4 Technological and Economic Potential of Options to Enhance, Maintain and
Manage Biological Carbon Reservoirs and Geo-engineering
4.1 Mitigation through Terrestrial Ecosystem and Land Management
Forests, agricultural lands, and other terrestrial ecosystems offer significant,
if often temporary, mitigation potential. Conservation and sequestration allow
time for other options to be further developed and implemented. The IPCC SAR
estimated that about 60 to 87GtC could be conserved or sequestered in forests
by the year 2050 and another 23 to 44GtC could be sequestered in agricultural
soils. The current assessment of the potential of biological mitigation options
is in the order of 100GtC (cumulative) by 2050, equivalent to about 10% to 20%
of projected fossil fuel emissions during that period. In this section, biological
mitigation measures in terrestrial ecosystems are assessed, focusing on the
mitigation potential, ecological and environmental constraints, economics, and
social considerations. Also, briefly, the so-called geo-engineering options
are discussed.
Increased carbon pools through the management of terrestrial ecosystems can
only partially offset fossil fuel emissions. Moreover, larger C stocks may pose
a risk for higher CO2 emissions in the future, if the C-conserving
practices are discontinued. For example, abandoning fire control in forests,
or reverting to intensive tillage in agriculture may result in a rapid loss
of at least part of the C accumulated during previous years. However, using
biomass as a fuel or wood to displace more energy-intensive materials can provide
permanent carbon mitigation benefits. It is useful to evaluate terrestrial sequestration
opportunities alongside emission reduction strategies, as both approaches will
likely be required to control atmospheric CO2 levels.
Carbon reservoirs in most ecosystems eventually approach some maximum level.
The total amount of carbon stored and/or carbon emission avoided by a forest
management project at any given time is dependent on the specific management
practices (see Figure TS.6). Thus, an ecosystem depleted
of carbon by past events may have a high potential rate of carbon accumulation,
while one with a large carbon pool tends to have a low rate of carbon sequestration.
As ecosystems eventually approach their maximum carbon pool, the sink (i.e.,
the rate of change of the pool) will diminish. Although both the sequestration
rate and pool of carbon may be relatively high at some stages, they cannot be
maximized simultaneously. Thus, management strategies for an ecosystem may depend
on whether the goal is to enhance short-term accumulation or to maintain the
carbon reservoirs through time. The ecologically achievable balance between
the two goals is constrained by disturbance history, site productivity, and
target time frame. For example, options to maximize sequestration by 2010 may
not maximize sequestration by 2020 or 2050; in some cases, maximizing sequestration
by 2010 may lead to lower carbon storage over time.
The effectiveness of C mitigation strategies, and the security of expanded
C pools, will be affected by future global changes, but the impacts of these
changes will vary by geographical region, ecosystem type, and local abilities
to adapt. For example, increases in atmospheric CO2, changes in climate,
modified nutrient cycles, and altered (either natural or human induced disturbance)
regimes can each have negative or positive effects on C pools in terrestrial
ecosystems.
Figure TS.6: Carbon balance from a hypothetical forest management
project.
Note: The figure shows cumulative carbon-stock changes for a scenario
involving afforestation and harvest for a mix of traditional forest products
with some of the harvest being used as a fuel. Values are illustrative
of what might be observed in the southeastern USA or Central Europe. Regrowth
restores carbon to the forest and the (hypothetical) forest stand is harvested
every 40 years, with some litter left on the ground to decay, and products
accumulate or are disposed of in landfills. These are net changes in that,
for example, the diagram shows savings in fossil fuel emissions with respect
to an alternative scenario that uses fossil fuels and alternative, more
energy-intensive products to provide the same services.
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In the past, land management has often resulted in reduced
C pools, but in many regions like Western Europe, C pools have now stabilized
and are recovering. In most countries in temperate and boreal regions forests
are expanding, although current C pools are still smaller than those in pre-industrial
or pre-historic times. While complete recovery of pre-historic C pools is unlikely,
there is potential for substantial increases in carbon stocks. The Food and
Agriculture Organization (FAO) and the UN Economic Commission for Europe (ECE)'s
statistics suggest that the average net annual increment exceeded timber fellings
in managed boreal and temperate forests in the early 1990s. For example, C stocks
in live tree biomass have increased by 0.17GtC/yr in the USA and 0.11GtC/yr
in Western Europe, absorbing about 10% of global fossil CO2 emissions
for that time period. Though these estimates do not include changes in litter
and soils, they illustrate that land surfaces play a significant and changing
role in the atmospheric carbon budget. Enhancing these carbon pools provides
potentially powerful opportunities for climate mitigation.
In some tropical countries, however, the average net loss of forest carbon
stocks continues, though rates of deforestation may have declined slightly in
the past decade. In agricultural lands, options are now available to recover
partially the C lost during the conversion from forest or grasslands.
4.2 Social and Economic Considerations
Land is a precious and limited resource used for many purposes in every country.
The relationship of climate mitigation strategies with other land uses may be
competitive, neutral, or symbiotic. An analysis of the literature suggests that
C mitigation strategies can be pursued as one element of more comprehensive
strategies aimed at sustainable development, where increasing C stocks is but
one of many objectives. Often, measures can be adopted within forestry, agriculture,
and other land uses to provide C mitigation and, at the same time, also advance
other social, economic, and environmental goals. Carbon mitigation can provide
additional value and income to land management and rural development. Local
solutions and targets can be adapted to priorities of sustainable development
at national, regional, and global levels.
A key to making C mitigation activities effective and sustainable is to balance
it with other ecological and/or environmental, economic, and social goals of
land use. Many biological mitigation strategies may be neutral or favourable
for all three goals and become accepted as "no regrets" or "win-win"
solutions. In other cases, compromises may be needed. Important potential environmental
impacts include effects on biodiversity, effects on amount and quality of water
resources (particularly where they are already scarce), and long-term impacts
on ecosystem productivity. Cumulative environmental, economic, and social impacts
could be assessed in individual projects and also from broader, national and
international perspectives. An important issue is "leakage" -
an expanded or conserved C pool in one area leading to increased emissions elsewhere.
Social acceptance at the local, national, and global levels may also influence
how effectively mitigation policies are implemented.
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