A
variety
of
watershed
responses
to
climate
change
are
expected
due
non-linear
interactions
between
various
hydrologic
processes
acting
at
different
timescales
that
modulated
by
properties.
Changes
in
statistical
structure
(spectral
properties)
streamflow
the
USA
were
studied
for
water
years
1980-2013.
The
Fractionally
differenced
Autoregressive
Integrated
Moving
Average
(FARIMA)
model
was
fit
deseasonalized
time-series
its
structure.
FARIMA
allows
separation
into
low
frequency
(slowly
varying)
and
high
(fast
components.
Results
show
snow
dominated
watersheds,
contribution
components
total
variance
has
decreased
over
study
period,
increased.
watersheds
primarily
driven
changes
rainfall
statistics
equivalent
but
also
seasonal
temperature
statistics.
Among
rain-driven
generally
increased
arid
regions
humid
regions.
In
both
increasing
winter
responsible
regimes.
These
results
have
consequences
predictability
presence
change.
We
expect
component
will
result
poorer
streamflow.
Ecohydrology,
Journal Year:
2023,
Volume and Issue:
16(7)
Published: Aug. 29, 2023
Abstract
The
Sierra
Nevada
has
experienced
unprecedented
wildfires
and
reduced
snowmelt
runoff
in
recent
decades,
due
partially
to
anthropogenic
climate
change
over
a
century
of
fire
suppression.
To
address
these
challenges,
public
land
agencies
are
planning
forest
restoration
treatments,
which
have
the
potential
both
increase
water
availability
reduce
likelihood
uncontrollable
wildfires.
However,
impact
on
snowpack
is
site
specific
not
well
understood
across
gradients
topography.
improve
our
understanding
how
might
diverse
conditions
central
Nevada,
we
run
high‐resolution
(1
m)
energy
mass
balance
Snow
Physics
Lidar
Mapping
(SnowPALM)
model
five
23–75
km
2
subdomains
region
where
thinning
planned
or
recently
completed.
We
conduct
two
virtual
experiments
by
removing
all
trees
shorter
than
10
20
m
tall
rerunning
SnowPALM
calculate
meltwater
input.
Our
results
indicate
heterogeneous
responses
differences
wind
subdomains.
also
predict
largest
increases
snow
retention
when
forests
with
(7–20
dense
(40–70%
canopy
cover)
trees,
highlighting
importance
pre‐thinning
vegetation
structure.
develop
decision
support
tool
using
random
determine
regions
would
most
benefit
from
thinning.
In
many
locations,
expect
major
accumulation,
while
other
areas
short
sparse
canopies,
as
sunny
windy
climates,
more
likely
see
decreased
following
provides
stand‐scale
(30
information
managers
best
take
advantage
existing
structure
obtain
greatest
benefits
restoration.
Abstract
This
review
article
focuses
on
the
complex
relationships
between
forests
and
water,
particularly
effects
of
streamflow
during
meteorological
droughts.
The
impact
water
resources
is
a
long‐standing
research
topic,
but
there
are
also
many
common
beliefs
that
not
based
scientific
evidence
or
only
selective
evidence.
We
critically
examine
origin
some
public
misconceptions
wealth
studies
how
precipitation,
soil
dynamics,
evapotranspiration,
streamflow.
Generally,
reforestation
increases
evapotranspiration
decreases
groundwater
recharge
However,
evaporated
will
return
as
potentially
offsetting
increased
losses.
Where
leads
to
more
extensive
infiltration
due
soil's
hydraulic
properties,
it
might
increase
dry
periods.
Although
these
individual
processes
have
been
studied,
predicting
impacts
remains
challenging
site‐specific
depend
factors,
such
climate,
forest‐
soil‐characteristics
before
after
reforestation,
hydrogeological
setting.
accurate
nuanced
understanding
role
hydrology
better
ability
predict
where
when
net
positive
negative
crucial
for
sustainable
forest
management.
categorized
under:
Science
Water
>
Environmental
Change
Hydrological
Processes
Engineering
Sustainable
Hydrological Processes,
Journal Year:
2024,
Volume and Issue:
38(11)
Published: Nov. 1, 2024
ABSTRACT
Wildfire
activity
in
the
western
United
States
(WUS)
is
increasingly
impacting
water
supply,
and
land
surface
models
(LSMs)
that
do
not
explicitly
account
for
fire
disturbances
can
have
critical
uncertainties
burned
areas.
This
study
quantified
responses
from
Weather
Research
Forecasting
Hydrological
modelling
system
(WRF‐Hydro)
to
a
suite
of
fire‐related
perturbations
hydrologic
soil
runoff
parameters,
vegetation
area,
cover
classifications
associated
properties,
snow
albedo
across
heavily
Feather
River
Basin
California.
These
experiments
were
used
quantify
impacts
model
simulations
under
observed
meteorological
conditions
during
2000–2022
years
determine
whether
applying
these
enhanced
post‐fire
accuracy
11–12
months
evaluated
herein.
The
most
comprehensive
fire‐aware
simulation
consistently
modelled
annual
catchment
streamflow
(by
8%–37%),
subsurface
flow
72%–116%),
moisture
4%–9%),
relative
baseline
which
neglected
impacts.
Simulated
fire‐enhanced
was
predominately
attributable
fire‐induced
area
reductions
reduced
transpiration.
enhancements
occurred
throughout
year,
excluding
early‐summer
(e.g.,
May–June)
when
relatively
more
snowmelt
because
caused
earlier
depletion.
Vegetation
favoured
increased
ground
accumulation
ablation
while
imposed
darkening
ablation,
ultimately
resulting
similar
peak
SWE
disappearance
(on
average
by
8‐days)
simulation.
had
large
degradations
following
major
events
likely
partially
neglecting
disturbances.
Applying
anomaly
biases
three
catchments.
However,
remaining
fire‐perturbed
underscores
importance
additional
observationally
constrained
fire‐disturbance
developments.
Ecological Indicators,
Journal Year:
2022,
Volume and Issue:
145, P. 109623 - 109623
Published: Nov. 2, 2022
Understanding
how
bushfire
affects
basin-wide
ecohydrological
processes
is
critical
for
ecological
restoration
and
water
supply.
However,
the
mechanisms
responsible
post-fire
streamflow
remain
poorly
explored
in
forested
basins
of
China
due
to
complex
scale-dependent
relationships
between
fire-induced
forest
changes
processes,
lack
reasonable
design
paired
watershed
experiments,
especially
data
scarcity.
Here,
we
re-examine
responses
Black
Dragon
fire
(one
largest
most
damaging
fires
on
record
globally)
an
annual
scale
three
(two
fire-impacted
basins,
namely
Emuer
Pangu,
a
nearly
unimpacted
basin,
Huma)
Daxing'an
Mountains
using
multiple
recent
datasets
methods.
We
found
that
decreased
annual-
basin-averaged
vegetation
leaf
area,
evapotranspiration,
interception
loss,
transpiration,
soil
moisture,
runoff,
discharge
capacity
1987
two
compared
with
basin.
The
evapotranspiration
(runoff)
did
not
reduce
(increase)
as
much
expected
LAI
given
precipitation
amount
which
properly
linked
quick
postfire
regrowth
growing
season.
Vegetation
area
productivity
can
quickly
recover
following
years
postfire,
but
hydrological
systems
need
more
than
10
adapt
this
disturbance.
These
findings
improve
understanding
disturbance
provide
scientific
evidence
protection
resources
management
under
intensified
natural
anthropogenic
disturbances.
Hydrological Processes,
Journal Year:
2024,
Volume and Issue:
38(6)
Published: June 1, 2024
Abstract
In
the
western
United
States,
water
supplies
largely
originate
as
snowmelt
from
forested
land.
Forests
impact
balance
of
these
headwater
streams,
yet
most
predictive
runoff
models
do
not
explicitly
account
for
changing
snow‐vegetation
dynamics.
Here,
we
present
a
case
study
showing
how
warmer
temperatures
and
forests
in
Henrys
Fork
Snake
River,
seasonally
snow‐covered
basin
Greater
Yellowstone
Ecosystem,
have
altered
relationship
between
April
1st
snow
equivalent
(SWE)
summer
streamflow.
Since
onset
recovery
severe
drought
early
2000s,
based
on
pre‐drought
relationships
over‐predict
all
three
tributaries
Fork,
despite
minimal
changes
precipitation
or
accumulation.
Compared
with
period,
late
springs
summers
(May–September)
are
vegetation
is
greener
denser
due
to
multiple
historical
disturbances.
Shifts
alignment
energy
availability
may
reduce
efficiency
by
amount
that
goes
evapotranspiration
versus
recharge.
To
quantify
timeframe
needed
models,
propose
new
metric,
Vegetation‐Water
Alignment
Index
(VWA),
characterize
synchrony
greenness
rain
inputs.
New
show
addition
SWE,
previous
year's
VWA
reference
significant
predictors
each
watershed
provide
more
power
than
traditionally
used
metrics.
These
results
suggest
timing
relative
start
growing
season
affects
only
annual
partitioning
streamflow,
but
can
also
determine
groundwater
storage
state
dictates
following
spring.
Water Resources Research,
Journal Year:
2024,
Volume and Issue:
60(9)
Published: Sept. 1, 2024
Abstract
Increasing
wildfire
frequency
and
severity
in
high‐elevation
seasonal
snow
zones
presents
a
considerable
water
resource
management
challenge
across
the
western
United
States
(U.S.).
Wildfires
can
affect
snowpack
accumulation
melt
patterns,
altering
quantity
timing
of
runoff.
While
prior
research
has
shown
that
generally
increases
rates
advances
disappearance
dates,
uncertainties
remain
regarding
variations
complex
terrain
energy
balance
between
burned
unburned
areas.
Utilizing
paired
situ
data
sources
within
2020
Cameron
Peak
burn
area
on
Front
Range
Colorado,
U.S.,
during
2021–2022
winter,
we
found
no
significant
difference
peak
equivalent
(SWE)
magnitude
However,
south
aspect
reached
SWE
22
days
earlier
than
north.
During
ablation
period,
were
71%
faster
rates,
whereas
north
94%
aspects.
Snow
disappeared
7–11
areas
Net
differences
at
weather
station
sites
seasonally
variable,
lost
more
net
but
gained
spring.
Increased
incoming
shortwave
radiation
site
was
6
x
impactful
decline
surface
albedo.
These
findings
emphasize
need
for
post‐wildfire
planning
accounts
aspect‐dependent
mass
to
accurately
predict
storage
runoff
timing.
Ecohydrology,
Journal Year:
2024,
Volume and Issue:
unknown
Published: Nov. 29, 2024
ABSTRACT
In
recent
decades,
forest
disturbances
caused
by
wildfire,
insect
and
disease‐induced
mortality
drought
have
increased
in
frequency
magnitude,
especially
the
Western
United
States.
Forest
been
shown
to
alter
water
budget
partitioning.
However,
response
disturbance
is
inconsistent
still
being
characterized
within
hydrology
(FDH)
literature.
this
review
synthesis,
we
evaluate
how
FDH
literature
has
grown
decades
(2000–2021),
extract
papers
discussing
compound
(or
overlapping)
We
then
compare
findings
with
actual
prevalence
of
(caused
insects
disease)
forested
catchments
States,
at
HUC‐8,
−10
−12
scales.
find
that
94%
HUC‐8
basins,
85%
HUC‐10
60%
HUC‐12
basins
experienced
wildfire
insect/disease
over
period
2000–2022,
virtually,
no
remain
undisturbed.
These
figures
contrast
literature,
where
relatively
few
studies
hydrologic
implications
disturbances.
suggest
not
‘meeting
moment’
perhaps,
more
critically,
true
control
‘static’)
are
nearly
nonexistent
highlight
as
a
community
ecohydrologists,
must
rethink
assess
post‐disturbance
This
will
require
better
tools
(e.g.,
models)
hydrology,
observations
cross‐disciplinary
collaborations
between
forestry
communities.
Forests,
Journal Year:
2023,
Volume and Issue:
14(8), P. 1530 - 1530
Published: July 26, 2023
This
study
investigates
the
relationship
between
soil
moisture
and
growth
of
Pinus
halepensis,
P.
nigra,
sylvestris
uncinata,
which
are
some
main
pine
species
Iberian
Peninsula,
response
these
to
drought.
The
role
played
by
climatic
geographic
factors
in
resilience
drought
events
is
also
evaluated.
A
total
110
locations
four
studied
were
selected,
with
data
ranging
from
1950
2007.
results
show
that
less
dependent
on
best
withstood
droughts,
while
those
more
it
showed
better
adaptability.
Additionally,
had
a
stronger
influence
species’
at
higher
altitudes.
this
can
help
us
understand
forest
ecosystem
dynamics
their
reaction
droughts
Mediterranean
areas,
where
phenomenon
will
be
much
severe
future
due
climate
change.
EarthArXiv (California Digital Library),
Journal Year:
2022,
Volume and Issue:
unknown
Published: Dec. 26, 2022
A
variety
of
watershed
responses
to
climate
change
are
expected
due
non-linear
interactions
between
various
hydrologic
processes
acting
at
different
timescales
that
modulated
by
properties.
Changes
in
statistical
structure
(spectral
properties)
streamflow
the
USA
were
studied
for
water
years
1980-2013.
The
Fractionally
differenced
Autoregressive
Integrated
Moving
Average
(FARIMA)
model
was
fit
deseasonalized
time
series
its
structure.
FARIMA
allows
separation
into
low-
(slowly
varying)
and
high-frequency
(fast
components.
Results
show
snow-dominated
watersheds,
contribution
low-frequency
components
total
variance
decreased
over
study
period,
increased.
watersheds
primarily
driven
changes
rainfall
statistics
snow
equivalent
but
also
seasonal
temperature
statistics.
Among
rain-driven
generally
increased
arid
regions
humid
regions.
In
both
increasing
winter
appears
be
responsible
These
results
have
consequences
predictability
presence
change.
We
expect
component
will
result
streamflow.
Further,
analysis
carried
out
this
understand
plausible
affect
without
using
process-based
or
conceptual
models.