Joule,
Journal Year:
2024,
Volume and Issue:
8(2), P. 430 - 449
Published: Jan. 19, 2024
Because
biomass
residues
do
not
cause
land-use
change,
soil
carbon
changes
are
commonly
considered
in
life
cycle
assessments
(LCAs)
of
biofuel
derived
from
forest
adopted
by
regulatory
agencies.
Here,
we
investigate
the
impacts
organic
(SOC)
caused
removing
Southern
US
on
intensity
biofuels.
We
show
that
average
greenhouse
gas
(GHG)
emissions
SOC
over
100
years
8.8–14.9
gCO2e
MJ−1,
accounting
for
20.3%–65.9%
GHG
biofuel.
These
SOC-associated
vary
time
frame,
site
conditions,
and
management
strategies.
For
land
management,
converting
to
is
more
climate
beneficial
than
on-land
decay
or
pile
burning,
depending
fossil
fuel
substitution
conditions.
Our
results
highlight
need
include
assessment
LCAs,
policymaking,
even
when
used
no
change
involved.
Proceedings of the National Academy of Sciences,
Journal Year:
2019,
Volume and Issue:
116(51), P. 25734 - 25744
Published: Nov. 25, 2019
The
response
of
forests
to
climate
change
depends
in
part
on
whether
the
photosynthetic
benefit
from
increased
atmospheric
CO
2
(∆C
a
=
future
minus
historic
)
compensates
for
physiological
stresses
higher
temperature
(∆T).
We
predicted
outcome
these
competing
responses
by
using
optimization
theory
and
mechanistic
model
tree
water
transport
photosynthesis.
simulated
current
productivity,
stress,
mortality
mature
monospecific
stands
with
soil,
species,
sampled
20
continental
US
locations.
modeled
without
acclimation
∆C
∆T,
where
acclimated
adjusted
leaf
area,
capacity,
stand
density
maximize
productivity
while
avoiding
stress.
Without
acclimation,
-driven
boost
net
primary
(NPP)
was
compromised
∆T-driven
stress
associated
vascular
failure.
With
NPP
biomass
(C
storage)
accentuated
cooler
futures
but
negated
warmer
reduction
biomass.
Thus,
hotter
reduced
forest
through
either
or
acclimation.
Forest
outcomes
depended
projected
climatic
/∆T
ratios
were
above
below
thresholds
that
neutralized
negative
impacts
warming.
Critically,
if
do
not
acclimate,
must
be
ca
.
89
ppm⋅°C
−1
avoid
chronic
threshold
met
55%
projections.
If
rise
67
increase,
lower
71%
Nature Communications,
Journal Year:
2018,
Volume and Issue:
9(1)
Published: Dec. 11, 2018
Abstract
Climate−tree
growth
relationships
recorded
in
annual
rings
have
recently
been
the
basis
for
projecting
climate
change
impacts
on
forests.
However,
most
trees
and
sample
sites
represented
International
Tree-Ring
Data
Bank
(ITRDB)
were
chosen
to
maximize
signal
are
characterized
by
marginal
growing
conditions
not
representative
of
larger
forest
ecosystem.
We
evaluate
magnitude
this
potential
bias
using
a
spatially
unbiased
tree-ring
network
collected
USFS
Forest
Inventory
Analysis
(FIA)
program.
show
that
U.S.
Southwest
ITRDB
samples
overestimate
regional
sensitivity
41–59%,
because
sampled
at
warmer
drier
locations,
both
macro-
micro-site
scale,
systematically
older
compared
FIA
collection.
Although
there
uncertainties
associated
with
our
statistical
approach,
projection
based
suggests
29%
less
change-induced
decrease
climate-sensitive
samples.
Ecology Letters,
Journal Year:
2016,
Volume and Issue:
19(9), P. 1150 - 1158
Published: July 28, 2016
Abstract
The
impacts
of
climate
change
on
forest
net
biomass
are
poorly
understood
but
critical
for
predicting
forest's
contribution
to
the
global
carbon
cycle.
Recent
studies
show
change‐associated
declines
in
mature
plots.
representativeness
these
plots
regional
forests,
however,
remains
uncertain
because
we
lack
an
assessment
whether
differ
with
age.
Using
data
from
varying
ages
17
210
years,
monitored
1958
2011
western
Canada,
found
that
has
little
effect
forests
≤
40
years
age
due
increased
growth
offsetting
mortality,
led
large
decreases
older
mortality
accompanying
gain.
Our
analysis
highlights
need
incorporate
profiles
examining
past
and
projecting
future
responses
change.
Global Change Biology,
Journal Year:
2018,
Volume and Issue:
24(6), P. 2284 - 2304
Published: Feb. 26, 2018
Abstract
Increasing
tree
mortality
from
global
change
drivers
such
as
drought
and
biotic
infestations
is
a
widespread
phenomenon,
including
in
the
boreal
zone
where
climate
changes
feedbacks
to
Earth
system
are
relatively
large.
Despite
importance
for
science
management
communities,
our
ability
forecast
at
landscape
continental
scales
limited.
However,
two
independent
information
streams
have
potential
inform
improve
forecasts:
repeat
forest
inventories
satellite
remote
sensing.
Time
series
of
tree‐level
growth
patterns
indicate
that
productivity
declines
related
temporal
dynamics
often
precede
years
decades
before
death.
Plot‐level
productivity,
turn,
has
been
satellite‐based
indices
Normalized
difference
vegetation
index
(
NDVI
).
Here
we
link
these
data
sources
show
early
warning
signals
evident
several
‐based
metrics
up
24
We
focus
on
three
products
across
western
North
America
influenced
by
periodic
drought.
These
capture
range
conditions
spatial
resolution
highlight
sensitivity
limitations
approach.
Overall,
results
use
mortality.
Relationships
broadly
consistent
inventories,
species,
resolutions,
although
utility
coarse‐scale
imagery
heterogeneous
aspen
parkland
was
Longer‐term
annually
remeasured
sites
with
high
levels
generate
strongest
signals,
still
found
robust
relationships
typical
5
year
frequency.
The
approach
developed
here
can
be
used
basis
improving
models
monitoring
systems.
Nature Communications,
Journal Year:
2018,
Volume and Issue:
9(1)
Published: Dec. 4, 2018
Abstract
Northern
forests
at
the
leading
edge
of
their
distributions
may
not
show
increased
primary
productivity
under
climate
warming,
being
limited
by
climatic
extremes
such
as
drought.
Looking
beyond
tree
growth
to
underlying
physiological
mechanisms
is
fundamental
for
accurate
predictions
forest
responses
warming
and
drought
stress.
Within
a
32-year
genetic
field
trial,
we
analyze
relative
contributions
xylem
plasticity
inferred
stomatal
response
tolerance
in
regional
populations
widespread
conifer.
Genetic
adaptation
leads
varying
Trailing-edge
produce
fewer
tracheids
with
thicker
cell
walls,
characteristic
drought-tolerance.
Stomatal
explains
moderate
central
areas
species
range.
Growth
loss
northern
population
linked
low
responsiveness
combined
production
thinner
walls.
Forests
western
boreal
therefore
lack
adaptations
necessary
tolerate
drier
conditions.
Global Change Biology,
Journal Year:
2020,
Volume and Issue:
26(4), P. 2463 - 2476
Published: Jan. 22, 2020
The
response
of
forest
productivity
to
climate
extremes
strongly
depends
on
ambient
environmental
and
site
conditions.
To
better
understand
these
relationships
at
a
regional
scale,
we
used
nearly
800
observation
years
from
271
permanent
long-term
monitoring
plots
across
Switzerland,
obtained
between
1980
2017.
We
assimilated
data
into
the
3-PG
ecosystem
model
using
Bayesian
inference,
reducing
bias
predictions
14%
5%
for
stem
carbon
stocks
45%
9%
stock
changes.
then
estimated
forests
dominated
by
Picea
abies
Fagus
sylvatica
period
1960-2018,
tested
shifts
in
along
elevational
gradient
extreme
years.
Simulated
net
primary
(NPP)
decreased
with
elevation
(2.86
±
0.006
Mg
C
ha-1
year-1
km-1
P.
0.93
0.010
F.
sylvatica).
During
warm-dry
extremes,
simulated
NPP
both
species
increased
higher
lower
elevations,
reductions
more
than
25%
up
21%
potential
distribution
range
Switzerland.
Reduced
plant
water
availability
had
stronger
effect
temperature
during
extremes.
Importantly,
cold-dry
negative
impacts
comparable
Overall,
our
calibrated
suggests
that
is
complex
simple
shift
toward
elevation.
Such
robust
estimates
are
key
increasing
understanding
ecosystems
dynamics
under
Global Change Biology,
Journal Year:
2019,
Volume and Issue:
26(2), P. 901 - 918
Published: Sept. 17, 2019
Climate
extremes
such
as
heat
waves
and
droughts
are
projected
to
occur
more
frequently
with
increasing
temperature
an
intensified
hydrological
cycle.
It
is
important
understand
quantify
how
forest
carbon
fluxes
respond
drought
stress.
In
this
study,
we
developed
a
series
of
daily
indices
sensitivity
stress
indicated
by
air
(Ta
)
evaporative
fraction
(EF).
Using
normalized
from
the
FLUXNET
Network
for
34
sites
in
North
America,
seasonal
pattern
sensitivities
net
ecosystem
productivity
(NEP),
gross
(GEP)
respiration
(RE)
response
Ta
EF
anomalies
were
compared
different
types.
The
results
showed
that
warm
temperatures
spring
had
positive
effect
on
NEP
conifer
forests
but
negative
impact
deciduous
forests.
GEP
increased
higher
decreased
summer.
drought-induced
decrease
NEP,
which
mostly
occurred
forests,
was
driven
reduction
GEP.
similar
dampening
both
RE,
therefore
leading
neutral
response.
mean
annual
temperature.
Drier
less
sensitive
Natural
older
stand
age
tended
be
resilient
climate
stresses
managed
younger
Classification
Regression
Tree
analysis
seasons
most
powerful
variables
explaining
variation
Our
implied
magnitude
direction
flux
changes
highly
dependent
dynamics
timing
extremes.