Ecological Indicators,
Journal Year:
2024,
Volume and Issue:
158, P. 111511 - 111511
Published: Jan. 1, 2024
Arid
and
humid
ecosystems
are
undergoing
significant
changes
over
the
past
decades
due
to
warming
temperature
frequent
occurrence
of
climate
extremes.
Quantifying
climatic
vegetation
sensitivity
in
regions
with
different
classifications
is
crucial
for
understanding
interaction
mechanisms
between
ongoing
change.
However,
such
knowledge
about
spatiotemporal
variations
its
driving
factors
arid
still
unclear.
Based
on
this
consideration,
a
moving-window-based
Vegetation
Sensitivity
Index
(VSI)
scheme
was
applied
Enhanced
(EVI),
Leaf
Area
(LAI),
Solar-induced
Chlorophyll
Fluorescence
(GOSIF)
data
evaluate
terrestrial
ecosystem
response
explore
from
2003
2020.
Results
indicated
that
high
VSI
(>60)
observed
tropical
rainforests
central
Eurasia
semi-arid
regions.
By
contrast,
low
(<40)
typically
Spatially,
we
found
exhibited
nonlinear
parabolic
variation
along
gradient
aridity
index
but
generally
presented
linear
an
upward
trend
Temporally,
showed
declining
two
displayed
significantly
increasing
areas.
Temperature
dominant
factor
explain
spatial
globally,
while
precipitation
mainly
dominated
temporal
VSI.
The
varied
across
as
were
main
drive
classifications,
respectively.
Our
results
provide
unique
insights
into
future
change
classifications.
Global Change Biology,
Journal Year:
2023,
Volume and Issue:
29(11), P. 3072 - 3084
Published: March 1, 2023
Vegetation
response
to
soil
and
atmospheric
drought
has
raised
extensively
controversy,
however,
the
relative
contributions
of
drought,
their
compound
droughts
on
global
vegetation
growth
remain
unclear.
Combining
changes
in
moisture
(SM),
vapor
pressure
deficit
(VPD),
(normalized
difference
index
[NDVI])
during
1982-2015,
here
we
evaluated
trends
these
three
types
quantified
impacts
NDVI.
We
found
that
VPD
increased
0.22
±
0.05
kPa·decade-1
this
trend
was
doubled
after
1996
(0.32
0.16
)
than
before
(0.16
0.15
).
Regions
with
large
increase
generally
accompanied
decreasing
SM,
leading
a
widespread
increasing
across
37.62%
land
areas.
further
dominated
browning
since
late
1990s,
contributing
declined
NDVI
64.56%.
Earth
system
models
agree
dominant
role
growth,
but
negative
magnitudes
are
considerably
underestimated,
half
observed
results
(34.48%).
Our
provided
evidence
droughts-induced
browning,
highlighting
importance
correctly
simulating
ecosystem-scale
under-appreciated
exposure
as
it
will
climate
change.
National Science Review,
Journal Year:
2023,
Volume and Issue:
10(8)
Published: April 24, 2023
Despite
the
mounting
attention
being
paid
to
vegetation
growth
and
their
driving
forces
for
water-limited
ecosystems,
relative
contributions
of
atmospheric
soil
moisture
dryness
stress
on
are
an
ongoing
debate.
Here
we
comprehensively
compare
impacts
high
vapor
pressure
deficit
(VPD)
low
water
content
(SWC)
in
Eurasian
drylands
during
1982-2014.
The
analysis
indicates
a
gradual
decoupling
between
over
this
period,
as
former
has
expanded
faster
than
latter.
Moreover,
VPD-SWC
relation
VPD-greenness
both
non-linear,
while
SWC-greenness
is
near-linear.
loosened
coupling
VPD
SWC,
non-linear
correlations
among
VPD-SWC-greenness
area
extent
which
SWC
acts
dominant
factor
all
provide
compelling
evidence
that
more
influential
stressor
drylands.
In
addition,
set
11
Earth
system
models
projected
continuously
growing
constraint
towards
2100.
Our
results
vital
dryland
ecosystems
management
drought
mitigation
Eurasia.
Global Change Biology,
Journal Year:
2024,
Volume and Issue:
30(1)
Published: Jan. 1, 2024
Abstract
Droughts
have
been
implicated
as
the
main
driver
behind
recent
vegetation
die‐off
and
are
projected
to
drive
greater
mortality
under
future
climate
change.
Understanding
coupling
relationship
between
drought
has
of
great
global
interest.
Currently,
is
mainly
evaluated
by
correlation
coefficients
or
regression
slopes.
However,
optimal
timescale
response
drought,
a
key
indicator
reflecting
sensitivity
largely
ignored.
Here,
we
apply
identification
method
examine
change
in
over
past
three
decades
(1982–2015)
with
long‐term
satellite‐derived
Normalized
Difference
Vegetation
Index
Standardized
Precipitation‐Evapotranspiration
data.
We
find
substantial
increasing
timescales
globally,
coefficient
overall
declines
1982
2015.
This
decrease
vegetation–drought
observed
regions
water
deficit,
although
its
initial
relatively
high.
water‐surplus
regions,
low
earlier
stages,
prone
show
an
trend.
The
changes
may
be
driven
trend
atmospheric
CO
2
.
Our
findings
highlight
more
pressing
risk
than
water‐deficit
which
advances
our
understanding
provides
essential
insights
for
mapping
changing
conditions.
Nature Communications,
Journal Year:
2025,
Volume and Issue:
16(1)
Published: Jan. 21, 2025
Precipitation
is
an
important
factor
influencing
the
date
of
foliar
senescence,
which
in
turn
affects
carbon
uptake
terrestrial
ecosystems.
However,
temporal
patterns
precipitation
frequency
and
its
impact
on
senescence
remain
largely
unknown.
Using
both
long-term
flux
data
satellite
observations
across
Northern
Hemisphere,
we
show
that,
after
excluding
impacts
from
temperature,
radiation
total
by
partial
correlation
analysis,
declining
may
drive
earlier
1982
to
2022.
A
decrease
intensifies
drought
stress
reducing
root-zone
soil
moisture
increasing
atmospheric
dryness,
limit
photosynthesis
necessary
for
sustained
growth.
The
enhanced
acclimation,
showing
a
more
rapid
response
drought,
also
explains
positive
relationship
between
date.
Finally,
find
30
current
state-of-art
Earth
system
models
fail
capture
sensitivity
DFS
changes
incorrectly
predict
direction
correlations
approximately
half
northern
global
lands,
historical
simulations
future
predictions.
Our
results
therefore
highlight
critical
need
include
frequency,
rather
than
just
precipitation,
into
accurately
forecast
plant
phenology
under
climate
change.
leaf
senescence.
Here,
authors
use
demonstrate
that
reduced
associated
with
faster
trees
don't
precipitation.
Engineering,
Journal Year:
2023,
Volume and Issue:
34, P. 109 - 119
Published: Sept. 14, 2023
Globally,
vegetation
has
been
changing
dramatically.
The
vegetation–water
dynamic
is
key
to
understanding
ecosystem
structure
and
functioning
in
water-limited
ecosystems.
Continual
satellite
monitoring
detected
global
greening.
However,
a
greenness
increase
does
not
mean
that
functions
increase.
intricate
interplays
resulting
from
the
relationships
between
precipitation
must
be
more
adequately
comprehended.
In
this
study,
data,
for
example,
leaf
area
index
(LAI),
net
primary
production
(NPP)
rainfall
use
efficiency
(RUE),
were
used
quantify
dynamics
their
relationship
with
different
reaches
of
Yellow
River
Basin
(YRB).
A
sequential
regression
method
was
detect
trends
NPP
sensitivity
rainfall.
results
showed
34.53%
YRB
exhibited
significant
greening
trend
since
2000.
Among
them,
20.54%,
53.37%,
16.73%
upper,
middle,
lower
reach
areas
positive
trend,
respectively.
similar
LAI
reaches.
notable
difference
noted
distributions
RUE
across
Moreover,
there
vegetation–rainfall
16.86%
YRB's
middle
reaches—14.08%
negative
2.78%
trends.
total
8.41%
marked
LAI,
NPP,
RUE.
Subsequently,
strategic
locations
reliant
on
correlation
identified
designated
restoration
planning
purposes
propose
future
ecological
efforts.
Our
analysis
indicates
most
variation
productivity.
present
study
underscores
significance
examining
within
context
high-quality
development
strategy
YRB.
outcomes
our
proposed
framework
can
provide
decision-makers
valuable
insights
executing
rational
basin
pattern
optimization
sustainable
management.