Earth s Future,
Journal Year:
2024,
Volume and Issue:
12(11)
Published: Oct. 31, 2024
Abstract
Wetland
methane
(CH
4
)
emissions
have
a
significant
impact
on
the
global
climate
system.
However,
current
estimation
of
wetland
CH
at
scale
still
has
large
uncertainties.
Here
we
developed
six
distinct
bottom‐up
machine
learning
(ML)
models
using
in
situ
fluxes
from
both
chamber
measurements
and
Fluxnet‐CH
network.
To
reduce
uncertainties,
adopted
multi‐model
ensemble
(MME)
approach
to
estimate
emissions.
Precipitation,
air
temperature,
soil
properties,
types,
types
are
considered
developing
models.
The
MME
is
then
extrapolated
1979
2099.
We
found
that
annual
146.6
±
12.2
Tg
yr
−1
(1
=
10
12
g)
2022.
Future
will
reach
165.8
11.6,
185.6
15.0,
193.6
17.2
last
two
decades
21st
century
under
SSP126,
SSP370,
SSP585
scenarios,
respectively.
Northern
Europe
near‐equatorial
areas
emission
hotspots.
further
constrain
quantification
uncertainty,
research
priorities
should
be
directed
comprehensive
better
characterization
spatial
dynamics
areas.
Our
data‐driven
ML‐based
products
for
contemporary
shall
facilitate
future
cycle
studies.
Geoscientific model development,
Journal Year:
2025,
Volume and Issue:
18(3), P. 863 - 883
Published: Feb. 14, 2025
Abstract.
Wetlands
are
major
contributors
to
global
methane
emissions.
However,
their
budget
and
temporal
variability
remain
subject
large
uncertainties.
This
study
develops
the
Satellite-based
Wetland
CH4
model
(SatWetCH4),
which
simulates
wetland
emissions
at
0.25°
×
monthly
resolution,
relying
mainly
on
remote-sensing
products.
In
particular,
a
new
approach
is
derived
assess
substrate
availability,
based
Moderate-Resolution
Imaging
Spectroradiometer
(MODIS)
data.
The
calibrated
using
eddy
covariance
flux
data
from
58
sites,
allowing
for
independence
other
estimates.
At
site
level,
effectively
reproduces
magnitude
seasonality
of
fluxes
in
boreal
temperate
regions
but
shows
limitations
capturing
tropical
sites.
Despite
its
simplicity,
provides
simulations
over
decades
produces
consistent
spatial
patterns
seasonal
variations
comparable
more
complex
land
surface
models
(LSMs).
Such
an
independent
data-driven
products
intended
allow
future
studies
intra-annual
addition,
our
highlights
uncertainties
issues
extent
datasets
need
seamless
satellite-based
future,
there
potential
integrate
this
one-step
into
atmospheric
inversion
frameworks,
thereby
optimization
parameters
concentrations
as
constraints
hopefully
better
estimates
Journal of Advances in Modeling Earth Systems,
Journal Year:
2025,
Volume and Issue:
17(2)
Published: Feb. 1, 2025
Abstract
Accurately
describing
the
distribution
of
in
atmosphere
with
atmospheric
tracer
transport
models
is
essential
for
greenhouse
gas
monitoring
and
verification
support
systems
to
aid
implementation
international
climate
agreements.
Large
deep
neural
networks
are
poised
revolutionize
weather
prediction,
which
requires
3D
modeling
atmosphere.
While
similar
this
regard,
subject
new
challenges.
Both,
stable
predictions
longer
time
horizons
mass
conservation
throughout
need
be
achieved,
while
IO
plays
a
larger
role
compared
computational
costs.
In
study
we
explore
four
different
(UNet,
GraphCast,
Spherical
Fourier
Neural
Operator
SwinTransformer)
have
proven
as
state‐of‐the‐art
prediction
assess
their
usefulness
modeling.
For
this,
assemble
CarbonBench
data
set,
systematic
benchmark
tailored
machine
learning
emulators
Eulerian
transport.
Through
architectural
adjustments,
decouple
performance
our
from
shift
caused
by
steady
rise
.
More
specifically,
center
input
fields
zero
mean
then
use
an
explicit
flux
scheme
fixer
assure
balance.
This
design
enables
conserving
over
6
months
all
network
architectures.
study,
SwinTransformer
displays
particularly
strong
emulation
skill:
90‐day
physically
plausible
multi‐year
forward
runs.
work
paves
way
toward
high
resolution
inverse
inert
trace
gases
networks.
Global Biogeochemical Cycles,
Journal Year:
2025,
Volume and Issue:
39(3)
Published: March 1, 2025
Abstract
Wetlands
are
the
largest
and
most
climate‐sensitive
natural
sources
of
methane.
Accurately
estimating
wetland
methane
emissions
involves
reconciling
inversion
(“top‐down”)
process‐based
(“bottom‐up”)
models
within
global
budget.
However,
estimates
from
these
two
model
types
inherently
interdependent
often
reveal
substantial
discrepancies.
To
enhance
reliability
both
approaches,
we
need
a
comprehensive
understanding
an
independent
high‐resolution
long‐term
flux
data
set.
Here,
employed
data‐driven
random
forest
approach
to
identify
key
variables
influencing
subtropical
freshwater
wetlands
in
Southeastern
United
States.
The
model‐estimated
monthly
mean
fluxes
fit
well
with
measured
(
R
2
=
0.67)
at
four
representative
FLUXNET‐CH4
sites
across
region.
Variable
importance
analysis
highlighted
sensitivity
variations
temperature
water
levels.
High
temperatures
facilitate
methanogenesis
by
enhancing
microbial
activities,
while
elevated
levels
maintain
anaerobic
conditions
necessary
for
production.
Notably,
response
level
fluctuations
is
contingent
on
conditions,
vice
versa.
Moreover,
constructed
first
high‐spatial‐resolution
(∼1
km
×
1
km)
(1982–2010)
gridded
regional
product
States,
annual
region
4.93
±
0.11
Tg
CH
4
yr
−1
1982–2010.
This
new
benchmark
holds
promise
validating
parameterizing
uncertain
emission
processes
bottom‐up
provides
improved
prior
information
top‐down
models.
Global Biogeochemical Cycles,
Journal Year:
2025,
Volume and Issue:
39(4)
Published: April 1, 2025
Abstract
Accurate
accounting
of
greenhouse‐gas
(GHG)
emissions
and
removals
is
central
to
tracking
progress
toward
climate
mitigation
for
monitoring
potential
climate‐change
feedbacks.
GHG
budgeting
reporting
can
follow
either
the
Intergovernmental
Panel
on
Climate
Change
methodologies
National
Greenhouse
Gas
Inventory
(NGHGI)
or
use
atmospheric‐based
“top‐down”
(TD)
inversions
process‐based
“bottom‐up”
(BU)
approaches.
To
help
understand
reconcile
these
approaches,
Second
REgional
Carbon
Cycle
Assessment
Processes
study
(RECCAP2)
was
established
quantify
carbon
dioxide
(CO
2
),
methane
(CH
4
)
nitrous
oxide
(N
O),
ten‐land
five‐ocean
regions
2010–2019.
Here,
we
present
results
North
American
land
region
(Canada,
United
States,
Mexico,
Central
America
Caribbean).
For
2010–2019,
NGHGI
reported
total
net‐GHG
7,270
TgCO
‐eq
yr
−1
compared
TD
estimates
6,132
±
1,846
BU
9,060
898
.
Reconciling
differences
between
NGHGI,
approaches
depended
(a)
lateral
fluxes
CO
along
land‐ocean‐aquatic
continuum
(LOAC)
trade,
(b)
correcting
land‐use
loss‐of‐additional‐sink
capacity
(LASC),
(c)
avoiding
double
counting
inland
water
CH
emissions,
(d)
adjusting
area
match
definition
managed‐land
proxy.
Uncertainties
remain
from
inland‐water
evasion,
conversion
nitrogen
fertilizers
N
O,
less‐frequent
non‐Annex‐1
countries.
The
RECCAP2
framework
plays
a
key
role
in
reconciling
independent
GHG‐reporting
support
policy
commitments
while
providing
insights
into
biogeochemical
processes
responses
change.
Frontiers in Environmental Science,
Journal Year:
2025,
Volume and Issue:
13
Published: April 7, 2025
The
Net
Ecosystem
Carbon
Balance
(NECB)
is
a
crucial
metric
for
understanding
integrated
carbon
dynamics
in
Arctic
and
boreal
regions,
which
are
vital
to
the
global
cycle.
These
areas
associated
with
significant
uncertainties
rapid
climate
change,
potentially
leading
unpredictable
alterations
dynamics.
This
mini-review
examines
key
components
of
NECB,
including
sequestration,
methane
emissions,
lateral
transport,
herbivore
interactions,
disturbances,
while
integrating
insights
from
recent
permafrost
region
greenhouse
gas
budget
syntheses.
We
emphasize
need
holistic
approach
quantify
incorporating
all
their
uncertainties.
review
highlights
methodological
advances
flux
measurements,
improvements
eddy
covariance
automatic
chamber
techniques,
as
well
progress
modeling
approaches
data
assimilation.
Key
research
priorities
identified,
such
improving
representation
inland
waters
process-based
models,
expanding
monitoring
networks,
enhancing
integration
long-term
field
observations
approaches.
efforts
essential
accurately
quantifying
current
future
budgets
rapidly
changing
northern
landscapes,
ultimately
informing
more
effective
change
mitigation
strategies
ecosystem
management
practices.
aligns
goals
Monitoring
Assessment
Program
(AMAP)
Conservation
Flora
Fauna
(CAFF),
providing
important
policymakers,
researchers,
stakeholders
working
understand
protect
these
sensitive
ecosystems.
Earth system science data,
Journal Year:
2025,
Volume and Issue:
17(5), P. 1873 - 1958
Published: May 9, 2025
Abstract.
Understanding
and
quantifying
the
global
methane
(CH4)
budget
is
important
for
assessing
realistic
pathways
to
mitigate
climate
change.
CH4
second
most
human-influenced
greenhouse
gas
in
terms
of
forcing
after
carbon
dioxide
(CO2),
both
emissions
atmospheric
concentrations
have
continued
increase
since
2007
a
temporary
pause.
The
relative
importance
compared
those
CO2
temperature
change
related
its
shorter
lifetime,
stronger
radiative
effect,
acceleration
growth
rate
over
past
decade,
causes
which
are
still
debated.
Two
major
challenges
factors
responsible
observed
arise
from
diverse,
geographically
overlapping
sources
uncertain
magnitude
temporal
destruction
by
short-lived
highly
variable
hydroxyl
radicals
(OH).
To
address
these
challenges,
we
established
consortium
multidisciplinary
scientists
under
umbrella
Global
Carbon
Project
improve,
synthesise,
update
regularly
stimulate
new
research
on
cycle.
Following
Saunois
et
al.
(2016,
2020),
present
here
third
version
living
review
paper
dedicated
decadal
budget,
integrating
results
top-down
emission
estimates
(based
situ
Greenhouse
Gases
Observing
SATellite
(GOSAT)
observations
an
ensemble
inverse-model
results)
bottom-up
process-based
models
estimating
land
surface
chemistry,
inventories
anthropogenic
emissions,
data-driven
extrapolations).
We
recent
2010–2019
calendar
decade
(the
latest
period
full
data
sets
available),
previous
2000–2009
year
2020.
revision
this
2025
edition
benefits
progress
inland
freshwater
with
better
counting
lakes
ponds,
reservoirs,
streams
rivers.
This
also
reduces
double
across
wetland
and,
first
time,
includes
estimate
potential
that
may
exist
(average
23
Tg
yr−1).
Bottom-up
approaches
show
combined
average
248
[159–369]
yr−1
decade.
Natural
fluxes
perturbed
human
activities
through
climate,
eutrophication,
use.
In
estimate,
component
contributing
emissions.
Newly
available
gridded
products
allowed
us
derive
almost
complete
latitudinal
regional
based
approaches.
For
estimated
inversions
(top-down)
be
575
(range
553–586,
corresponding
minimum
maximum
model
ensemble).
Of
amount,
369
or
∼
65
%
attributed
direct
fossil,
agriculture,
waste
biomass
burning
350–391
63
%–68
%).
period,
give
slightly
lower
total
than
2010–2019,
32
9–40).
2020
highest
reaches
608
581–627),
12
higher
2000s.
Since
2012,
trends
been
tracking
scenarios
assume
no
minimal
mitigation
policies
proposed
Intergovernmental
Panel
Climate
Change
(shared
socio-economic
SSP5
SSP3).
methods
suggest
16
(94
yr−1)
larger
(669
yr−1,
range
512–849)
inversion
period.
discrepancy
between
budgets
has
greatly
reduced
differences
(167
156
2020)
respectively),
time
uncertainties
overlap.
Although
bottom-up,
source
uncertainty
attributable
natural
especially
wetlands
freshwaters.
tropospheric
loss
methane,
as
main
contributor
at
563
[510–663]
chemistry–climate
models.
These
values
due
impact
rise
remaining
large
(∼
25
sink
633
[507–796]
554
[550–567]
However,
use
same
OH
distribution,
introduces
less
likely
justified.
agriculture
contributed
228
[213–242]
211
[195–231]
budget.
Fossil
fuel
115
[100–124]
120
[117–125]
Biomass
biofuel
27
[26–27]
28
[21–39]
identify
five
priorities
improving
budget:
(i)
producing
global,
high-resolution
map
water-saturated
soils
inundated
areas
emitting
robust
classification
different
types
ecosystems;
(ii)
further
development
inland-water
emissions;
(iii)
intensification
local
(e.g.
FLUXNET-CH4
measurements,
urban-scale
monitoring,
satellite
imagery
pointing
capabilities)
scales
(surface
networks
remote
sensing
measurements
satellites)
constrain
inversions;
(iv)
improvements
transport
representation
photochemical
sinks
(v)
integration
3D
variational
systems
using
isotopic
and/or
co-emitted
species
such
ethane
well
information
super-emitters
detected
(mainly
oil
sector
but
coal,
landfills)
improve
partitioning.
presented
can
downloaded
https://doi.org/10.18160/GKQ9-2RHT
(Martinez
al.,
2024).
Journal of Geophysical Research Biogeosciences,
Journal Year:
2023,
Volume and Issue:
128(11)
Published: Nov. 1, 2023
Abstract
Process‐based
land
surface
models
are
important
tools
for
estimating
global
wetland
methane
(CH
4
)
emissions
and
projecting
their
behavior
across
space
time.
So
far
there
no
performance
assessments
of
model
responses
to
drivers
at
multiple
time
scales.
In
this
study,
we
apply
wavelet
analysis
identify
the
dominant
scales
contributing
uncertainty
in
frequency
domain.
We
evaluate
seven
23
eddy
covariance
tower
sites.
Our
study
first
characterizes
site‐level
patterns
freshwater
CH
fluxes
(FCH
different
A
Monte
Carlo
approach
was
developed
incorporate
flux
observation
error
avoid
misidentification
that
dominate
error.
results
suggest
(a)
significant
model‐observation
disagreements
mainly
multi‐day
(<15
days);
(b)
most
can
capture
variability
monthly
seasonal
(>32
days)
boreal
Arctic
tundra
sites
but
have
bias
temperate
tropical/subtropical
sites;
(c)
errors
exhibit
increasing
power
spectrum
as
scale
increases,
indicating
biases
<5
days
could
contribute
persistent
systematic
on
longer
scales;
(d)
differences
pattern
related
structure
(e.g.,
proxy
production).
evaluation
suggests
need
accurately
replicate
FCH
variability,
especially
short
scales,
future
developments.
Abstract.
Wetlands
are
the
largest
natural
source
of
methane
(CH4)
emissions
globally.
Northern
wetlands
(>45°
N),
accounting
for
42
%
global
wetland
area,
increasingly
vulnerable
to
carbon
loss,
especially
as
CH4
may
accelerate
under
intensified
high-latitude
warming.
However,
magnitude
and
spatial
patterns
remain
relatively
uncertain.
Here
we
present
estimates
daily
fluxes
obtained
using
a
new
machine
learning-based
upscaling
framework
(WetCH4)
that
applies
most
complete
database
eddy
covariance
(EC)
observations
available
date,
satellite
remote
sensing
informed
environmental
conditions
at
10-km
resolution.
The
important
predictor
variables
included
near-surface
soil
temperatures
(top
40
cm),
vegetation
reflectance,
moisture.
Our
results,
modeled
from
138
site-years
across
26
sites,
had
strong
predictive
skill
with
mean
R2
0.46
0.62
absolute
error
(MAE)
23
nmol
m-2
s-1
21
monthly
fluxes,
respectively.
Based
on
model
estimated
an
annual
average
20.8
±2.1
Tg
yr-1
northern
region
(2016–2022)
total
budgets
ranged
13.7–44.1
yr-1,
depending
map
extents.
Although
86
budget
occurred
during
May–October
period,
considerable
amount
(1.4
±0.2
CH4)
winter.
Regionally,
West
Siberian
accounted
majority
(51
%)
interannual
variation
in
domain
emissions.
Significant
issues
data
coverage
remain,
only
sites
observing
year-round
11
Alaska
10
bog/fen
Canada
Fennoscandia,
general,
Western
Lowlands
underrepresented
by
EC
sites.
results
provide
high
spatiotemporal
information
cycle
possible
responses
climate
change.
Continued,
all-season
tower
improved
moisture
products
needed
future
improvement
upscaling.
dataset
can
be
found
https://doi.org/10.5281/zenodo.10802154
(Ying
et
al.,
2024).