seven years. Africa is characterized by considerable climatic variation, both spatial and temporal, and by extreme event such as flooding and drought. These have particularly seriously consequences for the region because of the difficulties experienced in predicting their occurrence and in mitigating their effect and also because many African countries lack the financial resources to make adequate and timely recovery before the next climatic event. The countries of the Horn of Africa and Sahel are the most prone to drought, while those of Western and Central experience flooding periodically. Climate change is likely to bring increased frequency and severity of flooding, and drought to these areas already experiencing variability in rainfall. Additional concerns are risk of desertification in the semi-arid and arid regions, resulting to food insecurity.
Urgent action is required to develop alternative, clean and renewable sources of energy particularly for Africa to avoid increasing GHG emission and to stem widespread deforestation. The ability of human systems to adapt to and cope with climate change depend on a number of factors such as; Gross Domestic Productivity ( Capital, Incidence of poverty, life expectancy, insurance mechanisms, degree of urbanization, access to public health, access to education, community organizations, existing early warning systems and political stability. Those with the least capacity to adapt are the most vulnerable.
Climate Change Mitigation and Adaptation
Since the industrial revolution, human-induced activities including industrial processes, energy generation from fossil fuels, deforestation and intensive land use practices have produced Green House Gases (GHG) emissions into the atmosphere at rate faster than the planet ability to sequester them. Worldwide CO2 emission from fossil fuels continue to increase at a rate of about 1% p.a under a business as usual scenario, by 2035 human will annually emit about 12 billion tons of CO2. IPCC (2001) stated that “human influences will continue to change atmosphere composition throughout the 21st century”. Projection suggest that the global average surface temperature is expected to increase by 1.4oC to 5.8oC until 2100, with extreme value of over 100oC possible with a low probability. Warming would be particularly evident and rapid in land area, with special reference to those placed in high latitude and during winter. Globally, precipitation is projected to rise with the occurrence of more rainfall and large annual variations in some regions and less in others. Average sea level would rise by 0.09-0.88 meters between 1990-2100. Unusual weather events would likely increase including for instance greater frequency and intensity of E.L Nino type of weather patterns. According to these projections, many territories will experience intensified rainfalls, more violent cyclones will intervene in tropical areas while mid-latitude continental regions would be at the risk of drought. Climate change as described in the IPCC scenarios will have impacts on food security, fresh water supply, rural and urban settlements and their infrastructure, even if emissions would be curbed immediately. Thus human need to mitigate and adapt to climate change.
Instruments for action: Mitigation and Adaptation
Climate change is a problem with unique characteristics. It is global, long term (up to several centuries) and involves complex interactions between climatic, environmental, economic, political, institutional, social and technological processes. The United Nations framework convention on climate change (UNFCCC) identified two response to climate change; mitigation of climate change by reducing Green House Gas emission and enhancing sinks and adaptation to the impacts of climate change. Until recently, mitigation was seen as a stand alone solution to solving the climate change problem. Most of the industrialized countries therefore committed themselves as signatories to UNFCCC, Kyoto Protocol and recently the Paris deal to adopting National Policies and taking corresponding measure on the mitigation of climate change and to reducing their overall green house gas emissions (United Nations 1997). Unfortunately, an assessment of current efforts aimed at mitigating climate change as presented by the Working Group II fourth Assessment Report (WGIII AR4, 2007, Chapter II), shows that current commitments would not lead to a stabilization of atmospheric green house gas concentrations. In fact according to the Working Group I fourth Assessment Report (WGIAR4), no mitigation effort, no matter how rigorous and relentless, will prevent climate change from happening in the next few decades (Christensen et. Al, 2007, Meehl et. Al 2007). Adaptation is therefore unavoidable (Parry et.al 1998). However, reliance on adaptation alone is also likely to lead to a magnitude of climate change in the long run to which effective adaptation is no longer possible or only at very high social, economic and environmental costs. Today, it is no longer a question of whether to mitigate climate change or to adapt to it. Both adaptation and mitigation are now essential in reducing the expected impacts of climate change in human and their environment.
Mitigation and Adaptation: Complementary, Substitutable or Independent?
Adaptation and mitigation can be complementary, substitutable or independent of each other. Both are complimentary because they are tied to sustainable development. Although adaptation and mitigation may be substitutes for each other since mitigation will always be required to avoid dangerous and irreversible changes to the climate system. Both may be independent in the sense that the adaptation research community has put its emphasis on local and place-based analysis, the mitigation research community on the other hand has always focused attention on the global level. The mitigation research community has also focused strongly through not exclusively, on technological and economic issues and has traditionally relied on ‘top-dawn” aggregate modeling for studying tradeoffs inherent in mitigation, while the adaptation research community has focused on “bottom up” approach addressing several sectoral issues.
Irrespective of the scale of the mitigation measures that are implemented in the next 10-20 years, adaptation measures will still be required due to the inertia in the climate system. As noted by Stern (2006) and IPCC (2007) reports changes in the climate are already causing setbacks to economic and social development in some developing countries with temperature increases of less than 1oC. Unabated climate change would increase the risks and lost very substantially. Both adaptation and mitigation depend on capital assets, including social capital, and both affect capital vulnerability and GHG emissions. Through this mutual dependence, both are tied to sustainable development.
Important
Difference and Similarities between mitigation and adaptation
A:
Difference
Mitigation
|
Adaptation
|
1.
mitigation reduces all impact of climate change and reduces the adaptation
challenges.
|
1.
Adaptation is selective: it can take advantage of positive impact and reduce
negative one.
|
2.
Mitigation has global benefits: ancillary benefits might be released at the
local/regional level.
|
2.
Adaptation typically works on the scale of an impact system, which is regional
at best, but mostly local (although some adaptation might result in
spill-overs across national boundaries, for example by changing International
commodity prices in agriculture or forest product markets).
|
3.
Expressed at CO2 equivalents emissions reductions achieved by
different mitigation actions can be compassed and if the cost of implementing
the actions are known, their cost effectiveness can be determined and
compared.
|
3.
the benefits of adaptation are difficult to express in a simple meric,
impending comparisons between adaptation efforts. Moreover, as a result of
the predominantly local or regional effect of adaptation, benefits of
adaptation will be valued differently depending on the social, economic and
political context within which they occur.
|
4.
The benefits of mitigation carried out today will be evident in several
decades because of the long resistance time of the green house gases in the
atmosphere (ancillary benefits such as reduced pollution are possible in the
near term.)
|
4.
Many adaptation measures would be effective immediately and yield benefits by
reducing vulnerability to climate variability.
|
5.
The initiative for mitigation has tended to stem from international agreement
and ensuing national public policies (sometimes supplemented by
community-based or private-sector initiatives)
|
5.
whereas the bulk of adaptation actions have historically been motivated by
the self interest of affected private actors and communities, possible
facilitated by public policies.
|
B.
Similarities
Mitigation/Adaptation
1. The two
options are implemented on the same local or regional scale, and may be
motivated by local and regional priorities and interests as well as global
concerns.
2. Both options change relative price, which can
lead to slight adjustments in consumption and investment patterns and thus to
changes in the affected economy’s development pathway, but direct trade-offs
are rare.
3. Mitigation efforts can foster adaptive capacity
if they eliminate market failures and distortions as well as perverse subsidues
that prevent actors from making decisions on the basis of the true social cost
of the available options.
4. The implications of adaptation can be both positive
and negative, for mitigation. For example, afforestation that is a part of
regional adaptation strategy also make a positive contribution to mitigation.
In contrast, adaptation actions that require increase energy use from
carbon-emitting source (e.g in door cooking) would affect mitigation effort
negatively.
5. Both are tied to sustainable development.
Why
climate change mitigation and adaptation (Five reasons for concern)
Mitigation
and adaptation as response strategies are crucial in the world today because of
the following reasons; unique and threatened ecosystems, global aggregate
impacts, distribution of impacts, extreme weather events and large scale
singular effect.
(i) Unique and threatened ecosystems
Small
increases in global average temperature (e.g < 1oC mean global warming) can
cause significant and irreversible damage to some systems and species,
including possible local, regional and global loss. Aquatic life, critically
endangered species and natural systems such as forest birds, mountain gorillas,
coral reefs, mangroves, wetlands, semi-arid lands are being threatened by
climate change impacts. Human settlements along coastal regions, Islands, flood
plains and those who depend on natural resources that are sensitive to climate
change are already facing the impact of climate change.
(ii) Aggregate Impacts
A
small temperature increase could negatively impact on aggregate market sector
thereby affecting many Nation Gross Domestic Product (GDP). Sector such as
agriculture, water resources, human health could have negative net impact.
(iii) Distribution of Impacts
Developing
countries tend to be more vulnerable and are expected to suffer more to climate
change than developed countries. A small temperature increase will have net
negative impacts on market sectors in many developing countries due to low
adaptive capacity, poverty, illiteracy and other factors.
(iv) Extreme Weather Events
Many
climate impacts are related to extreme weather events, which cause massive
damage arising from their severity, suddenness and unpredictability. The
impacts of extreme events such as floods, cyclone, storms, hurricanes, high temperature
and fire could strangle affect specific sectors and regions. Agriculture and
water resources may be particularly vulnerable to change in hydrological and
temperature extremes. Heat-related mortality could increase with higher
temperatures. Floods may lead to the widespread of water related and vector
borne diseases, particularly in developing countries. Many of the monetary
damages from extreme events will have repercussions on a broad scale of
financial institutions, from insurance to investors to banks.
(iv) Large Scale Singular Effects
Human
induced climate change has the potential to trigger large scale changes in
earth’s systems that could have severe consequences at regional or global scales.
Example of such events include disintegration of the West Antarctic and
Greenland and Ice sheets, and major Perturbation of biosphere-related carbon
dynamics. These discontinuities could cause severe impacts on the regional and
even global scale that may be difficult to adapt to or mitigate.
Mitigation
as a response strategy
Mitigation
of climate change aims to answer some of these questions:
-
What can we do to reduce or avoid
climate change?
-
What are the policy action that can
overcome the barriers to implementation?
-
What will happen if we do not act now?
Key
Mitigation Technologies and Practices (options) currently available
S/N
|
Sector
|
Mitigation
Options
|
1
|
Forestry
|
Afforestation,
agroforestation, forest protection, community forestry, woodlot, reforestation,
etc
|
2
|
Energy
|
Improved
supply and distribution efficiency: fuel switching from coal to gas: nuclear
power, renewable heat and power (hydropower, solar, wind, geothermal and
bioenergy); combined heat and power.
|
3
|
Transport
|
More
fuel efficient vehicles, biofuels, modal shifts from road transport to rail
and public transport systems, non motorized transport cycling, walking);
land-use and transport planning.
|
4
|
Building
|
Efficient
lighting: more efficient electrical appliance and heating and cooling
devices, improved cook stores, improved insulation, passive and active solar
design for heating and cooling; alternative refrigeration fluids recovery and
recycle of fluorinated gases.
|
5
|
Industry
|
More
efficient end-use electrical equipment; heat and power recovery, material
recycling and substitution, control of non-CO2 gases emission, and
a wide array of process specific technologies.
|
6
|
Agriculture
|
Improve
crop and grazing land management, restoration of cultivated peaty soils and
degraded land; improved rice cultivation techniques and livestock and manure
management to reduce methane emission, improved nitrogen, fertilizer
application techniques to reduce N2O emissions, dedicated energy
crops to replace fossil fuel use; improve energy efficiency.
|
7
|
Waste
|
Landfill
methane recovery, waste incineration with energy recovery, composing of
organic waste, control waste treatment, recycling and waste minimization.
|
What
are the market based mechanisms for mitigating climate change according to
Kyoto Protocol?
Those
marked based mitigation mechanisms agreed upon in the Kyoto Protocol which will
be implemented by Annext 1 Parties (industrialized Countries) include the Clean
Development Mechanism (CDM), Emission Trading (ET) and Joint Implementation
(JI). These market mechanisms seek to lower
the cost of achieving emissions targets. The CDM allows Annex 1 Parties to
invest in projects in non-Annex 1 parties that reduce emissions or that enhance
sinks through afforestation or reforestation. The Annex 1 Party can then use
credits generated by those projects towards meeting its emissions target. Similarly,
through JI, Annex 1 Parties can receive credit for investing in projects in
other Annex 1 Parties. Finally, emission trading allows Annex 1 Parties to
trade credits or emission allowance among themselves.
It is
crucial for indigenous people to understand more fully these market-based
mechanisms. Equipped with adequate information, they can evaluate the risks and
opportunities which will allow them to make their own decisions on whether to
engage with the emission market or not. The best way to mitigate climate change
is to change the unsustainable production and consumption pattern which is
still the prevalent system dominating this world. The best mitigation measures involve
changing lifestyles individually and collectively, and structurally changing
the development path towards a sustainable and low-carbon one.
Adaptation
as a Response Strategy
According
to the IPCC, the requirements for a country to assume a high adaptative
capacity include; a prosperous and stable economy, a high degree of access to technology
options, well designed adaptation strategies, a system in place for the
dissemination of climate change and adaptation information at all levels as well
as a distribution of access to resources based on equity principles.
Baba
Ali Mustapha is with the Department of Planning/Research, Ministry of
Environment, Maiduguri, Borno State, Nigeria.
Reference:
The
research was based on the work of Professor Haruna K. Ayuba and Dr. A. Dami,
both of University of Maiduguri, Nigeria, from the Book “ Environmental
Science, an introductory text”.
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