Hydrology and earth system sciences,
Journal Year:
2022,
Volume and Issue:
26(2), P. 279 - 304
Published: Jan. 24, 2022
Abstract.
This
study
analyses
river
discharge
into
the
Arctic
Ocean
using
state-of-the-art
reanalyses
such
as
fifth-generation
European
Reanalysis
(ERA5)
and
reanalysis
component
from
Global
Flood
Awareness
System
(GloFAS).
GloFAS,
in
its
operational
version
2.1,
combines
land
surface
model
(Hydrology
Tiled
Centre
for
Medium-Range
Weather
Forecasts
–
ECMWF
Scheme
Surface
Exchanges
over
Land,
HTESSEL)
ECMWF’s
ERA5
with
a
hydrological
channel
routing
(LISFLOOD).
Furthermore,
we
analyse
GloFAS'
most
recent
3.1,
which
is
not
coupled
to
HTESSEL
but
uses
full
configuration
of
LISFLOOD.
Seasonal
cycles
well
annual
runoff
trends
are
analysed
major
watersheds
Yenisei,
Ob,
Lena,
Mackenzie
where
reanalysis-based
can
be
compared
available
observed
records.
calculate
whole
pan-Arctic
region
and,
by
combination
atmospheric
inputs,
storage
changes
Gravity
Recovery
Climate
Experiment
(GRACE)
oceanic
volume
transports
ocean
reanalyses,
assess
closure
non-steric
water
budget.
Finally,
provide
best
estimates
every
budget
equation
term
variational
adjustment
scheme.
Runoff
GloFAS
v2.1
features
pronounced
declining
induced
two
temporal
inhomogeneities
ERA5's
data
assimilation
system,
seasonal
peaks
underestimated
up
50
%
observations.
The
new
v3.1
product
exhibits
distinct
improvements
performs
terms
seasonality
long-term
means;
however,
contrast
gauge
observations,
it
also
trends.
Calculating
indirectly
through
divergence
moisture
flux
only
estimate
that
able
reproduce
increases
measured
observations
(pan-Arctic
increase
2
per
decade).
In
addition,
examine
Greenlandic
discharge,
contributes
about
10
total
strong
mainly
due
glacial
melting.
yields
reliable
on
an
scale,
requiring
moderate
adjustments
less
than
3
each
individual
term.
Approximately
6583±84
km3
freshwater
leaves
year
boundaries.
About
two-thirds
this
contributed
surrounding
areas
(4379±25
yr−1),
one-third
supplied
atmosphere.
However,
scale
residuals
some
calendar
months
were
too
large
eliminated
within
priori
spreads
terms.
suggests
systematical
errors
present
sets,
considered
our
uncertainty
estimation.
Earth system science data,
Journal Year:
2021,
Volume and Issue:
13(9), P. 4349 - 4383
Published: Sept. 7, 2021
Abstract.
Framed
within
the
Copernicus
Climate
Change
Service
(C3S)
of
European
Commission,
Centre
for
Medium-Range
Weather
Forecasts
(ECMWF)
is
producing
an
enhanced
global
dataset
land
component
fifth
generation
ReAnalysis
(ERA5),
hereafter
referred
to
as
ERA5-Land.
Once
completed,
period
covered
will
span
from
1950
present,
with
continuous
updates
support
monitoring
applications.
ERA5-Land
describes
evolution
water
and
energy
cycles
over
in
a
consistent
manner
production
period,
which,
among
others,
could
be
used
analyse
trends
anomalies.
This
achieved
through
high-resolution
numerical
integrations
ECMWF
surface
model
driven
by
downscaled
meteorological
forcing
ERA5
climate
reanalysis,
including
elevation
correction
thermodynamic
near-surface
state.
shares
most
parameterizations
that
guarantees
use
state-of-the-art
modelling
applied
weather
prediction
(NWP)
models.
A
main
advantage
compared
older
ERA-Interim
horizontal
resolution,
which
globally
9
km
31
(ERA5)
or
80
(ERA-Interim),
whereas
temporal
resolution
hourly
ERA5.
Evaluation
against
independent
situ
observations
satellite-based
reference
datasets
shows
added
value
description
hydrological
cycle,
particular
soil
moisture
lake
description,
overall
better
agreement
river
discharge
estimations
available
observations.
However,
snow
depth
fields
present
mixed
performance
when
those
ERA5,
depending
on
geographical
location
altitude.
The
cycle
comparable
results
Nevertheless,
reduces
averaged
root
mean
square
error
skin
temperature,
taking
MODIS
data,
mainly
due
contribution
coastal
points
where
spatial
important.
Since
January
2020,
has
extended
1981
near
2-
3-month
delay
respect
real
time.
segment
prior
production,
aiming
release
whole
summer/autumn
2021.
high
ERA5-Land,
its
consistency
produced
makes
it
valuable
studies,
initialize
NWP
models,
diverse
applications
dealing
resource,
land,
environmental
management.
full
(Muñoz-Sabater,
2019a)
monthly
2019b)
presented
this
paper
are
C3S
Data
Store
at
https://doi.org/10.24381/cds.e2161bac
https://doi.org/10.24381/cds.68d2bb30,
respectively.
Water Resources Research,
Journal Year:
2021,
Volume and Issue:
57(5)
Published: May 1, 2021
Abstract
The
hydrological
response
to
climate
change
in
mountainous
basins
manifests
itself
at
varying
spatial
and
temporal
scales,
ranging
from
catchment
large
river
basin
scale
sub‐daily
decade
century
scale.
To
robustly
assess
the
21st
impact
for
hydrology
entire
High
Mountain
Asia
(HMA)
a
wide
range
of
we
use
high
resolution
cryospheric‐hydrological
model
covering
15
upstream
HMA
quantify
compound
effects
future
changes
precipitation
temperature
based
on
projections
Coupled
Model
Intercomparison
Project
Phase
6
ensemble.
Our
analysis
reveals
contrasting
responses
HMA's
rivers,
dictated
by
their
regimes.
At
seasonal
scale,
earlier
onset
melting
causes
shift
magnitude
peak
water
availability,
year.
after
an
initial
increase,
glacier
melt
declines
mid
or
end
except
Tarim
basin,
where
it
continues
increase.
Despite
variability
regimes
across
our
results
indicate
relatively
consistent
terms
total
availability
decadal
time
scales.
Although
increases
headwaters,
seasonality
may
diverge
widely
between
need
be
addressed
while
adapting
region
food
security,
energy
security
as
well
biodiversity,
livelihoods
many
depend
HMA.
Water Resources Research,
Journal Year:
2022,
Volume and Issue:
58(3)
Published: March 1, 2022
Abstract
Quantification
of
the
global
irrigation
water
use
(IWU)
is
crucial
to
understanding
anthropogenic
disturbance
natural
hydrological
cycle
and
optimal
agricultural
management.
However,
it
challenging
obtain
time
series
data
with
conventional
survey‐based
approach,
while
current
satellite‐based
IWU
estimations
are
subject
gaps
model
structure.
In
this
paper,
we
propose
a
comprehensive
framework
couple
different
processes
associated
integrate
multiple
satellite
observations
estimate
IWU.
The
ensemble
demonstrates
an
improved
performance
when
compared
obtained
from
individual
observations.
results
show
reasonable
correlation
withdrawal
in
states
US
(bias
=
−0.42
km
3
),
provinces
China
−3.10
country
statistics
Food
Agriculture
Organization
−10.84
).
Large
amounts
apparent
India,
China,
US,
Europe,
Pakistan,
making
up
>70%
A
general
underestimation
found
both
work
previous
studies,
due
coarse
resolution
asynchronism
various
products,
changes
irrigated
areas,
deficiency
detecting
events
under
case
saturated
soil
moisture.
Nevertheless,
demonstrate
advantages
integrating
reduce
uncertainty
estimating
additional
efforts
needed
produce
high‐quality
finer
spatiotemporal
further
improve
accuracy
estimation.
Scientific Data,
Journal Year:
2024,
Volume and Issue:
11(1)
Published: May 3, 2024
Quantifying
terrestrial
evapotranspiration
(ET)
and
soil
moisture
dynamics
accurately
is
crucial
for
understanding
the
global
water
cycle
surface
energy
balance.
We
present
a
novel,
long-term
dataset
of
ET
derived
from
newly
developed
Simple
Terrestrial
Hydrosphere
model,
version
2
(SiTHv2).
This
ecohydrological
driven
by
multi-source
satellite
observations
hydrometeorological
variables
reanalysis
data,
provides
daily
ET-related
estimates
(e.g.,
total
ET,
plant
transpiration,
evaporation,
intercepted
evaporation)
three-layer
at
0.1°
spatial
resolution.
Validation
with
in-situ
measurements
comparisons
mainstream
products
demonstrate
robust
performance
SiTHv2
in
both
magnitude
temporal
multiple
scales.
The
comprehensive
path
characterization
model
makes
this
seamless
particularly
valuable
studies
requiring
synchronized
budget
vegetation
response
to
constraints.
With
its
coverage
high
spatiotemporal
resolution,
SiTHv2-derived
product
will
be
suitable
support
analyses
related
hydrologic
cycle,
drought
assessment,
ecosystem
health.
Frontiers in Environmental Science,
Journal Year:
2022,
Volume and Issue:
10
Published: May 25, 2022
Long-term
and
high-resolution
gridded
products
of
precipitation
temperature
data
are
highly
important
to
study
the
changes
in
climate
environment
under
global
warming.
Considering
uncertainties
these
mountainous
areas,
it
is
necessary
evaluate
reliability.
This
evaluates
performances
CMFD
(China
Meteorological
Forcing
Dataset)
ERA5-Land
simulating
Qilian
Mountains
over
period
1980–2018.
We
use
observation
28
basic
meteorological
stations
compare
with
reanalysis
products.
Error
metrics
(the
correlation
coefficient
(CC),
root
mean
square
error
(RMSE),
absolute
(MAE),
relative
bias
(BIAS))
used
quantify
monthly
differences
existence
between
observed
data.
Our
findings
indicate
that
both
could
well
reproduce
spatial
distribution
region.
A
good
found
OBS
different
amounts
conditions.
The
average
temperatures
reveal
a
high
results.
Moreover,
CC
values
highest
autumn
lowest
winter,
higher
spring
autumn.
However,
we
find
underestimate
varying
degrees,
amount
overestimated
by
ERA5-Land.
results
evaluation
show
errors
yielded
as
whole
distinctly
fewer
than
those
ERA5-Land,
while
air
nearly
identical
each
other.
Overall,
more
suitable
for
studying
trends
Mountains.
As
simulation
precipitation,
performs
better
central
eastern
parts
Mountains,
whereas
western
part
Frontiers in Earth Science,
Journal Year:
2022,
Volume and Issue:
10
Published: Aug. 8, 2022
Reanalysis
temperature
products
are
important
datasets
for
estimates
over
high-elevation
areas
with
few
meteorological
stations.
In
this
study,
surface
2
m
air
data
from
17
stations
1979
to
2017
in
the
Qilian
Mountains
(QLM)
used
comparison
newest
reanalysis
product:
ERA5-Land
derived
European
Centre
Medium-Range
Weather
Forecasts
(ECMWF).
general,
product
can
reproduce
observation
variation
at
different
time
scales
very
well.
A
high
monthly
correlation
coefficient
that
ranges
0.978
0.998
suggests
could
capture
observations
However,
attention
should
be
paid
before
using
individual
sites
because
of
average
root-mean-square-error
(RMSE)
2.2°C
all
The
biases
between
and
mainly
caused
by
elevation
differences
grid
points
sites.
annual
mean
shows
a
significant
warming
trend
(0.488°C/decade)
based
on
observations.
captures
increasing
well
(0.379°C/decade).
biggest
positive
trends
both
found
summer
values
0.574°C/decade
0.496°C/decade,
respectively.
We
suggest
generally
reproduces
is
reliable
scientific
research
QLM.
Earth system science data,
Journal Year:
2023,
Volume and Issue:
15(9), P. 3905 - 3930
Published: Sept. 4, 2023
Abstract.
Permafrost
over
the
Qinghai–Tibet
Plateau
(QTP)
has
received
increasing
attention
due
to
its
high
sensitivity
climate
change.
Numerous
spatial
modeling
studies
have
been
conducted
on
QTP
assess
status
of
permafrost,
project
future
changes
in
and
diagnose
contributors
permafrost
degradation.
Due
scarcity
ground
stations
QTP,
these
are
often
hampered
by
lack
validation
references,
calibration
targets,
model
constraints;
however,
a
high-quality
distribution
map
would
be
good
option
as
benchmark
for
simulations.
Existing
maps
can
poorly
serve
this
purpose.
An
ideal
should
methodologically
sound,
sufficient
accuracy,
based
observations
from
mapping
years
rather
than
all
historical
data
spanning
several
decades.
Therefore,
study,
we
created
new
2010
using
novel
approach
with
satellite-derived
surface
thawing
freezing
indices
inputs
survey-based
subregion
constraints.
This
accounted
effects
local
factors
incorporating
(into
model)
an
empirical
soil
parameter
whose
values
were
optimally
estimated
through
clustering
optimization
constrained
maps,
was
also
improved
reduce
parametric
equifinality.
showed
total
area
about
1.086×106
km2
(41.2
%
area)
seasonally
frozen
1.447×106
(54.9
%)
2010,
excluding
glaciers
lakes.
Validations
(κ=0.74)
borehole
records
(overall
accuracy
=0.85
κ=0.43)
higher
compared
two
other
recent
maps.
Inspection
regions
obvious
distinctions
between
affirms
that
is
more
realistic
Zou
et
al.
(2017)
map.
Given
demonstrated
excellent
constraining/validating
land
simulations
reference
projecting
context
global
warming.
The
dataset
available
repository
hosted
Figshare
(Cao
al.,
2022):
https://doi.org/10.6084/m9.figshare.19642362.
International Journal of Climatology,
Journal Year:
2024,
Volume and Issue:
44(7), P. 2318 - 2342
Published: April 11, 2024
Abstract
Reanalysis
datasets
provide
a
continuous
picture
of
the
past
climate
for
every
point
on
Earth.
They
are
especially
useful
in
areas
with
few
direct
observations,
such
as
Siberia.
However,
to
ensure
these
sufficiently
accurate
they
need
be
validated
against
readings
from
meteorological
stations.
Here,
we
analyse
how
values
six
variables—the
minimum,
mean
and
maximum
2‐metre
air
temperature,
snow
depth
(SD),
total
precipitation
wind
speed
(WSP)—from
three
reanalysis
datasets—ERA‐Interim,
ERA5
ERA5‐Land—compare
observations
29
stations
across
Siberia
Russian
Far
East
daily
timescale
1979
2019.
All
reanalyses
produce
temperature
that
close
those
observed,
average
absolute
bias
not
exceeding
1.54°C.
care
should
taken
minimum
during
summer
months—there
nine
where
correlation
<0.60
due
inadequate
night‐time
cooling.
The
SD
generally
observed
after
1992,
ERA5,
when
data
some
began
assimilated,
but
used
caution
(if
at
all)
before
1992
lack
assimilation
leads
large
overestimations.
For
low
good
approximations,
however
struggle
attain
extreme
high
values.
Similarly,
10‐metre
WSP;
perform
well
speeds
up
2.5
ms
−1
above
5.0
.
variables,
recommend
using
over
ERA‐Interim
ERA5‐Land
future
research.
shows
minor
improvements
ERA‐Interim,
and,
despite
an
increased
spatial
resolution,
there
is
no
advantage
ERA5‐Land.