NEW JAMES BAY DAMS TO DESTROY PRISTINE QUEBEC RIVER

*New **James Bay** Dams to Destroy Pristine **Quebec** **River** *

International Opposition and Outrage over Hydro-Quebec’s Destructive $5B
Power Grab

ALBANY, NY, Sept. 12 /PRNewswire/ – American environmental groups today
announced their support for Canadian environmental groups and three Cree
Indian communities fighting Hydro-Quebec’s most recent assault on the James
Bay wilderness in Quebec, Canada.

Hydro-Quebec’s primary purpose for damming and diverting the Rupert River
-one of the last undammed major river in Northern Quebec – and creating a
massive reservoir equivalent in size to flooding two-thirds of Montreal, or
half of New York or New Orleans, is to generate new power capacity to sell to
the northeastern United States. Continue reading

Billings Gazette (Billings, Montana, U.S.)
September 25, 2007.

Forest experts consider research on climate change, fires
http://www.billingsgazette.net/articles/2007/09/25/news/state/29-forrest.txt

By NOELLE STRAUB
Gazette Washington Bureau

WASHINGTON – U.S. Forest Service officials and experts agreed Monday
that forest managers must take into account the complex relationship
between global climate change and increased wildfires when setting
policy.

Ann Bartuska, Forest Service deputy chief for research and
development, said the global climate is changing and will continue to
do so for many decades and that decisions made today by resource
managers will have implications through the next century.

The Forest Service’s climate change research focuses on how to help
forests adapt to increased stress, how to capture carbon dioxide in
soils, plants and wood products, and providing information to
policymakers, she said.

She said the agency has been gathering information on climate change
for years but that “we have more work to do.”

Last week, 75 scientists came together to look at gaps in knowledge
and new research and development, she said.

But if the agency focuses just on science and research, she said, it
will not meet the obligation to inform on-the-ground management
approaches.

“It doesn’t make sense if we’re just going to do the science if we
don’t put it in a form and in a way that is available to practitioners
and helping managers make better decisions,” Bartuska said. “And that
really is the foundation of the work we’re moving into.”

Bartuska said the growing cost of firefighting is one of the agency’s
“more significant challenges” and that it is eating into the budget
for overall programs.

“The escalating cost is something we’re very concerned about,” she said.

She advocated increasing fuel reduction work to reduce the threat of wildfires.

Susan Conard, Forest Service national program leader for fire ecology
research, said changes in temperature and precipitation patterns are
expected to lead to longer and more severe fire seasons in many areas
of the U.S. Increased burning will result in increased emissions of
carbon dioxide and other greenhouse gases, she said.

She said improved models will help scientists predict the interaction
between climate change, vegetation and wildfire. But she said more
research must be done.

“We need to understand more about fuels, about the effects of changing
burn severity on carbon release, and about how these effects will vary
regionally,” she said.

John Helms, professor emeritus at the University of California,
Berkeley, said various climate models show different outcomes, but
that one estimate is that wildfires will increase 50 percent by 2050
and will double by 2100.

Higher temperatures, lower humidity, increased drought and wind and
more lightning will be factors in the increased wildfires, he said.

Helms recommended fuels reduction to create better forest densities.

Climate change is expected to lower forest productivity in the West,
Helms added. As forests are placed under increased temperature and
water stress they will face a loss of vigor and increased mortality,
and that decay will add substantially to carbon emissions, he said.
Exposed soils will become warmer and subject to erosion, also
releasing substantial amounts of carbon to the atmosphere, he said.

A temperature increase of 3.5 degrees Centigrade (6.3 degrees
Fahrenheit) in the Rocky Mountain zone means the equivalent of
vegetation habitat moving 2,000 feet up slope or 200 miles further
north, Helms said.

Sen. Jon Tester, D-Mont., asked whether the Forest Service has taken
climate change into account in projecting its firefighting budget
needs over the next decade or two. Bartuska said the agency has not.

“We actually have just begun looking at what are the management
activities that are needed in response to climate change based on the
science that we’ve done, so we believe we’ll be improving our
estimates over time,” she added.

Tester also asked about let-it-burn policy during years when the
snowpack is below normal.

Helms replied that forest canopy plays a crucial role in protecting
snow on the ground from melting and emphasized the importance of
forests in relation to water supply.

Copyright (c) The Billings Gazette, a division of Lee Enterprises.
_________________________________________________________

MASSIVE, WARMING-INDUCED FOREST DIE-BACK!!

Calculations of forests’ potential as sustainable
biofuel assume that forests will survive expected
climate changes. But will they?
Lance

———————————————–
MASSIVE FOREST DIEBACK

ALLEN, CRAIG D.
U.S. Geological Survey, Jemez Mountains Field Station, Los Alamos, NM 87544

Presented August 9, 2007 at joint meeting of
Ecological Society of America and Society for
Ecological Restoration

In coming decades, climate changes are expected
to produce large shifts in vegetation
distributions, largely due to mortality.
However, most field studies and model-based
assessments of vegetation responses to climate
have focused on changes associated with natality
and growth, which are inherently slow processes
for woody plants-even though the most rapid
changes in vegetation are caused by mortality
rather than natality. This talk reviews the
sensitivity of western montane forests to massive
dieback, including drought-induced tree mortality
and related insect outbreaks. This overview
illustrates the potential for widespread and
rapid forest dieback, and associated ecosystem
effects, due to anticipated global climate change.

Climate is a key determinant of vegetation
patterns at landscape and regional spatial
scales. Precipitation variability, including
recurrent drought conditions, has typified the
climate of the Mountain West for at least
thousands of years (Sheppard et al. 2002).

Dendrochronological studies and historical
reports show that past droughts have caused
extensive vegetation mortality across this
region, e.g., as documented in the American
Southwest for severe droughts in the 1580s, 1890s
to early 1900s, 1950s, and the current drought
since 1996 (Swetnam and Betancourt 1998, Allen
and Breshears 1998 and in press). Drought stress
is documented to lead to dieback in many woody
plant species in the West, including spruce
(Picea spp.), fir (Abies spp.), Douglas-fir
(Pseudotsuga menziesii.), pines (Pinus spp.),
junipers (Juniperus spp.), oaks (Quercus spp.),
mesquite (Prosopis spp.), manzanitas
(Arctostaphylos spp.), and paloverdes (Cercidium
spp.).

Drought-induced tree mortality exhibits a variety
of nonlinear ecological dynamics. Tree mortality
occurs when drought conditions cause threshold
levels of plant water stress to be exceeded,
which can result in tree death by loss of
within-stem hydraulic conductivity (Allen and
Breshears – in press). Also, herbivorous insect
populations can rapidly build up to outbreak
levels in response to increased food availability
from drought-weakened host trees, such as the
various bark beetle species (e.g. Dendroctonus,
Ips, and Scolytus spp.) that attack forest trees
(Furniss and Carolin 1977). As bark beetle
populations build up they become increasingly
successful in killing drought-weakened trees
through mass attacks (Figure 1), with positive
feedbacks for further explosive growth in beetle
numbers which can result in nonlinear ecological
interactions and complex spatial dynamics (cf.
Logan and Powell 2001, Bjornstad et al. 2002).
Bark beetles also selectively kill larger and
low-vigor trees, truncating the size and age
distributions of host species (Swetnam and
Betancourt 1998).

The temporal and spatial patterns of
drought-induced tree mortality also reflect
non-linear dynamics. Through time mortality is
usually at lower background levels, punctuated by
large pulses of high tree death when threshold
drought conditions are exceeded (Swetnam and
Betancourt 1998, Allen and Breshears – in press).
The spatial pattern of drought-induced dieback
often reveals preferential mortality along the
drier, lower fringes of tree species
distributions in western mountain ranges. For
example, the 1950s drought caused a rapid,
drought-induced ecotone shift on the east flank
of the Jemez Mountains in northern New Mexico,
USA (Allen and Breshears 1998). A time sequence
of aerial photographs shows that the ecotone
between semiarid ponderosa pine forest and
piñon-juniper woodland shifted upslope
extensively (2 km or more) and rapidly (< 5 years) due to the death of most ponderosa pine across the lower fringes of that forest type (Figure 1). This vegetation shift has been persistent since the 1950s, as little ponderosa pine reestablishment has occurred in the ecotone shift zone. Severe droughts also markedly reduce the productivity and cover of herbaceous plants like grasses. Such reductions in ground cover can trigger nonlinear increases in erosion rates once bare soil cover exceeds critical threshold values (Davenport et al. 1998, Wilcox et al. 2003). For example, in concert with historic land use practices (livestock grazing and fire suppression), the 1950s drought apparently initiated persistent increases in soil erosion in piñon-juniper woodland sites in the eastern Jemez Mountains that require management intervention to reverse (Sydoriak et al. 2000). Thus, a short- duration climatic event apparently brought about persistent changes in multiple ecosystem properties. Over the past decade, many portions of the Western US have been subject to significant drought, with associated increases in tree mortality evident. GIS compilations of US Forest Service aerial surveys of insect-related forest dieback since 1997 show widespread mortality in many areas. For example the cumulative effect of multi-year drought since 1996 in the Southwest has resulted in the emergence of extensive bark beetle outbreaks and tree mortality across the region. In the Four Corners area piñon (Pinus edulis) has been particularly hard hit since 2002, with mortality exceeding 90% of mature individuals across broad areas (Figure 1), shifting stand compositions strongly toward juniper dominance. Across the montane forests of the West substantial dieback has been recently observed in many tree species, including Engelmann spruce (Picea engelmanni), Douglas-fir, lodgepole pine (Pinus contorta), ponderosa pine, piñon, junipers, and even aspen (Populus tremuloides). Continue reading

Environmental Science and Technology
September 19, 2007

Long legacy of fossil fuels
Earth may not recover from CO2-induced climate
change for hundreds of thousands of years.

By NAOMI LUBICK

The oceans have long memories. Researchers
recently reported that even if humans change
their carbon-producing ways, some of the impacts
of anthropogenic climate change, such as higher
ocean temperatures, will last for at least a
century. Now it appears that the long-term legacy
of burning fossil fuels may last for hundreds of
thousands of years, according to new research
published in Tellus B (DOI
10.1111/j.1600-0889.2007.00290.x) in September.

Toby Tyrrell and colleagues at Southampton
University (U.K.) call the long-term effects of
CO2 a “fossil fuel hangover”. They modeled the
movement of various forms of carbon through the
ocean and the atmosphere. In the model, they
imposed a huge dose of carbon on the planet from
1900 to 2300-a pulse of 4000 gigatons of
carbon-to simulate the burning of all fossil fuel
reserves.

At first, the modeled oceans became more acidic
because of rising CO2. But over many millennia,
the researchers found, oceans reached a different
final steady state compared with preindustrial
times. This new steady state had higher
atmospheric CO2 levels than before fossil fuel
burning, and the oceans were more alkaline and
had higher levels of dissolved inorganic carbon
(DIC). A feedback mechanism causes more carbonate
to dissolve in seawater, pushing even more carbon
back into the atmosphere. Depending on how much
CO2 humans produce in coming centuries, DIC and
alkalinity could increase by 50% over
preindustrial levels and atmospheric carbon by
100%.

“The system converges to a new equilibrium,” the
authors write. This means that the earth won’t be
able to recover completely from recent industrial
carbon emissions, as it did in the past when CO2
levels were high. Past high levels of atmospheric
carbon have been attributed to changes in earth’s
orbit, which occur about every 100,000 years and
trigger ice ages. According to Tyrrell and
colleagues, should business-as-usual CO2
emissions continue, the planet’s next ice age may
not come to pass for at least a half million
years.


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