Water Resources Research,
Journal Year:
2021,
Volume and Issue:
57(10)
Published: Sept. 21, 2021
Abstract
Forests
modify
snow
accumulation
and
ablation
rates
as
well
overall
storage
amounts
durations,
with
multiple
processes
acting
simultaneously
often
in
different
directions.
To
synthesize
complex
forest–snow
relations
help
guide
near‐term
management
decisions,
we
present
a
decision
tree.
The
framework
is
based
on
hypothesized
hierarchy
of
associated
variables
that
predict
forest
effects
storage.
In
locations
high
wind
speeds,
forests
enhance
magnitude
duration
relative
to
open
areas.
Where
speeds
are
low,
winter
spring
air
temperatures
colder,
diminish
but
duration.
warmer,
both
Forest
structure
aspect
secondary
influences.
We
apply
the
tree
map
influence
under
historic
climate
conditions
across
western
United
States,
this
applicable
any
region
snow.
This
provides
practitioners
first‐step
evaluation
decisions
consider
where
how
can
be
managed
optimize
situ
water
alongside
other
objectives,
such
reducing
wildfire
hazard.
also
articulates
geospatial
hypotheses,
order
anticipated
importance,
tested
future
investigations
forest–snow–climate
relations.
Proceedings of the National Academy of Sciences,
Journal Year:
2022,
Volume and Issue:
119(10)
Published: Feb. 22, 2022
Streamflow
often
increases
after
fire,
but
the
persistence
of
this
effect
and
its
importance
to
present
future
regional
water
resources
are
unclear.
This
paper
addresses
these
knowledge
gaps
for
western
United
States
(WUS),
where
annual
forest
fire
area
increased
by
more
than
1,100%
during
1984
2020.
Among
72
forested
basins
across
WUS
that
burned
between
2019,
multibasin
mean
streamflow
was
significantly
elevated
0.19
SDs
(P
<
0.01)
an
average
6
years
postfire,
compared
range
results
expected
from
climate
alone.
Significance
is
assessed
comparing
prefire
postfire
responses
also
among
107
control
experienced
little
no
wildfire
study
period.
The
response
scales
with
extent:
29
>20%
in
a
year,
over
first
0.38
SDs,
or
30%.
Postfire
were
significant
all
four
seasons.
Historical
fire-climate
relationships
combined
model
projections
suggest
2021
2050
will
see
repeated
when
fire-conducive
2020,
year
currently
holding
modern
record
burned.
These
findings
center
on
relatively
small,
minimally
managed
basins,
our
areas
grow
enough
next
3
decades
enhance
at
scales.
Wildfire
emerging
driver
runoff
change
increasingly
alter
impacts
supplies
runoff-related
risks.
Forest Ecology and Management,
Journal Year:
2022,
Volume and Issue:
519, P. 120324 - 120324
Published: June 6, 2022
Forest
thinning
can
significantly
affect
hydrological
processes.
However,
these
effects
largely
vary
with
forest
types,
climate,
intensity,
and
variables
of
interest.
Understanding
their
variations
support
treatments'
design
selection
to
ensure
desired
benefits.
In
this
global-level
review
paper,
we
report
the
first
comprehensive
meta-analysis
on
major
processes
an
emphasis
rainfall
partitioning,
soil
moisture
evapotranspiration
The
synthesized
reviewed
studies
encompass
different
biophysical
conditions
(climate
ecosystems),
silvicultural
systems,
time
scales
(from
weeks
decades)
across
continents.
results
showed
a
significant
increase
in
net
precipitation,
tree-level
water
use
after
(the
effect
sizes
are
1.19,
1.14
1.56
relative
value
control,
respectively),
while
decreases
stemflow
transpiration
0.42
0.6
respectively).
Thinning
intensity
about
50%
stand
density
is
determined
as
threshold
at
or
over
which
affected.
duration
be
set
between
2.6
4.3
(throughfall)
3.1–8.6
years
(soil
transpiration),
asking
for
repeated
order
effectively
sustain
effects.
These
global
averages
serve
benchmarks
assessment
comparisons,
but
depend
local
treatments.
literature
rest
studied
suggests
that
generally
enhance
runoff
yield
groundwater
recharge.
also
have
positive
limited
role
efficiency
(WUE),
it
mitigates
drought
through
increasing
WUE.
Moderate
adverse
quality
prevented
by
adequate
managements
prevent
degradation.
Nevertheless,
more
researches
relatively
less
regions
needed
robust
analysis
variables.
management
implications
suggested
discussed
within
context
climate
change.
Water Resources Research,
Journal Year:
2025,
Volume and Issue:
61(1)
Published: Jan. 1, 2025
Abstract
Models
of
climate
change
impacts
could
be
missing
significant
risks
to
hydrologic
and
water
infrastructure
systems
through
a
shared
feature:
the
idea
that
temperatures
rise
monotonically.
By
contrast,
temperature
overshoot
pathways
describe
non‐monotonic
warming
trajectories,
in
which
global
first
exceed
given
target
before
declining
target.
Risks
from
are
qualitatively
different
associated
with
monotonic
likely
underestimated
current
research
policy.
suggest
may
almost
unavoidable
if
more
stringent
Paris
Agreement
limiting
1.5°C
over
preindustrial
levels
is
met
by
2100.
While
has
been
relatively
widely
described
literature,
on
individual
system
characteristics
have
not.
We
failure
consider
disparities
between
hydrology
resources
presents
particular
due
divergent
adaptation
needs.
Processes
decadal
hysteresis
especially
vulnerable.
These
include
glacial
contributions
streamflow;
consequences
vegetation
change;
altered
groundwater;
higher
use
for
fossil
fuel
combustion
carbon
dioxide
removal;
policy
depends
conditions.
argue
cannot
fully
captured
integrated
assessment
models
needs
specifically
evaluated
adequately
characterize
risk
system.
how
modeling
tools
adapted
evaluate
consequences,
but
also
recognize
decisions
must
made
even
without
perfect
knowledge.
Earth-Science Reviews,
Journal Year:
2022,
Volume and Issue:
230, P. 104055 - 104055
Published: May 12, 2022
As
CO2
concentration
in
the
atmosphere
rises,
there
is
a
need
for
improved
physical
understanding
of
its
impact
on
global
plant
transpiration.
This
knowledge
gap
poses
major
hurdle
robustly
projecting
changes
hydrologic
cycle.
For
this
reason,
here
we
review
different
processes
by
which
atmospheric
affects
transpiration,
several
uncertainties
related
to
complex
physiological
and
radiative
involved,
gaps
be
filled
order
improve
predictions
Although
high
degree
certainty
that
rising
will
exact
nature
remains
unclear
due
interactions
between
climate,
key
aspects
morphology
physiology.
The
interplay
these
factors
has
substantial
consequences
not
only
future
climate
vegetation,
but
also
water
availability
needed
sustaining
productivity
terrestrial
ecosystems.
Future
transpiration
response
enhanced
are
expected
driven
availability,
evaporative
demand,
processes,
emergent
disturbances
increasing
temperatures,
modification
physiology
coverage.
Considering
universal
sensitivity
natural
agricultural
systems
argue
reliable
projections
an
issue
highest
priority,
can
achieved
integrating
monitoring
modeling
efforts
representation
effects
next
generation
earth
system
models.
Earth s Future,
Journal Year:
2023,
Volume and Issue:
11(2)
Published: Jan. 17, 2023
Abstract
Continued
climate
warming
is
reducing
seasonal
snowpacks
in
the
western
United
States,
where
>50%
of
historical
water
supplies
were
snowmelt‐derived.
In
Upper
Colorado
River
Basin,
declining
snow
equivalent
(SWE)
and
altered
surface
input
(SWI,
rainfall
snowmelt
available
to
enter
soil)
timing
magnitude
affect
streamflow
generation
availability.
To
adapt
effectively
future
conditions,
we
need
understand
current
spatiotemporal
distributions
SWE
SWI
how
they
may
change
decades.
We
developed
100‐m
SnowModel
simulations
for
years
2001–2013
two
scenarios:
control
(CTL)
pseudo‐global‐warming
(PGW).
The
PGW
fraction
precipitation
falling
as
was
lower
relative
CTL,
except
November–April
at
high
elevations.
peak
low
(−45%)
mid
elevations
(−14%),
while
date
uniformly
earlier
year
all
(17–23
days).
Currently
unmonitored
elevation
represented
a
greater
total
SWE.
daily
higher
(30%–42%),
dates
peaks
centroids
under
PGW.
displayed
elevated
winter
SWI,
summer
changes
spring
elevation‐dependent.
Although
compared
more
evenly
distributed
throughout
These
simulated
shifts
have
broad
implications
management
dry,
snow‐dominated
regions.
Journal of Ecology,
Journal Year:
2024,
Volume and Issue:
112(11), P. 2451 - 2461
Published: May 24, 2024
Abstract
Via
sheltering,
decoupling
and
buffering
mechanisms,
tree
canopies
have
the
capacity
to
mitigate
impacts
of
multiple
global‐change
drivers
on
below‐canopy
processes
organisms
in
forests.
As
a
result,
an
important
potential
as
nature‐based
solution.
The
optimal
combinations
forest
canopy
structural
attributes
jointly
received
little
attention
date.
To
help
solving
this
research
gap,
here
we
review
how
modulate
effects
four
drivers—climate
warming,
drought,
air
pollution
biological
invasions—on
conditions.
Particular
is
paid
mitigating
that
can
be
influenced
by
management,
including
cover,
species
composition
vertical
horizontal
structure.
Synthesis
.
We
show
highly
context‐dependent
canopy‐based
solutions
strongly
depend
environmental
context
targeted
subcanopy
organisms.
Hence,
holistic
approaches,
which
maximize
synergies
minimize
trade‐offs,
are
needed
optimize
solution
canopies.
Landscape Ecology,
Journal Year:
2024,
Volume and Issue:
39(3)
Published: Feb. 24, 2024
Abstract
Context
Wildland-urban
interface
(WUI)
areas
are
facing
increased
forest
fire
risks
and
extreme
precipitation
events
due
to
climate
change,
which
can
lead
post-fire
flood
events.
The
city
of
Flagstaff
in
northern
Arizona,
USA
experienced
WUI
thinning,
fire,
record
rainfall
events,
collectively
contributed
large
floods
damages
the
urban
neighborhoods
infrastructure.
Objectives
We
demonstrate
multi-temporal,
high
resolution
image
applications
from
an
unoccupied
aerial
vehicle
(UAV)
terrestrial
lidar
estimating
landscape
disturbance
impacts
within
WUI.
Changes
vegetation
bare
ground
cover
WUIs
particularly
challenging
estimate
with
coarse-resolution
satellite
images
fine-scale
processes
changes
that
often
result
mixed
pixels.
Methods
Using
Sentinel-2
images,
we
document
burn
severity.
2016
2021
UAV
multispectral
Structure-from-Motion
data,
post-thinning
canopy
cover,
patch
sizes,
height
distribution,
cover.
repeat
data
a
smaller
area
watershed,
quantify
geomorphic
effects
associated
subsequent
flooding.
Results
thinning
significantly
reduced
size,
tree
density,
mean
resulting
substantially
active
crown
future.
However,
equipment
ignited
burned
at
varying
severity
top
watershed
drains
into
city.
Moderate-high
burns
occurred
3
km
downtown
threatening
upstream
then
100-year
200–500-year
resulted
runoff-driven
sedimentation
Conclusion
photogrammetry
combined
provide
detailed
accurate
estimates
impacts,
could
not
be
estimated
coarser-resolution
images.
Communities
around
world
may
need
prepare
their
for
catastrophic
fires
increase
capacity
manage
sediment-laden
stormwater
since
both
weather
projected
increase.
Hydrology and earth system sciences,
Journal Year:
2025,
Volume and Issue:
29(1), P. 27 - 43
Published: Jan. 3, 2025
Abstract.
Increasing
watershed
disturbance
regimes,
such
as
from
wildfire,
are
a
growing
concern
for
natural
resource
managers.
However,
the
influence
of
disturbances
on
event-scale
rainfall–runoff
patterns
has
proved
challenging
to
disentangle
other
hydrologic
controls.
To
better
isolate
effects,
this
study
evaluates
several
time-varying
controls
patterns,
including
water
year
type,
seasonality,
and
antecedent
precipitation.
accomplish
this,
we
developed
Rainfall–Runoff
Event
Detection
Identification
(RREDI)
toolkit,
an
automated
time-series
event
separation
attribution
algorithm
that
overcomes
limitations
existing
techniques.
The
RREDI
toolkit
was
used
generate
dataset
5042
events
nine
western
US
watersheds.
By
analyzing
large
dataset,
type
season
were
identified
significant
whereas
moisture
pinpointed
limited
control.
Specific
effects
wildfire
runoff
response
then
demonstrated
two
burned
watersheds
by
first
grouping
based
controls,
wet
versus
dry
types.
role
should
be
considered
in
future
analysis
increasing
changing
wildfires
streamflow.
could
readily
applied
investigate
patterns.