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The natural vegetation
covering about 70% of the US land surface is strongly influenced
both by
the climate and by the atmospheric carbon dioxide (CO2)
concentration. To
provide a common base of information about potential changes in
vegetation
across the nation for use in the regional and sector studies,
specialized
ecosystem models were run using the two
major climate model scenarios selected for this Assessment. A
summary
of the national level results follows. Agricultural and production forestry systems are the
focus of separate sections of this Overview report.
What are Ecosystems?
Ecosystems are communities
of plants, animals, microbes, and the physical environment in
which they
exist. They can be characterized by their biological richness, by
the
magnitude of flows of energy and materials between their
constituent
species and their physical environment, and by the interactions
among the
biological species themselves, that is, by which species are
predators and
prey, which are competitors, and which are symbiotic.
Ecologists often categorize
ecosystems by their dominant vegetation -- the deciduous
broad-leafed
forest ecosystems of New England, the short-grass prairie
ecosystems of
the Great Plains, the desert ecosystems of the Southwest. The term
"ecosystem" is used not only to describe natural systems (such
as coral reefs, alpine meadows, old growth forests, or riparian
habitats),
but also for plantation forests and agricultural systems, although
these
ecosystems obviously differ in many important ways from the
natural
ecosystems they have replaced.
Ecosystems Supply Vital
Goods and Services
While we value natural
ecosystems in their own right, ecosystems of all types, from the
most
natural to the most extensively managed, produce a variety of
goods and
services that benefit humans. Some of these enter the market and
contribute directly to the economy. Thus, forests as sources of
timber and
pulpwood, and agro-ecosystems as sources of food are important to
us. But
ecosystems also provide a set of un-priced services that are
valuable, but
that typically are not traded in the marketplace. There is no
current
market, for example, for the services that forests and wetlands
provide
for improving water quality, regulating stream flow, and providing
some
measure of protection from floods. However, these services are
very
valuable to society.
Ecosystems are also valued
for recreational, aesthetic, and ethical reasons. These are also
difficult
to value monetarily, but are nevertheless important. The bird life
of the
coastal marshes of the Southeast and the brilliant autumn colors
of the
New England forests are treasured components of our regional
heritages,
and important elements of our quality of life.
Climate and Ecosystems
Climatic conditions
determine where individual species of plants and animals can live,
grow,
and reproduce. Thus, the collections of species that we are
familiar with
-- the southeastern mixed deciduous forest, the desert
ecosystems of the
arid Southwest, or the productive grasslands of the Great Plains
-- are
influenced by climate as well as other factors such as land-use.
The
species in some ecosystems are so strongly influenced by the
climate to
which they are adapted that they are vulnerable even to modest
climate
changes. For example, alpine meadows at high elevations in the
West exist
where they do entirely because the plants that comprise them are
adapted
to the cold conditions that would be too harsh for other species
in the
region. The desert vegetation of the Southwest is adapted to the
high
summer temperatures and aridity of the region. Forests in the east
are
adapted to relatively high rainfall and soil moisture; if drought
conditions were to persist, grasses and shrubs could begin to
out-compete
tree seedlings, leading to completely different ecosystems.
There are also many
freshwater and marine examples of sensitivities to climate
variability and
change. In aquatic ecosystems, for example, many fish can breed
only in
water that falls within a narrow range of temperatures. Thus,
species of
fish that are adapted to cool waters can quickly become unable to
breed
successfully if water temperatures rise. Wetland plant species can
adjust
to rising sea levels by dispersing to new locations, within
limits. Too
rapid sea-level rise can surpass the ability of the plants to
disperse,
making it impossible for coastal wetland ecosystems to
re-establish
themselves.
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Both temperature and
precipitation limit the distribution of plant communities.
The
climate (temperature and precipitation) zones of some of
the major
plant communities (such as temperate forests, grasslands,
and
deserts) in the US are shown in this figure. Note that
grasslands'
zone encloses a wide range of environments. This zone can
include
a mixture of woody plants with the grasses. The shrublands
and
woodlands of the West are examples of grass/woody
vegetation mixes
that occur in the zone designated as grasslands.
With climate change,
the areas occupied by these zones will shift relative to
their
current distribution. Plant species are expected to shift
with
their climate zones. The new plant communities that result
from
these shifts are likely to be different from current plant
communities because individual species will very likely
migrate at
different rates and have different degrees of success in
establishing themselves in new places. |
Effects of Increased CO2
Concentration on Plants
The ecosystem models used in
this Assessment consider not only changes in climate, but also
increases
in atmospheric CO2. The atmospheric concentration of CO2 affects
plant
species in ecosystems since it has a direct physiological effect
on
photosynthesis, the process by which plants use CO2 to create new
biological material. Higher concentrations of CO2 generally
enhance plant
growth if the plants also have sufficient water and nutrients,
such as
nitrogen, to sustain this enhanced growth.
For this reason, the CO2
levels in commercial greenhouses are sometimes boosted in order to
stimulate plant growth. In addition, higher CO2 levels can raise
the
efficiency with which plants use water. Different types of plants
respond
at different rates to increases in atmospheric CO2, resulting in a
divergence of growth rates due to CO2 increase. Some species grow
faster,
but provide reduced nutritional value. The effects of increased
CO2 level
off at some point; thus, continuing to increase CO2 levels will
not result
in increased plant growth indefinitely. There is still much we do
not
understand about the CO2 fertilization -- effect, its limits,
and its
direct and indirect implications.
Species Responses to
Changes in Climate and CO2
The responses of ecosystems
to changes in climate and CO2 are made up of the individual
responses of
their constituent species and how they interact with each other.
Species
in current ecosystems can differ substantially in their tolerances
of
changes in temperature and precipitation, and in their responses
to
changes in CO2; thus, new climate conditions are very likely to
result in
current ecosystems breaking apart, and new assemblages of species
being
created. Current ecosystem models have great difficulty in
predicting
these kinds of biological and ecological responses, thus leading
to large
uncertainties in projections.
What the Models Project
Modeling results to date
indicate that natural ecosystems on land are very likely to be
highly
sensitive to changes in surface temperature, precipitation
patterns, other
climate parameters, and atmospheric CO2 concentrations. Two types
of
models utilized in this Assessment to examine the ecological
effects of
climate change are biogeochemistry models and biogeography models.
Biogeochemistry models simulate changes in basic ecosystem
processes such
as the cycling of carbon, nutrients, and water (ecosystem
function).
Biogeography models simulate shifts in the geographic distribution
of
major plant species and communities (ecosystem structure).
The biogeochemistry models
used in this analysis generally simulate increases in the amount
of carbon
in vegetation and soils over the next 30 years for the continental
US as a
whole. These probable increases are small -- in the range of 10%
or less,
and are not uniform across the country. In fact, for some regions
the
models simulate carbon losses over the next 30 years. One of the
biogeochemistry models, when operating with the Canadian climate
scenario,
simulates that by about 2030, parts of the Southeast will likely
lose up
to 20% of the carbon from their forests. A carbon loss by a forest
is
treated as an indication that it is in decline. The same
biogeochemistry
model, when operating with the Hadley climate scenario, simulates
that
forests in the same part of the Southeast will likely gain between
5 and
10% in carbon in trees over the next 30 years.
Why do the two climate
scenarios result in opposite ecosystem responses in the Southeast?
The
Canadian climate scenario shows the Southeast as a hotter and
drier place
in the early decades of the 21st century than does the Hadley
scenario.
With the Canadian scenario, forests will be under stress due to
insufficient moisture, which causes them to lose more carbon in
respiration than they gain in photosynthesis. In contrast, the
Hadley
scenario simulates relatively plentiful soil moisture, robust tree
growth,
and forests that accumulate carbon.
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The maps above show
projections of relative changes in vegetation carbon
between 1990
and the 2030s for two climate scenarios. Under the
Canadian model
scenario, vegetation carbon losses of up to 20% are
projected in
some forested areas of the Southeast in response to
warming and
drying of the region by the 2030s. A carbon loss by
forests is
treated as an indication that they are in decline. Under
the same
scenario, vegetation carbon increases of up to 20% are
projected
in the forested areas in the West that receive substantial
increases in precipitation. Output
from Terrestrial Ecosystem Model (TEM) as part of the Vegetation
Ecosystem
Modeling and Analysis Project (VEMAP II) study.
Prolonged stress due to
insufficient soil moisture can make trees more susceptible to
insect
attack, lead to plant death, and increase the probability of fire
as dead
plant material adds to an ecosystem's "fuel load." The
biogeography models used in this analysis simulate at least part
of this
sequence of climate-triggered events in ecosystems as a prelude to
shifts
in the geographic distribution of major plant species. One of the
biogeography models, when operating with the Canadian climate
scenario,
simulates that towards the end of the 21st century, a hot dry
climate in
the Southeast will result in the replacement of the current mixed
evergreen and deciduous forests by savanna/woodlands and
grasslands, with
much of the change involving fire. This change in habitat type in
the
Southeast would imply that the animal populations of the region
would also
change, although the biogeography models are not designed to
simulate
these changes. The same biogeography model, when operating with
the Hadley
scenario, simulates a slight northward expansion of the mixed
evergreen
and deciduous forests of the Southeast with no significant
contraction
along the southern boundary. Other biogeography models show
similar
results. |
Major Uncertainties
Major uncertainties exist in
the biogeochemistry and biogeography models. For example,
ecologists are
uncertain about how increases in atmospheric CO2 affect the carbon
and
water cycles in ecosystems. What they assume about these CO2
effects can
significantly influence model simulation results. One of these
models was
used to show the importance of testing these assumptions.
Consideration of
climate change alone results in a 10% decrease in plant
productivity.
Consideration of both climate and CO2 effects results in an
increase in
plant productivity of 10%. This illustrates the importance of
resolving
uncertainties about the effects of CO2 on ecosystems.
With respect to biogeography
models, scientists are uncertain about the frequency and size of
disturbances produced by factors such as fire and pests that
initiate
changes in the distribution of major plant and animal species.
Will
disturbances caused by climate change be regular and small or will
they be
episodic and large? The latter category of disturbances is likely
to have
a negative impact on ecosystems services; the ability of
ecosystems to
cleanse the air and water, stabilize landscapes against erosion,
and store
carbon, for example, are very likely to be diminished.
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Maps of current and
projected potential vegetation distribution for the
conterminous
US. Potential vegetation means the vegetation that would
be there
in the absence of human activity. Changes in vegetation
distribution by the end of the 21st century are in
response to two
climate scenarios, the Canadian and the Hadley. Output is
from Mapped
Atmosphere-Plant-Soil System (MAPSS). |
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A substantial
portion of the Southeast's mixed forest is replaced by a
combination of savanna and grassland in response to fire
caused by
warming and drying of the region as projected by the
Canadian
model. The Hadley climate projection leads to a simulated
northward expansion of the mixed forest.
These particular
model runs show the response of vegetation to atmospheric
concentrations of CO2 that have stabilized at about 700
parts per
million, approximately twice the present level.
In the Southwest,
large areas of arid lands are replaced with grassland or
shrub/woodland in response to increases in precipitation
projected
by both models. |
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