Water Resources Research,
Journal Year:
2022,
Volume and Issue:
58(3)
Published: March 1, 2022
Abstract
Accurate
estimation
of
the
spatio‐temporal
distribution
snow
water
equivalent
is
essential
given
its
global
importance
for
understanding
climate
dynamics
and
change,
as
a
source
fresh
water.
Here,
we
explore
potential
using
Long
Short‐Term
Memory
(LSTM)
network
continental
regional
scale
modeling
daily
accumulation
melt
at
4‐km
pixel
resolution
across
conterminous
US
(CONUS).
To
reduce
training
costs
(data
are
available
∼0.31
million
snowy
pixels),
combine
spatial
sampling
with
stagewise
model
development,
whereby
first
pretrained
entire
CONUS
then
subjected
to
fine‐tuning.
Accordingly,
evaluation
focused
on
out‐of‐sample
predictive
performance
space
(analogous
prediction
in
ungauged
basins
problem).
We
find
that,
identical
inputs
(precipitation,
temperature,
elevation),
single
CONUS‐wide
LSTM
provides
significantly
better
generalization
than
regionally
calibrated
version
physical‐conceptual
temperature‐index‐based
SNOW17
model.
Adding
more
meteorological
information
(dew
point
vapor
pressure
deficit,
longwave
radiation,
shortwave
radiation)
further
improves
performance,
while
rendering
redundant
local
provided
by
elevation.
Overall,
exhibits
transferability
locations
that
were
not
included
data
set,
reinforcing
advantages
structure
learning
over
parameter
learning.
Our
results
suggest
an
LSTM‐based
approach
could
be
used
develop
continental/global‐scale
systems
dynamics.
Nature Climate Change,
Journal Year:
2023,
Volume and Issue:
13(2), P. 182 - 188
Published: Jan. 19, 2023
Abstract
The
time
required
for
an
ecosystem
to
recover
from
severe
drought
is
a
key
component
of
ecological
resilience.
phenology
effects
on
recovery
are,
however,
poorly
understood.
These
centre
how
variations
impact
biophysical
feedbacks,
vegetation
growth
and,
ultimately,
itself.
Using
multiple
remotely
sensed
datasets,
we
found
that
more
than
half
ecosystems
in
mid-
and
high-latitudinal
Northern
Hemisphere
failed
extreme
droughts
within
single
growing
season.
Earlier
spring
the
year
slowed
when
occurred
mid-growing
Delayed
subsequent
all
types
(with
importance
ranging
46%
58%).
were
comparable
or
larger
other
well-known
postdrought
climatic
factors.
results
strongly
suggest
interactions
between
must
be
incorporated
into
Earth
system
models
accurately
quantify
Earth s Future,
Journal Year:
2022,
Volume and Issue:
10(3)
Published: March 1, 2022
Abstract
Thousands
of
glacier
lakes
have
been
forming
behind
natural
dams
in
high
mountains
following
retreat
since
the
early
20th
century.
Some
these
abruptly
released
pulses
water
and
sediment
with
disastrous
downstream
consequences.
Yet
it
remains
unclear
whether
reported
rise
lake
outburst
floods
(GLOFs)
has
fueled
by
a
warming
atmosphere
enhanced
meltwater
production,
or
simply
growing
research
effort.
Here
we
estimate
trends
biases
GLOF
reporting
based
on
largest
global
catalog
1,997
dated
glacier‐related
six
major
mountain
ranges
from
1901
to
2017.
We
find
that
positive
trend
number
GLOFs
decayed
distinctly
after
break
1970s,
coinciding
independently
detected
changes
annual
air
temperatures
field‐based
surveys
(a
proxy
scientific
reporting).
observe
reports
decelerated,
while
temperature
accelerated
past
five
decades.
Enhanced
alone
can
thus
hardly
explain
GLOFs,
suggesting
temperature‐driven
formation,
growth,
failure
are
weakly
coupled,
outbursts
overlooked.
Indeed,
our
analysis
emphasizes
distinct
geographic
temporal
bias
reporting,
project
between
two
four
out
average
might
gone
unnoticed
mid‐20th
recommend
such
should
be
considered,
better
corrected
for,
when
attributing
frequency
atmospheric
warming.
Photochemical & Photobiological Sciences,
Journal Year:
2022,
Volume and Issue:
21(3), P. 275 - 301
Published: Feb. 21, 2022
Abstract
The
Environmental
Effects
Assessment
Panel
of
the
Montreal
Protocol
under
United
Nations
Environment
Programme
evaluates
effects
on
environment
and
human
health
that
arise
from
changes
in
stratospheric
ozone
layer
concomitant
variations
ultraviolet
(UV)
radiation
at
Earth’s
surface.
current
update
is
based
scientific
advances
have
accumulated
since
our
last
assessment
(Photochem
Photobiol
Sci
20(1):1–67,
2021).
We
also
discuss
how
climate
change
affects
depletion
radiation,
change.
resulting
interlinking
depletion,
UV
are
assessed
terms
air
quality,
carbon
sinks,
ecosystems,
health,
natural
synthetic
materials.
further
highlight
potential
impacts
biosphere
extreme
events
occurring
with
increasing
frequency
as
a
consequence
These
other
interactive
examined
respect
to
benefits
its
Amendments
providing
life
Earth
by
controlling
production
various
substances
contribute
both
Photochemical & Photobiological Sciences,
Journal Year:
2023,
Volume and Issue:
22(5), P. 1049 - 1091
Published: Feb. 1, 2023
Terrestrial
organisms
and
ecosystems
are
being
exposed
to
new
rapidly
changing
combinations
of
solar
UV
radiation
other
environmental
factors
because
ongoing
changes
in
stratospheric
ozone
climate.
In
this
Quadrennial
Assessment,
we
examine
the
interactive
effects
ozone,
climate
on
terrestrial
biogeochemical
cycles
context
Montreal
Protocol.
We
specifically
assess
organisms,
agriculture
food
supply,
biodiversity,
ecosystem
services
feedbacks
system.
Emphasis
is
placed
role
extreme
events
altering
exposure
potential
biodiversity.
also
address
responses
plants
increased
temporal
variability
radiation,
change
(e.g.
drought,
temperature)
crops,
driving
breakdown
organic
matter
from
dead
plant
material
(i.e.
litter)
biocides
(pesticides
herbicides).
Our
assessment
indicates
that
interact
various
ways
affect
structure
function
ecosystems,
by
protecting
layer,
Protocol
continues
play
a
vital
maintaining
healthy,
diverse
land
sustain
life
Earth.
Furthermore,
its
Kigali
Amendment
mitigating
some
negative
consequences
limiting
emissions
greenhouse
gases
carbon
sequestration
vegetation
pool.
Abstract
Mountain
snowpacks
act
as
natural
water
towers,
storing
winter
precipitation
until
summer
months
when
downstream
demand
is
greatest.
We
introduce
a
Snow
Storage
Index
(SSI),
representing
the
temporal
phase
difference
between
daily
and
surface
inputs—sum
of
rainfall
snowmelt
into
terrestrial
systems—weighted
by
relative
magnitudes.
Different
from
snow
equivalent
or
fraction,
SSI
represents
degree
to
which
snowpack
delays
timing
magnitude
inputs
precipitation,
fundamental
component
how
storage
influences
hydrologic
cycle.
In
western
North
America,
annual
has
decreased
(
p
<
0.05)
1950–2013
in
over
25%
mountainous
areas,
result
substantially
earlier
spring
months,
with
additional
declines
precipitation.
The
associated
trends
offer
new
perspective
on
sensitivity
climate
change
have
broad
implications
for
resources
ecosystems.
Water Resources Research,
Journal Year:
2025,
Volume and Issue:
61(1)
Published: Jan. 1, 2025
Abstract
Snow
drought,
characterized
by
an
anomalous
reduction
in
snowpack,
exerts
profound
hydrological
and
socioeconomic
impacts
cold
regions.
Despite
its
significance,
the
influence
of
diverse
snow
drought
types,
including
warm,
dry,
warm‐and‐dry
variants,
on
streamflow
remains
inadequately
understood.
Here
we
present
first
hemispheric‐scale,
observation‐based
assessment
patterns
seasonal
annual
(
Q
)
across
3049
northern
catchments
over
1950–2020.
Our
findings
reveal
that
with
a
lower
mean
snowfall
fraction
()
exhibit
heightened
prevalence
severity
warm
droughts,
whereas
high‐
experience
more
prevalent
but
less
severe
dry
drought.
This
disparity
arises
from
distinct
sensitivities
snowpack
to
cold‐season
precipitation
temperature.
In
addition,
droughts
induce
during
both
seasons,
culminating
significant
decrease
.
Conversely,
increases
decreases
,
attributable
trade‐off
between
increased
c
decreased
warm‐season
w
).
With
ongoing
climate
warming,
continued
is
anticipated,
which
expected
further
increase
frequency
warm‐dry
droughts.
These
circumstances,
particularly
impactful
under
low
conditions,
are
poised
formidable
challenges
for
water
resources
management
regions
globally.