Natural Resources Forum,
Journal Year:
2024,
Volume and Issue:
unknown
Published: Jan. 4, 2024
Abstract
The
2030
United
Nations
Sustainable
Development
Goals
(SDG)
Target
3.9
aims
to
“
reduce
the
number
of
deaths
and
illnesses
from
hazardous
chemicals
air
,
water
soil
pollution
contamination.
”
Methane
belongs
class
greenhouse
gases
it
is
a
harmful
ambient
atmospheric
pollutant
with
adverse
effects
on
human
health.
Hence,
this
paper
aligns
SDG
3
11
analyze
impact
methane
emissions
infant
mortality
rate
in
Europe.
Using
an
unbalanced
panel
data
53
European
countries
1990
2018,
we
probe
if
differs
by
union
membership.
Consistent
findings
static
dynamic
techniques
reveal
that:
exhibit
mortality‐inducing
properties
full
sample,
Union
(EU)
non‐EU
0.041%,
0.037%,
0.047%,
respectively;
EU
show
lower
rates
relative
−0.164%;
persistent.
Additional
sensitivity
checks
including
nitrous
oxide
as
regressor
indicates
that
picks
up
due
collinearity
(in
analysis)
but
aggravating
upheld
model.
Likewise,
results
are
sustained
when
control
for
outliers
excluding
Russia
(the
largest
emitter
Europe)
robustness
using
under‐5
uphold
mortality‐increasing
effect
emissions.
Based
our
empirical
investigations,
adequate
policy
recommendations
provided
help
stemming
environment
such
reduces
its
These
outcomes
enrich
health
economics
child
literature,
discussed.
Abstract.
Understanding
and
quantifying
the
global
methane
(CH4)
budget
is
important
for
assessing
realistic
pathways
to
mitigate
climate
change.
Emissions
atmospheric
concentrations
of
CH4
continue
increase,
maintaining
as
second
most
human-influenced
greenhouse
gas
in
terms
forcing
after
carbon
dioxide
(CO2).
The
relative
importance
compared
CO2
temperature
change
related
its
shorter
lifetime,
stronger
radiative
effect,
acceleration
growth
rate
over
past
decade,
causes
which
are
still
debated.
Two
major
challenges
reducing
uncertainties
factors
explaining
well-observed
arise
from
diverse,
geographically
overlapping
sources
uncertain
magnitude
temporal
destruction
by
short-lived
highly
variable
hydroxyl
radicals
(OH).
To
address
these
challenges,
we
have
established
a
consortium
multi-disciplinary
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
in-situ
observing
satellite
(GOSAT)
observations
an
ensemble
inverse-model
results)
bottom-up
process-based
models
estimating
land-surface
emissions
chemistry,
inventories
anthropogenic
emissions,
data-driven
extrapolations).
We
recent
2010–2019
calendar
decade
(the
latest
period
full
datasets
available),
previous
2000–2009
year
2020.
revision
this
edition
benefits
progress
inland
freshwater
with
better
accounting
lakes
ponds,
reservoirs,
streams
rivers.
This
also
reduces
double
across
wetland
and,
first
time,
includes
estimate
potential
that
exists
(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,
land
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).
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
respectively),
time
uncertainty
overlap.
distribution
inversion-based
indicates
predominance
tropical
southern
hemisphere
(~65
<30°
N)
mid
(30°
N–60°
N,
~30
emissions)
high-northern
latitudes
(60°
N–90°
~4
emissions).
similar
though
contributions
latitudes,
smaller
tropics
inversions.
Although
bottom-up,
source
attributable
natural
especially
those
wetlands
freshwaters.
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
at
local
(e.g.,
FLUXNET-CH4
measurements,
urban-scale
monitoring,
imagery
pointing
capabilities)
scales
(surface
networks
remote
sensing
measurements
satellites)
constrain
both
inversions;
iv)
improvements
transport
representation
photochemical
sinks
inversions,
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.
data
presented
can
downloaded
https://doi.org/10.18160/GKQ9-2RHT
(Martinez
al.,
2024).
Journal of Geophysical Research Biogeosciences,
Journal Year:
2024,
Volume and Issue:
129(3)
Published: Feb. 26, 2024
Abstract
Significant
progress
in
permafrost
carbon
science
made
over
the
past
decades
include
identification
of
vast
stocks,
development
new
pan‐Arctic
maps,
an
increase
terrestrial
measurement
sites
for
CO
2
and
methane
fluxes,
important
factors
affecting
cycling,
including
vegetation
changes,
periods
soil
freezing
thawing,
wildfire,
other
disturbance
events.
Process‐based
modeling
studies
now
key
elements
cycling
advances
statistical
inverse
enhance
understanding
region
C
budgets.
By
combining
existing
data
syntheses
model
outputs,
is
likely
a
wetland
source
small
ecosystem
sink
with
lower
net
uptake
toward
higher
latitudes,
excluding
wildfire
emissions.
For
2002–2014,
strongest
was
located
western
Canada
(median:
−52
g
m
−2
y
−1
)
smallest
sinks
Alaska,
Canadian
tundra,
Siberian
tundra
(medians:
−5
to
−9
).
Eurasian
regions
had
largest
median
fluxes
(16–18
CH
4
Quantifying
regional
scale
balance
remains
challenging
because
high
spatial
temporal
variability
relatively
low
density
observations.
More
accurate
require:
(a)
better
maps
characterizing
wetlands
dynamics
disturbances,
abrupt
thaw;
(b)
establishment
year‐round
flux
underrepresented
areas;
(c)
improved
models
that
represent
cycle
dynamics,
non‐growing
season
emissions
effects.
The Science of The Total Environment,
Journal Year:
2024,
Volume and Issue:
922, P. 171218 - 171218
Published: Feb. 27, 2024
Freshwater
wetlands
have
a
disproportionately
large
influence
on
the
global
carbon
cycle,
with
potential
to
serve
as
long-term
sinks.
Many
of
world's
freshwater
been
destroyed
or
degraded,
thereby
affecting
carbon-sink
capacity.
Ecological
restoration
degraded
is
thus
becoming
an
increasingly
sought-after
natural
climate
solution.
Yet
time
required
revert
wetland
from
source
sink
remains
largely
unknown.
Moreover,
increased
methane
(CH4)
and
nitrous
oxide
(N2O)
emissions
might
complicate
benefit
that
may
represent.
We
conducted
meta-analysis
evaluate
benefits
in
terms
net
ecosystem
greenhouse
gas
balance.
Most
studies
(76
%)
investigated
peatlands
(bogs,
fens,
peat
swamps)
northern
hemisphere,
whereas
effects
non-peat
(freshwater
marshes,
swamps,
riparian
wetlands)
remain
unexplored.
Despite
higher
CH4
emissions,
most
restored
(77
all
were
sinks,
(69
sources.
Conversely,
similar
across
restored,
wetlands.
When
considering
radiative
forcings
atmospheric
lifetimes
different
gases,
average
for
cooling
effect
after
525
years
141
The
does,
therefore,
not
meet
timeframe
set
by
Paris
Agreement
limit
warming
2100.
conservation
protection
should
be
prioritised
over
those
ecosystems
already
play
key
role
change
mitigation.
Frontiers in Water,
Journal Year:
2024,
Volume and Issue:
5
Published: Jan. 17, 2024
Freshwater
ecosystems,
including
lakes,
wetlands,
and
running
waters,
are
estimated
to
contribute
over
half
the
natural
emissions
of
methane
(CH
4
)
globally,
yet
large
uncertainties
remain
in
inland
water
CH
budget.
These
related
highly
heterogeneous
nature
complex
regulation
emission
pathways,
which
involve
diffusion,
ebullition,
plant-associated
transport.
The
latter,
particular,
represents
a
major
source
uncertainty
our
understanding
dynamics.
Many
freshwater
ecosystems
harbor
habitats
colonized
by
submerged
emergent
plants,
transport
variable
amounts
atmosphere
but
whose
presence
may
also
profoundly
influence
local
Yet,
dynamics
vegetated
their
potential
contribution
budgets
waters
understudied
poorly
quantified.
Here
we
present
synthesis
literature
pertaining
habitats,
(i)
provide
an
overview
different
ways
aquatic
vegetation
can
(i.e.,
production,
oxidation,
transport)
(ii)
summarize
methods
applied
study
fluxes
from
(iii)
existing
data
on
associated
types
waters.
Finally,
discuss
implications
with
for
current
estimates
at
global
scale.
plant
areas
varied
widely,
ranging
from−8.6
2835.8
mg
m
−2
d
−1
,
were
average
high
relative
non-vegetated
habitats.
We
conclude
that,
based
coverage
flux
intensities
fluxes,
exclusion
these
lake
balances
lead
underestimation
emissions.
This
highlights
need
incorporate
into
further
identifies
research
aspects
relevant
future
directions.
Global Change Biology,
Journal Year:
2024,
Volume and Issue:
30(2)
Published: Feb. 1, 2024
Abstract
Wetlands
are
the
largest
natural
source
of
methane
(CH
4
)
globally.
Climate
and
land
use
change
expected
to
alter
CH
emissions
but
current
future
wetland
budgets
remain
uncertain.
One
important
predictor
flux,
plants,
play
an
role
in
providing
substrates
for
‐producing
microbes,
increasing
consumption
by
oxygenating
rhizosphere,
transporting
from
soils
atmosphere.
Yet,
there
various
mechanistic
knowledge
gaps
regarding
extent
which
plant
root
systems
their
traits
influence
emissions.
Here,
we
present
a
novel
conceptual
framework
relationships
between
range
processes
wetlands.
Based
on
literature
review,
propose
four
main
‐relevant
categories
function:
gas
transport,
carbon
substrate
provision,
physicochemical
influences
system
architecture.
Within
these
categories,
discuss
how
individual
production,
consumption,
transport
(PCT).
Our
findings
reveal
concerning
trait
functions
influences,
mycorrhizae
temporal
dynamics
PCT.
We
also
identify
priority
research
needs
such
as
integrating
measurements
different
function
measuring
root‐CH
linkages
along
environmental
gradients,
following
standardized
ecology
protocols
vocabularies.
Thus,
our
identifies
relevant
belowground
that
will
help
improve
predictions
reduce
uncertainties
budgets.
Biogeosciences,
Journal Year:
2024,
Volume and Issue:
21(1), P. 93 - 107
Published: Jan. 3, 2024
Abstract.
Shallow
lakes
and
ponds
undergo
frequent
temporary
thermal
stratification.
How
this
affects
greenhouse
gas
(GHG)
emissions
is
moot,
with
both
increased
reduced
GHG
hypothesised.
Here,
weekly
estimations
of
emissions,
over
the
growing
season
from
May
to
September,
were
combined
temperature
oxygen
profiles
an
11
ha
temperate
shallow
lake
investigate
how
stratification
shapes
emissions.
There
three
main
periods
profound
anoxia
occurring
in
bottom
waters
upon
isolation
atmosphere.
Average
diffusive
methane
(CH4)
nitrous
oxide
(N2O)
larger
more
variable
stratified
phase,
whereas
carbon
dioxide
(CO2)
was
on
average
lower,
though
these
differences
not
statistically
significant.
In
contrast,
there
a
significant
order
magnitude
increase
CH4
ebullition
phase.
Furthermore,
at
end
period
stratification,
large
efflux
CO2
as
mixed.
Two
relatively
isolated
turnover
events
estimated
have
released
majority
emitted
between
September.
These
results
demonstrate
patterns
can
shape
highlight
role
need
for
high-frequency
measurements
which
are
required
accurately
characterise
particularly
temporarily
stratifying
lakes.
Biogeosciences,
Journal Year:
2025,
Volume and Issue:
22(1), P. 305 - 321
Published: Jan. 15, 2025
Abstract.
Due
to
ongoing
climate
change,
methane
(CH4)
emissions
from
vegetated
wetlands
are
projected
increase
during
the
21st
century,
challenging
mitigation
efforts
aimed
at
limiting
global
warming.
However,
despite
reports
of
rising
emission
trends,
a
comprehensive
evaluation
and
attribution
recent
changes
remains
limited.
Here
we
assessed
wetland
CH4
2000–2020
based
on
an
ensemble
16
process-based
models.
Our
results
estimated
average
158
±
24
(mean
1σ)
Tg
yr−1
over
total
annual
area
8.0
2.0×106
km2
for
period
2010–2020,
with
6–7
in
2010–2019
compared
2000–2009.
The
increases
four
latitudinal
bands
90–30°
S,
30°
S–30°
N,
30–60°
60–90°
N
were
0.1–0.2,
3.6–3.7,
1.8–2.4,
0.6–0.8
yr−1,
respectively,
2
decades.
modeled
sensitivities
temperature
show
reasonable
consistency
eddy-covariance-based
measurements
34
sites.
Rising
was
primary
driver
increase,
while
precipitation
atmospheric
CO2
concentrations
played
secondary
roles
high
levels
uncertainty.
These
suggest
that
change
is
driving
increased
direct
sustained
needed
monitor
developments.
Abstract
Agricultural
ponds
have
some
of
the
highest
methane
emissions
per
area
among
freshwater
systems,
and
these
anthropogenic
should
be
included
in
national
greenhouse
gas
inventories.
Here
we
deliver
a
continental-scale
assessment
from
agricultural
United
States
Australia.
We
source
maps
ponds,
compile
meta-analysis
for
their
use
published
data
to
correct
temperature
relative
contributions
two
fluxes
(diffusion
ebullition).
In
States,
2.56
million
cover
420.9
kha
emit
about
95.8
kt
year
−1
methane.
Australia,
1.76
291.2
75.1
Despite
large
uncertainties,
our
findings
suggest
that
small
water
bodies
twice
as
much
than
is
currently
accounted
Managing
systems
can
reduce
while
benefiting
productivity,
ecosystem
services,
biodiversity.