Frontiers in Environmental Science,
Journal Year:
2023,
Volume and Issue:
11
Published: Oct. 25, 2023
Wetlands
act
as
an
important
natural
source
of
global
methane
(CH
4
).
The
emission
rate
wetland
CH
is
jointly
affected
by
climate
change,
carbon
dioxide
(CO
2
)
fertilization,
and
distribution.
In
this
study,
we
implemented
a
module
into
the
Yale
Interactive
Biosphere
(YIBs)
model
to
quantify
spatiotemporal
variations
emissions
in
2001–2020.
Site-level
validations
showed
that
YIBs
reasonably
captures
seasonality
magnitude
at
28
out
33
sites
with
significantly
positive
correlations
low
relative
biases.
On
scale,
predicts
annual
mean
147.5
Tg
yr
−1
2000–2017,
very
close
estimate
147.9
from
ensemble
13
process-based
models.
Global
trend
0.74
−2
past
decades,
leading
increase
7.4
(5.2%)
2008–2017
than
2000–2009.
Climate
change
CO
fertilization
accounted
for
over
70%
changes.
Among
them,
impact
grew
steadily
became
dominant
factor
after
year
2008.
most
significant
changes
were
located
tropical
regions
following
perturbations
temperature
drives
ecosystem
productivity.
We
found
limited
high
latitudes
because
moderate
area
fraction.
rise
poses
emerging
threat
warming
likely
escalates
tropospheric
air
pollutants.
Environmental Research Letters,
Journal Year:
2025,
Volume and Issue:
20(2), P. 023001 - 023001
Published: Jan. 22, 2025
Abstract
Wetlands
are
the
single
largest
natural
source
of
atmospheric
methane
(CH
4
),
contributing
approximately
30%
total
surface
CH
emissions,
and
they
have
been
identified
as
uncertainty
in
global
budget
based
on
most
recent
Global
Carbon
Project
report.
High
uncertainties
bottom–up
estimates
wetland
emissions
pose
significant
challenges
for
accurately
understanding
their
spatiotemporal
variations,
scientific
community
to
monitor
from
space.
In
fact,
there
large
disagreements
between
versus
top–down
inferred
inversion
concentrations.
To
address
these
critical
gaps,
we
review
development,
validation,
applications
well
how
used
inversions.
These
estimates,
using
(1)
empirical
biogeochemical
modeling
(e.g.
WetCHARTs:
125–208
TgCH
yr
−1
);
(2)
process-based
WETCHIMP:
190
±
39
(3)
data-driven
machine
learning
approach
UpCH4:
146
43
).
Bottom–up
subject
(∼80
Tg
ranges
different
do
not
overlap,
further
amplifying
overall
when
combining
multiple
data
products.
substantial
highlight
gaps
our
biogeochemistry
inundation
dynamics.
Major
tropical
arctic
complexes
regional
hotspots
emissions.
However,
scarcity
satellite
over
tropics
northern
high
latitudes
offer
limited
information
inversions
improve
estimates.
Recent
advances
measurements
fluxes
FLUXNET-CH
)
across
a
wide
range
ecosystems
including
bogs,
fens,
marshes,
forest
swamps
provide
an
unprecedented
opportunity
existing
We
suggest
that
continuous
long-term
at
representative
wetlands,
fidelity
mapping,
combined
with
appropriate
framework,
will
be
needed
significantly
There
is
also
pressing
unmet
need
fine-resolution
high-precision
observations
directed
wetlands.
Nature,
Journal Year:
2023,
Volume and Issue:
616(7958), P. 740 - 746
Published: April 5, 2023
Tropical
peatlands
cycle
and
store
large
amounts
of
carbon
in
their
soil
biomass1-5.
Climate
land-use
change
alters
greenhouse
gas
(GHG)
fluxes
tropical
peatlands,
but
the
magnitude
these
changes
remains
highly
uncertain6-19.
Here
we
measure
net
ecosystem
exchanges
dioxide,
methane
nitrous
oxide
between
October
2016
May
2022
from
Acacia
crassicarpa
plantation,
degraded
forest
intact
within
same
peat
landscape,
representing
land-cover-change
trajectories
Sumatra,
Indonesia.
This
allows
us
to
present
a
full
plantation
rotation
GHG
flux
balance
fibre
wood
on
peatland.
We
find
that
has
lower
emissions
than
site
with
similar
average
groundwater
level
(GWL),
despite
more
intensive
land
use.
The
over
(35.2
±
4.7
tCO2-eq
ha-1
year-1,
standard
deviation)
were
around
two
times
higher
those
(20.3
3.7
year-1),
only
half
current
Intergovernmental
Panel
Change
(IPCC)
Tier
1
emission
factor
(EF)20
for
this
Our
results
can
help
reduce
uncertainty
estimates,
provide
an
estimate
impact
develop
science-based
peatland
management
practices
as
nature-based
climate
solutions.
Journal of Geophysical Research Biogeosciences,
Journal Year:
2023,
Volume and Issue:
128(7)
Published: July 1, 2023
Abstract
Mineral
binding
of
organic
carbon
(OC)
is
one
the
key
mechanisms
promoting
soil
(SOC)
persistence,
which
vital
for
long‐term
sequestration
atmospheric
dioxide
into
soils.
However,
relative
importance
two
main
types
minerals
‐
metal
oxides
and
silicate
clay—in
SOC
protection
remains
unclear,
hampering
our
ability
to
predict
protect
this
important
pool
persistent
SOC.
Here,
we
analyzed
OC
bound
(OC
)
versus
clay
in
soils
from
contrasting
environments
(i.e.,
wetlands
uplands)
using
sequential
dissolution
by
dithionite
hydrofluoric
acid.
We
found
that
%
was
higher
than
both
uplands,
indicating
dominance
protection.
The
sum
constituted
a
fraction
suggesting
an
underappreciated
role
mineral
(in
particular,
oxide)
wetland
preservation.
Furthermore,
lignin
phenol
analysis
tandem,
∼23%
phenols
were
additionally
released
after
removal
clay,
providing
potential
means
assess
“hidden”
matrices.
Given
wide
use
as
tracers
terrestrial
plant‐derived
OC,
results
suggest
contribution
or
sedimentary
stocks
mineral‐protected
deserves
reassessment.
These
findings
highlight
differential
various
its
components
environments,
warrants
better
recognition
understanding
distribution
dynamics
Atmospheric Environment X,
Journal Year:
2023,
Volume and Issue:
21, P. 100223 - 100223
Published: Nov. 15, 2023
Early
control
of
atmospheric
methane
is
essential
to
achieving
a
1.5
°C
warming
pathway.
This
paper
considers
range
academic
and
gray
literature
reviews
techniques,
as
starting
point
for
more
comprehensive,
integrative
review.
Novel
approaches
are
considered
across
anthropogenic
natural
sources;
where
these
lacking,
existing
discussed.
review
identifies
four
principal
sectors
meriting
action
research:
fugitive
emissions
in
mining,
oil
&
gas;
agriculture,
including
near-term
minor
interventions
later
synthetic
food
production;
best
practice
municipal
solid
waste
wastewater
management;
sources
(e.g.,
permafrost,
clathrates,
wetlands).
Where
abatement
impractical,
this
discusses
speculative
geoengineering
technologies
enhancing
the
•OH
•Cl
sinks,
photocatalysis,
adsorbent
air
capture).
Atmospheric
removal
proposals
merit
research,
but
may
remain
impractical
due
concentrations
lifetime.
Carbon Management,
Journal Year:
2023,
Volume and Issue:
14(1)
Published: Nov. 1, 2023
Peatlands
are
a
globally
important
carbon
store,
but
peatland
ecosystems
from
high
latitudes
to
the
tropics
highly
degraded
due
increasingly
intensive
anthropogenic
activity,
making
them
significant
greenhouse
gas
(GHG)
sources.
Peatland
restoration
and
conservation
have
been
proposed
as
nature-based
solution
climate
change,
by
restoring
function
of
peatlands
net
sink,
this
may
implications
for
many
local
communities
who
rely
on
income
activities
associated
with
transformed
peatlands,
particularly
those
drained
agriculture.
However,
without
changing
way
that
humans
interact
exploit
in
most
regions,
will
continue
degrade
be
lost.
We
propose
there
ultimately
three
potential
trajectories
management:
business
usual,
whereby
sink
capacity
continues
eroded,
responsible
agricultural
management
(with
mitigate
emissions,
unlikely
restore
sink),
conservation.
term
three-peat
challenge,
it
means
view
benefits
environment,
well
such
transitions
ecosystem
services
(particularly
provisioning)
consequences
arising
lack
action.
Ultimately,
decisions
regarding
which
given
localities
follow
torequire
principles
equitable
decision-making,
support
ensure
just
transitions,
their
livelihoods.
PNAS Nexus,
Journal Year:
2024,
Volume and Issue:
3(4)
Published: March 28, 2024
Restoring
wetlands
will
reduce
nitrogen
contamination
from
excess
fertilization
but
estimates
of
the
efficacy
strategy
vary
widely.
The
intervention
is
often
described
as
effective
for
reducing
export
watersheds
to
mediate
bottom-level
hypoxia
threatening
marine
ecosystems.
Other
research
points
necessity
applying
a
suite
interventions,
including
wetland
restoration
mitigate
meaningful
quantities
export.
Here,
we
use
process-based
physical
modeling
evaluate
effects
two
hypothetical,
plausible
large-scale
programs
intended
nutrient
Gulf
Mexico.
We
show
that
full
adoption
currently
in
place
can
meet
little
10%
much
60%
reduction
targets
Mexico
dead
zone.
These
reductions
are
lower
than
prior
three
reasons.
First,
net
storage
leachate
subsurface
precludes
interception
and
thereby
dampens
percent
decline
caused
by
policy.
Unlike
previous
studies,
first
constrained
riverine
fluxes
match
observed
throughout
basin.
Second,
locations
many
restorable
lands
geographically
disconnected
heavily
fertilized
croplands,
limiting
runoff.
Third,
daily
resolution
model
simulations
captured
seasonal
stormflow
dynamics
inhibit
removal
because
peak
effectiveness
does
not
coincide
with
timing
inputs.
To
improve
health
efforts
eliminate
nutrient,
loading
should
be
implemented
beyond
field-margin
strategies
investigated
here.
Agricultural Water Management,
Journal Year:
2024,
Volume and Issue:
296, P. 108806 - 108806
Published: April 1, 2024
Irrigation
can
increase
crop
yields
and
could
be
a
key
climate
adaptation
strategy.
At
present,
under
the
background
of
increasing
food
demand
continuous
expansion
irrigation
cropland,
there
still
uncertainties
about
soil
carbon
dynamics
change
water
volume
irrigated
area
in
view
large-scale
spatial
heterogeneity.
Therefore,
this
paper
uses
space-for-time
+
meta-analysis
two-step
methodology
based
on
residual
trend
analysis
to
quantitatively
analyze
relationship
between
organic
(SOC)
respiration
(Rs)
response
fluctuations
land
extents.
Here
we
show
that
within
100–1000
mm
had
negative
impact
SOC,
was
correlated
with
volume.
Different
levels
manifest
distinct
effects
SOC
content
across
varying
depths.
When
quantities
are
less
than
700
mm,
0–30
cm
depth
layer
surpasses
30–200
layer.
Conversely,
when
equal
or
exceed
pattern
is
reversed.
The
overall
stock
at
0–200
−14.88±6.7%.
Tillage,
planting
intensity,
topography,
type
cropland
all
exert
variable
impacts
content.
Whether
these
influences
deleterious
beneficial
hinges
predominantly
upon
balance
augmentation
due
heightened
inputs
from
crops
reduction
through
alterations
microbial
activity.
Mann-Kendall
showed
2000
2015,
Rs
an
trend,
rate
3.67
g/m2/year.
global
mainly
driven
by
factors
(temperature,
precipitation
solar
radiation),
while
decrease
small
number
areas
management
practices
(fertilizer
nitrogen,
irrigation,
tillage).
Our
study
further
quantifies
dynamics,
thereby
offering
potential
pathways
data
support
for
advancement
sustainable
agriculture.