Ecology,
Journal Year:
2023,
Volume and Issue:
104(4)
Published: Feb. 17, 2023
Abstract
Drought
events
are
projected
to
be
more
extreme
and
frequent
in
the
future
have
profound
influences
on
structure
functions
of
terrestrial
ecosystems.
Thus,
better
understanding
mechanisms
recovery
is
critical
for
predicting
dynamics
We
performed
a
7‐year
field
precipitation
experiment
examine
grassland
ecosystem
from
different
magnitudes
sustained
drought,
slight
extreme.
The
was
exposed
treatments
first
3
years
(2010–2012)
recovered
during
last
4
(2013–2016)
without
treatments.
Overall,
large
reductions
aboveground
net
primary
productivity
(ANPP,
−43.3%)
perennial
forb
biomass
(−83.1%)
were
observed
third
year
(2012)
drought
only.
Nevertheless,
ANPP
fully
within
1
after
terminated,
rapid
mainly
due
increased
soil
total
nitrogen
root
allocation
drought.
Surprisingly,
increases
under
treatment
occurred
periods
2013
2015
(+74.1,
+88.5,
+119.8
g
m
−2
−1
)
compared
control.
overcompensation
offset
drought‐induced
reduction
primarily
ascribed
enhanced
grasses
(PG).
Higher
resistance
fast
resource
acquisition
strategy
might
drive
expansion
PG.
Our
findings
revealed
grasslands
role
community
maintaining
function
stability
climate
change
scenarios.
Global Change Biology,
Journal Year:
2021,
Volume and Issue:
27(19), P. 4630 - 4643
Published: July 6, 2021
Abstract
Understanding
vegetation
recovery
after
drought
is
critical
for
projecting
dynamics
in
future
climates.
From
1997
to
2009,
Australia
experienced
a
long‐lasting
known
as
the
Millennium
Drought
(MD),
which
led
widespread
reductions
productivity.
However,
post‐drought
and
its
determinants
remain
unclear.
This
study
leverages
remote
sensing
products
from
different
sources—fraction
of
absorbed
photosynthetically
active
radiation
(FPAR),
based
on
optical
data,
canopy
density,
derived
microwave
data—and
random
forest
algorithms
assess
over
Australian
natural
during
20‐year
period
centered
MD.
Post‐drought
was
prevalent
across
continent,
with
6
out
10
events
seeing
full
within
about
months.
Canopy
density
slower
recover
than
leaf
area
seen
FPAR.
The
probability
most
strongly
controlled
by
return
interval,
hydrological
condition,
length.
Full
seldom
observed
when
occurred
at
intervals
3
months
or
less,
moderately
dry
(standardized
water
balance
anomaly
[SWBA]
[−1,
−0.76])
conditions
resulted
less
complete
wet
(SWBA
>
0.3)
conditions.
Press
droughts,
are
long
term
but
not
extreme,
delayed
more
pulse
droughts
(short
extreme)
higher
frequency
persistent
decline.
Following
press
decline
differed
little
among
biome
types
peaked
semi‐arid
regions
aridity
levels.
Forests
savanna
required
longest
times
drought,
while
grasslands
were
slowest
drought.
provides
quantitative
thresholds
that
could
be
used
improve
modeling
ecosystem
post‐drought.
Earth System Dynamics,
Journal Year:
2021,
Volume and Issue:
12(4), P. 1015 - 1035
Published: Oct. 15, 2021
Abstract.
In
2018
and
2019,
central
Europe
was
affected
by
two
consecutive
extreme
dry
hot
summers
(DH18
DH19).
The
DH18
event
had
severe
impacts
on
ecosystems
likely
vegetation
activity
in
the
subsequent
year,
for
example
through
depletion
of
carbon
reserves
or
damage
from
drought.
Such
legacies
drought
heat
stress
can
further
increase
susceptibility
to
additional
hazards.
Temporally
compound
extremes
such
as
DH19
can,
therefore,
result
an
amplification
due
preconditioning
effects
past
disturbance
legacies.
Here,
we
evaluate
how
these
impacted
responses
first
(DH18)
modulated
second
(DH19).
To
quantify
changes
vulnerability
each
event,
train
a
set
statistical
models
period
2001–2017,
which
are
then
used
predict
enhanced
index
(EVI)
anomalies
MODIS.
These
estimates
correspond
expected
EVI
based
sensitivity
climate.
Large
departures
predicted
values
indicate
conditions
be
identify
modulating
composition
other
environmental
factors
observed
impacts.
We
find
regions
(DH)
events
were
significantly
stronger
than
those
previous
climate–vegetation
relationships.
One
region,
largely
dominated
grasslands
crops,
showed
much
both
DH
their
drought,
possibly
linked
changing
background
CO2
temperature
conditions.
A
forests
grasslands,
browning
DH19,
even
though
partly
alleviated
2019.
This
trajectory
mainly
explained
role
interannual
legacy
increased
biotic
disturbances,
also
promoted
warm
Dry
become
more
frequent
coming
decades,
posing
major
threat
stability
European
forests.
show
that
state-of-the-art
process-based
could
not
represent
decline
response
because
they
missed
gaps
may
overestimation
resilience
temperate
future
model
projections.
Current Forestry Reports,
Journal Year:
2021,
Volume and Issue:
7(2), P. 69 - 80
Published: Feb. 27, 2021
Abstract
Purpose
of
Review
Society
is
concerned
about
the
long-term
condition
forests.
Although
a
clear
definition
forest
health
still
missing,
to
evaluate
health,
monitoring
efforts
in
past
40
years
have
concentrated
on
assessment
tree
vitality,
trying
estimate
photosynthesis
rates
and
productivity.
Used
decline
Central
Europe
since
1980s,
crown
foliage
transparency
has
been
commonly
believed
be
best
indicator
relation
air
pollution,
although
annual
variations
appear
more
closely
related
water
stress.
not
good
rates,
defoliation
one
most
used
indicators
vitality.
Tree
rings
often
as
However,
growth
trends
are
difficult
interpret
because
sampling
bias,
ring
width
patterns
do
provide
any
information
physiological
processes.
Recent
Findings
In
two
decades,
tree-ring
stable
isotopes
only
reconstruct
impact
climatic
events,
such
drought,
but
also
study
induced
by
pollution
episodes,
other
natural
disturbances
environmental
stress,
pest
outbreaks
wildfires.
They
proven
useful
tools
for
understanding
processes
response
stress
factors.
Summary
Tree-ring
integrate
transpiration
may
enhance
our
promising
We
call
use
future
programmes.
Functional Ecology,
Journal Year:
2021,
Volume and Issue:
36(1), P. 4 - 23
Published: Oct. 30, 2021
Abstract
With
ongoing
climate
change,
the
probability
of
crossing
environmental
thresholds
promoting
abrupt
changes
in
ecosystem
structure
and
functioning
is
higher
than
ever.
In
drylands
(areas
where
it
rains
<65%
what
could
be
potentially
evaporated),
recent
research
has
shown
how
three
aridity
[at
(1‐Aridity
Index)
values
0.54,
0.70
0.80]
leads
to
on
structural
functional
attributes.
Despite
importance
these
findings
their
implications
develop
effective
monitoring
adaptation
actions
combat
change
desertification,
we
lack
a
proper
understanding
mechanisms
unleashing
shifts.
Here
review
multiple
that
may
explain
existence
observed
across
global
drylands,
discuss
potential
amplification
underpin
hypothetical
temporal
shifts
with
change.
We
propose
each
threshold
caused
by
different
specific
mechanisms.
The
first
mainly
physiological
plant
water
shortages.
second
unleashed
involving
soil
processes
plant–soil
interactions
such
as
erosion,
community
nutrient
cycling
circulation.
collapse
vegetation
once
third
(0.8)
crossed
related
survival
limits
plants
cause
sudden
cover
diversity
losses
plant–atmospheric
feedbacks
link
further
aridification.
By
identifying,
revising
linking
relevant
observed,
provide
set
hypotheses
identify
knowledge
gaps
concerning
study
emergence
drylands.
were
also
able
establish
plausible
factors
are
context
dependent
influence
occurrence
time.
Our
help
focus
future
efforts
strategies
monitor,
adapt
or
even
revert
A
free
Plain
Language
Summary
can
found
within
Supporting
Information
this
article.
Ecological Indicators,
Journal Year:
2021,
Volume and Issue:
130, P. 108146 - 108146
Published: Aug. 26, 2021
Drought
is
the
most
widespread
event
under
climate
change
and
projected
to
lead
high
uncertainties
in
quantifying
terrestrial
carbon
exchange.
However,
considering
complexity
of
drought
quantification
differences
physiological
responses
among
different
vegetation
types,
potential
mechanisms
response
across
regions
their
at
varying
time
scales
remain
unclear
globally.
Here,
we
analyzed
activity
determined
scale
dominating
drought-induced
variations,
then
explored
its
driving
factors
(temperature,
precipitation,
evapotranspiration,
water
balance)
climatic
conditions
types
from
2000
2015
using
Standardized
Precipitation
Evapotranspiration
Index
(SPEI)
Net
Primary
Productivity
(NPP).
Our
results
indicated
that
NPP-SPEI
correlation
was
stronger
arid
semi-arid
compared
humid
sub-humid
zones
Vegetation
mainly
responded
short
medium
shortest
observed
for
deciduous
needle-leaf
forests
closed
shrublands,
which
located
southeastern
Australia,
central
Africa,
southern
Russia.
Moreover,
grassland
cropland
ecosystems
were
found
be
also
highly
vulnerable
globe.
Analysis
effects
various
meteorological
on
timescales
showed
balance
predominant
factor
affecting
drought.
In
particular,
increase
significantly
reduced
intensity
prolonged
timescales.
time-scales
reduces
prolongs
time-scales.
Therefore,
identification
dominant
mostly
impact
land
biomes
assist
assessing
stability
ecosystem
thus
support
mitigation
reduce
degradation.
Journal of Ecology,
Journal Year:
2021,
Volume and Issue:
109(9), P. 3157 - 3170
Published: Jan. 17, 2021
Abstract
Understanding
the
impacts
of
extreme
drought
on
forest
productivity
requires
a
comprehensive
assessment
tree
and
resilience.
However,
current
approaches
to
quantifying
resilience
limit
our
understanding
response
dynamics,
recovery
trajectories
legacies
by
constraining
temporal
scale
resolution
assessment.
We
compared
individual
growth
histories
with
forecasted
using
dynamic
regression
at
an
annual
resolution,
allowing
impact
stand
level
dynamics
be
assessed
relative
scenario
where
no
occurred.
The
novel
application
this
approach
allowed
us
quantify
cumulative
legacy
radial
multiple
stem
heights
different
densities.
show
that
choice
pre‐
post‐drought
periods
over
which
is
can
lead
systematic
bias
in
both
estimates
interpretations
indices.
In
contrast,
measuring
annually
revealed
clear
nonlinearities
trajectories.
Furthermore,
we
demonstrate
influence
pre‐drought
attributes
such
as
size,
rates
densities
were
only
detectable
certain
stages
recovery.
Importantly,
become
positive
for
some
individuals,
extending
up
9
years
after
event
post‐recovery
result
reclamation
lost
basal
area.
Synthesis
.
importance
increasing
order
understand
patterns
drivers
highlight
shortcomings
collapsing
into
single
average
value
how
persist
phase,
even
positively
impacting
trees.
If
unaccounted
for,
phase
underestimation
overestimation
above‐ground
losses
productivity,
highlighting
considering
longer‐term
compensatory
Global Change Biology,
Journal Year:
2022,
Volume and Issue:
28(9), P. 2956 - 2978
Published: Feb. 19, 2022
Extreme
events
such
as
the
summer
drought
of
2018
in
Central
Europe
are
projected
to
occur
more
frequently
future
and
may
cause
major
damages
including
increased
tree
mortality
negative
impacts
on
forest
ecosystem
services.
Here,
we
quantify
response
>1
million
pixels
10
×
m
across
Switzerland
terms
resistance,
recovery,
resilience.
We
used
Normalized
Difference
Water
Index
(NDWI)
derived
from
Sentinel-2
satellite
data
a
proxy
for
canopy
water
content
analyzed
its
relative
change.
calculated
NDWI
change
between
2017
pre-drought
years
(indicating
resistance),
2019
post-drought
recovery),
2017-2019
resilience).
Analyzing
this
large
natural
experiment,
found
that
4.3%
Swiss
declined
2018,
indicating
areas
with
low
resistance
effects.
While
roughly
50%
area
recovered,
2.7%
forested
continued
decline
2019,
suggesting
prolonged
effects
or
delayed
damage.
differential
responses
associated
site
topographic
characteristics
stand
characteristics,
lesser
extent
climatic
conditions
interactions
these
drivers.
Low
high
recovery
were
most
prominent
at
edges,
but
also
south-facing
slopes
lower
elevations.
Tree
functional
type
was
important
driver
resilience,
damage
stands
conifer
abundance.
Our
results
demonstrate
suitability
satellite-based
quantification
drought-induced
spatial
resolution
areas.
Such
information
is
predict
how
local
impact
vulnerability
extreme
help
search
appropriate
adaptation
strategies.
New Phytologist,
Journal Year:
2022,
Volume and Issue:
235(2), P. 420 - 431
Published: April 4, 2022
Drought
is
intensifying
globally
with
climate
change,
creating
an
urgency
to
understand
ecosystem
response
drought
both
during
and
after
these
events
end
limit
loss
of
functioning.
The
literature
replete
studies
how
ecosystems
respond
drought,
yet
there
are
far
fewer
focused
on
dynamics
ends.
Furthermore,
while
the
terms
used
describe
can
be
variable
inconsistent,
so
those
that
responses
following
drought.
With
this
review,
we
sought
evaluate
create
clear
definitions
ecologists
use
post-drought
responses.
We
found
legacy
effects,
resilience
recovery
were
most
commonly
respect
responses,
but
variable.
Based
our
review
literature,
propose
a
framework
for
generalizing
ends,
which
refer
as
'the
period'.
suggest
future
papers
need
clearly
characteristics
imposed
encourage
authors
term
period
general
encompasses
ends
other
more
specific
descriptors
period.
New Phytologist,
Journal Year:
2022,
Volume and Issue:
237(5), P. 1508 - 1524
Published: Nov. 14, 2022
Summary
The
physiological
challenges
posed
by
climate
change
for
seasonal,
perennial
plants
include
increased
risk
of
heat
waves,
postbudbreak
freezing
(‘false
springs’),
and
droughts.
Although
considerable
work
has
shown
that
the
traits
conferring
tolerance
to
these
stressors
–
thermotolerance,
cold
hardiness,
water
deficit
stress,
respectively
are
not
static
in
time,
they
frequently
treated
as
such.
In
this
review,
I
synthesize
recent
literature
on
predictable
seasonal
therefore,
phenological
patterns
acclimation
deacclimation
heat,
cold,
water‐deficit
stress
perennials,
focusing
woody
native
temperate
climates.
highlight
promising,
high‐throughput
techniques
quantifying
drought
tolerance.
For
each
forms
tolerance,
summarize
current
balance
evidence
regarding
temporal
over
course
a
year
suggest
characteristic
scale
responses
environmental
stress.
doing
so,
offer
synthetic
framework
‘phenological
physiology’,
which
understanding
leveraging
seasonally
recurring
(phenological)
can
facilitate
adaptation
mitigation.
Plant Biology,
Journal Year:
2022,
Volume and Issue:
24(7), P. 1186 - 1197
Published: July 23, 2022
The
occurrence
of
hot
drought,
i.e.
low
water
availability
and
simultaneous
high
air
temperature,
represents
a
severe
threat
to
ecosystems.
Here,
we
investigated
how
the
2018
drought
in
Central
Europe
caused
tipping
point
tree
ecosystem
functioning
Scots
pine
(Pinus
sylvestris
L.)
forest
southwest
Germany.
Measurements
stress
indicators,
such
as
needle
potential,
carbon
assimilation
volatile
organic
compound
(VOC)
emissions,
dominant
P.
trees
were
deployed
evaluate
during
drought.
Ecosystem
impact
recovery
assessed
exchange,
normalized
difference
vegetation
index
(NDVI)
from
satellite
data
mortality
data.
During
summer
2018,
potentials
dropped
minimum
values
-7.5
±
0.2
MPa,
which
implied
hydraulic
impairment
sylvestris.
Likewise,
VOC
emissions
strongly
declined
after
mid-July.
Decreasing
NDVI
August
onwards
detected,
along
with
defoliation
sylvestris,
impairing
flux
2019,
shifting
into
year-round
source.
A
total
47%
all
monitored
(n
=
368)
died
by
September
2020.
recovered
pre-2018
levels
likely
emerging
broadleaved
understorey
species.
had
negative
impacts
on
co-occurrence
unfavourable
site-specific
conditions
recurrent
droughts
resulted
accelerated
mortality.
Thus,
pushed
stand
towards
its
point,
subsequent
shift
broadleaf-dominated
forest.