Ecosphere,
Journal Year:
2017,
Volume and Issue:
8(7)
Published: July 1, 2017
Abstract
Forests
around
the
world
are
experiencing
increasingly
severe
droughts
and
elevated
competitive
intensity
due
to
increased
tree
density.
However,
influence
of
interactions
between
drought
competition
on
forest
growth
remains
poorly
understood.
Using
a
unique
dataset
stand‐scale
dendrochronology
sampled
from
6405
trees,
we
quantified
how
annual
entire
populations
responds
in
eight,
long‐term
(multi‐decadal),
experiments
with
replicated
levels
density
(e.g.,
intensity)
arrayed
across
broad
climatic
compositional
gradient.
Forest
(cumulative
individual
within
stand)
declined
during
drought,
especially
more
drier
climates.
declines
were
exacerbated
by
high
at
all
sites
but
one,
particularly
periods
drought.
Surprisingly,
was
persistent
overall,
these
impacts
greater
humid
than
arid
sites.
Significant
occurred
extreme
warmer
temperatures
semi‐arid
cooler
Because
has
consistent
over
response
maintaining
forests
lower
may
enhance
resilience
Science,
Journal Year:
2020,
Volume and Issue:
368(6488), P. 261 - 266
Published: April 16, 2020
Trees
are
the
living
foundations
on
which
most
terrestrial
biodiversity
is
built.
Central
to
success
of
trees
their
woody
bodies,
connect
elevated
photosynthetic
canopies
with
essential
belowground
activities
water
and
nutrient
acquisition.
The
slow
construction
these
carbon-dense,
skeletons
leads
a
generation
time,
leaving
forests
highly
susceptible
rapid
changes
in
climate.
Other
long-lived,
sessile
organisms
such
as
corals
appear
be
poorly
equipped
survive
changes,
raises
questions
about
vulnerability
contemporary
future
climate
change.
emerging
view
that,
similar
corals,
tree
species
have
rather
inflexible
damage
thresholds,
particularly
terms
stress,
especially
concerning.
This
Review
examines
recent
progress
our
understanding
how
looks
for
growing
hotter
drier
atmosphere.
Fire Ecology,
Journal Year:
2020,
Volume and Issue:
16(1)
Published: Jan. 27, 2020
Abstract
Background
Wildfires
in
the
Pacific
Northwest
(Washington,
Oregon,
Idaho,
and
western
Montana,
USA)
have
been
immense
recent
years,
capturing
attention
of
resource
managers,
fire
scientists,
general
public.
This
paper
synthesizes
understanding
potential
effects
changing
climate
regimes
on
forests,
including
disturbance
stress
interactions,
forest
structure
composition,
post-fire
ecological
processes.
We
frame
this
information
a
risk
assessment
context,
conclude
with
management
implications
future
research
needs.
Results
Large
severe
fires
are
associated
warm
dry
conditions,
such
conditions
will
likely
occur
increasing
frequency
warming
climate.
According
to
projections
based
historical
records,
current
trends,
simulation
modeling,
protracted
warmer
drier
drive
lower
fuel
moisture
longer
seasons
future,
extent
compared
twentieth
century.
Interactions
between
other
disturbances,
as
drought
insect
outbreaks,
be
primary
drivers
ecosystem
change
Reburns
also
more
frequently
drought,
tree
regeneration
species
composition.
Hotter,
sites
may
particularly
at
for
failures.
Conclusion
Resource
managers
unable
affect
total
area
burned
by
fire,
trend
is
driven
strongly
However,
treatments,
when
implemented
spatially
strategic
manner,
can
help
decrease
intensity
severity
improve
resilience
insects,
drought.
Where
treatments
less
effective
(wetter,
high-elevation,
coastal
forests),
consider
implementing
breaks
around
high-value
resources.
When
where
planting
an
option,
different
genetic
stock
than
has
used
past
increase
seedling
survival.
Planting
seedlings
cooler,
wetter
microsites
In
driest
topographic
locations,
need
they
try
forestall
allow
conversions
vegetation
what
currently
dominant.
BioScience,
Journal Year:
2017,
Volume and Issue:
68(2), P. 77 - 88
Published: Nov. 20, 2017
Massive
tree
mortality
has
occurred
rapidly
in
frequent-fire-adapted
forests
of
the
Sierra
Nevada,
California.
This
is
a
product
acute
drought
compounded
by
long-established
removal
key
ecosystem
process:
frequent,
low-
to
moderate-intensity
fire.
The
recent
many
implications
for
future
these
and
ecological
goods
services
they
provide
society.
Future
wildfire
hazard
following
this
can
be
generally
characterized
decreased
crown
fire
potential
increased
surface
intensity
short
intermediate
term.
scale
present
so
large
that
greater
"mass
fire"
exists
coming
decades,
driven
amount
continuity
dry,
combustible,
woody
material
could
produce
large,
severe
fires.
For
long-term
adaptation
climate
change,
we
highlight
importance
moving
beyond
triage
dead
dying
trees
making
"green"
(live)
more
resilient.
Global Change Biology,
Journal Year:
2017,
Volume and Issue:
23(9), P. 3742 - 3757
Published: Jan. 30, 2017
Abstract
Ongoing
climate
change
poses
significant
threats
to
plant
function
and
distribution.
Increased
temperatures
altered
precipitation
regimes
amplify
drought
frequency
intensity,
elevating
stress
mortality.
Large‐scale
forest
mortality
events
will
have
far‐reaching
impacts
on
carbon
hydrological
cycling,
biodiversity,
ecosystem
services.
However,
biogeographical
theory
global
vegetation
models
poorly
represent
recent
die‐off
patterns.
Furthermore,
as
trees
are
sessile
long‐lived,
their
responses
extremes
substantially
dependent
historical
factors.
We
show
that
periods
of
favourable
climatic
management
conditions
facilitate
abundant
tree
growth
can
lead
structural
overshoot
aboveground
biomass
due
a
subsequent
temporal
mismatch
between
water
demand
availability.
When
environmental
favourability
declines,
increases
in
temperature
protracted,
rapid,
or
both,
drive
gradient
modify
self‐thinning
relationships.
Responses
ranging
from
premature
leaf
senescence
partial
canopy
dieback
whole‐tree
reduce
area
during
the
period
for
lagged
recovery
window
thereafter.
Such
mismatches
requirements
availability
occur
at
local
regional
scales
throughout
species
geographical
range.
As
projections
predict
large
future
fluctuations
both
wet
dry
conditions,
we
expect
forests
become
increasingly
structurally
mismatched
thus
overbuilt
more
stressful
episodes.
By
accounting
context
development,
our
approach
explain
previously
problematic
aspects
large‐scale
mortality,
such
why
it
range
yet
still
be
locally
highly
variable,
some
seem
readily
attributable
an
ongoing
while
others
do
not.
This
refined
understanding
better
responses,
enabling
improved
prediction
changes
distribution
scales.
Nature Communications,
Journal Year:
2019,
Volume and Issue:
10(1)
Published: Sept. 26, 2019
Forest
mortality
is
accelerating
due
to
climate
change
and
the
largest
trees
may
be
at
greatest
risk,
threatening
critical
ecological,
economic,
social
benefits.
Here,
we
combine
high-resolution
airborne
LiDAR
optical
data
track
tree-level
rates
for
~2
million
in
California
over
8
years,
showing
that
tree
height
strongest
predictor
of
during
extreme
drought.
Large
die
twice
rate
small
environmental
gradients
temperature,
water,
competition
control
intensity
height-mortality
relationship.
These
findings
suggest
future
persistent
drought
cause
widespread
on
Earth.
Journal of Water Resources Planning and Management,
Journal Year:
2018,
Volume and Issue:
144(10)
Published: July 31, 2018
California’s
5-year
drought
has
ended,
even
as
its
aftermath
lingers.
From
2012–2016
much
or
all
of
California
was
under
severe
conditions,
with
greatly
diminished
precipitation,
snowpack,
and
streamflow
higher
temperatures.
Water
shortages
to
forests,
aquatic
ecosystems,
hydroelectric
power
plants,
rural
drinking
water
supplies,
agriculture,
cities
caused
billions
dollars
in
economic
losses,
killed
millions
forest
trees,
brought
several
fish
species
closer
extinction,
inconvenience
some
expense
households
businesses.
The
also
innovations
improvements
management,
which
will
better
prepare
for
future
droughts.
This
paper
summarizes
the
magnitude
impacts
drought.
then
reviews
arising
from
larger
historical
context
management
California.
Lessons
modern
are
discussed.
Droughts
modern,
well-managed
systems
serving
globalized
economies
need
not
be
economically
catastrophic,
but
always
have
challenges,
particularly
native
ecosystems.
In
every
other
system,
droughts
usefully
expose
weaknesses
inadequate
preparation
management.
this
regard
California,
managers
ecosystems
small
supplies
had
most
learn.
Frontiers in Ecology and Evolution,
Journal Year:
2019,
Volume and Issue:
7
Published: July 10, 2019
Resilience
and
resistance
concepts
have
broad
application
to
ecology
society.
is
an
emergent
property
that
reflects
the
amount
of
disruption
a
system
can
withstand
before
its
structure
or
organization
uncharacteristically
shift.
Resistance
component
resilience.
Before
advent
intensive
forest
management
fire
suppression,
western
North
American
forests
exhibited
naturally
occurring
resilience
wildfires
other
disturbances.
Using
evidence
from
ten
ecoregions,
spanning
Canada
Mexico,
we
review
properties
these
reinforced
those
qualities.
We
show
examples
multi-level
landscape
resilience,
feedbacks
within
among
levels,
how
conditions
changed
under
climatic
influences.
highlight
geographic
similarities
differences
in
historical
landscapes,
their
types,
abrupt
large-scale
disruptions.
discuss
regional
climates’
role
episodically
abruptly
reorganizing
plant
animal
biogeography,
give
clear
changes
suggest
managing
for
resilient
construct
strongly
dependent
on
scale
social
values.
It
involves
human
community
adaptations
work
with
ecosystems
they
depend
processes
shape
them.
entails
actively
factors
exploiting
mechanisms
drive
dynamics
at
each
level
as
means
adapting
species,
communities
climate
change,
maintaining
core
ecosystem
functions,
processes,
services.
Finally,
it
compels
us
prioritize
incorporates
ongoing
disturbances
anticipated
effects
changes,
support
dynamically
shifting
patchworks
nonforest.
Doing
so
will
make
wildfire
regimes
more
gradual
less
disruptive
individuals
Ecological Applications,
Journal Year:
2021,
Volume and Issue:
31(8)
Published: Aug. 2, 2021
Implementation
of
wildfire-
and
climate-adaptation
strategies
in
seasonally
dry
forests
western
North
America
is
impeded
by
numerous
constraints
uncertainties.
After
more
than
a
century
resource
land
use
change,
some
question
the
need
for
proactive
management,
particularly
given
novel
social,
ecological,
climatic
conditions.
To
address
this
question,
we
first
provide
framework
assessing
changes
landscape
conditions
fire
regimes.
Using
framework,
then
evaluate
evidence
change
contemporary
relative
to
those
maintained
active
regimes,
i.e.,
uninterrupted
or
human-induced
exclusion.
The
cumulative
results
research
document
persistent
substantial
deficit
widespread
alterations
ecological
structures
functions.
These
are
not
necessarily
apparent
at
all
spatial
scales
dimensions
regimes
forest
nonforest
Nonetheless,
loss
once
abundant
influence
low-
moderate-severity
fires
suggests
that
even
least
fire-prone
ecosystems
may
be
affected
alteration
surrounding
and,
consequently,
ecosystem
Vegetation
patterns
fire-excluded
forested
landscapes
no
longer
reflect
heterogeneity
interacting
Live
dead
vegetation
(surface
canopy
fuels)
generally
continuous
before
European
colonization.
As
result,
current
vulnerable
direct
indirect
effects
seasonal
episodic
increases
drought
fire,
especially
under
rapidly
warming
climate.
Long-term
exclusion
contemporaneous
social-ecological
influences
continue
extensively
modify
landscapes.
Management
realigns
adapts
can
moderate
transitions
as
human
communities
adapt
changing
disturbance
adaptation
developed,
evaluated,
implemented,
objective
scientific
evaluation
ongoing
monitoring
aid
differentiation
warranted
unwarranted
Scientific Data,
Journal Year:
2018,
Volume and Issue:
5(1)
Published: May 22, 2018
Abstract
Hydroclimate
extremes
critically
affect
human
and
natural
systems,
but
there
remain
many
unanswered
questions
about
their
causes
how
to
interpret
dynamics
in
the
past
climate
change
projections.
These
uncertainties
are
due,
part,
lack
of
long-term,
spatially
resolved
hydroclimate
reconstructions
information
on
underlying
physical
drivers
for
regions.
Here
we
present
first
global
associated
dynamical
variables
over
two
thousand
years.
We
use
a
data
assimilation
approach
tailored
reconstruct
that
optimally
combines
2,978
paleoclimate
proxy-data
time
series
with
constraints
an
atmosphere—ocean
model.
The
annually
or
seasonally
include
spatiotemporal
drought
indices,
near-surface
air
temperature,
index
North
Atlantic
variability,
location
intertropical
convergence
zone,
monthly
Niño
indices.
This
database,
called
Paleo
Hydrodynamics
Data
Assimilation
product
(PHYDA),
will
provide
critical
new
platform
investigating
variability
extremes,
while
informing
interpretations
future