Inland Waters,
Journal Year:
2025,
Volume and Issue:
unknown, P. 1 - 53
Published: Feb. 3, 2025
Methane
emissions
from
lakes
will
increase
with
climate
warming.
However,
these
are
not
accounted
for
in
the
land
surface
schemes
of
Global
Climate
Models
(GCMs).
Because
projections
depend
on
future
atmospheric
CH4
concentrations,
positive
feedback
loop
between
and
warming
is
simulated.
To
address
this
issue,
our
objective
was
to
develop
a
modelling
approach
where
an
arctic-lake
emission
model
forced
directly
GCM
output
(no
downscaling)
formulated
parameters
that
generally
available
within
framework.
This
enable
lake-model
coupling.
The
hindcast
1976-2005
forecast
2071-2100.
Using
observed
meteorological
forcing,
hindcasts
had
cold
bias
(-0.15
-0.63
°C)
root-mean-square
error
(RMSE)
0.38
0.90
°C,
relative
observations.
GCM-forced
warm
(+0.96
+3.13°C)
RMSE
1.03
3.50
°C.
Our
diffusion
parameterization
transferable
four
Alaskan
lakes,
after
local
adjustment
wind
drag,
but
different
ebullition
parameterizations
were
required
two
deeper
versus
shallower
lakes.
Under
three
scenarios,
we
simulated
lake-bottom
water
by
up
2.24°C,
increasing
flux
38-129%.
limited
availability
data
renders
results
poorly
validated.
Therefore,
should
be
considered
as
proof-of-concept
pathway
toward
direct
coupling
lake-models
GCMs.
Rigorous
validation
would
require
additional
timeseries
observations
areal
free-surface
diffusive
ebullitive
fluxes
Earth system science data,
Journal Year:
2023,
Volume and Issue:
15(3), P. 1197 - 1268
Published: March 21, 2023
Abstract.
Knowledge
of
the
spatial
distribution
fluxes
greenhouse
gases
(GHGs)
and
their
temporal
variability
as
well
flux
attribution
to
natural
anthropogenic
processes
is
essential
monitoring
progress
in
mitigating
emissions
under
Paris
Agreement
inform
its
global
stocktake.
This
study
provides
a
consolidated
synthesis
CH4
N2O
using
bottom-up
(BU)
top-down
(TD)
approaches
for
European
Union
UK
(EU27
+
UK)
updates
earlier
syntheses
(Petrescu
et
al.,
2020,
2021).
The
work
integrates
updated
emission
inventory
data,
process-based
model
results,
data-driven
sector
results
inverse
modeling
estimates,
it
extends
previous
period
1990–2017
2019.
BU
TD
products
are
compared
with
national
gas
inventories
(NGHGIs)
reported
by
parties
United
Nations
Framework
Convention
on
Climate
Change
(UNFCCC)
2021.
Uncertainties
NGHGIs,
UNFCCC
EU
member
states,
also
included
synthesis.
Variations
estimates
produced
other
methods,
such
atmospheric
inversion
models
or
spatially
disaggregated
datasets
(BU),
arise
from
diverse
sources
including
within-model
uncertainty
related
parameterization
structural
differences
between
models.
By
comparing
NGHGIs
approaches,
activities
key
source
bias
e.g.,
fluxes,
which
inversions
sensitive
prior
geospatial
emissions.
For
emissions,
over
2015–2019
period,
covers
sufficiently
robust
number
overlapping
most
importantly
directly
comparable,
accounting
mean
20.5
Tg
yr−1
(EDGARv6.0,
last
year
2018)
18.4
(GAINS,
2015),
close
NGHGI
17.5±2.1
yr−1.
give
higher
they
detect
Over
same
high-resolution
regional
report
34
Coarser-resolution
global-scale
result
23
24
inferred
GOSAT
surface
(SURF)
network
measurements,
respectively.
magnitude
peatland
mineral
soil
JSBACH–HIMMELI
model,
rivers,
lake
reservoir
geological
sources,
biomass
burning
together
could
account
gap
8
both
(EDGARv6.0
GAINS)
value
0.9
yr−1,
data
(0.8±55
%
yr−1).
was
1.4
(excluding
TOMCAT,
no
data).
comparison
method
defined
this
can
be
operationalized
future
annual
calculation
budgets
at
EU27
scales.
Future
comparability
will
enhanced
further
steps
involving
analysis
finer
resolutions
estimation
intra-annual
timescales,
great
importance
N2O,
may
help
identify
contributions
divergence
posterior
and/or
inter-annual
scale.
Even
if
currently
highly
uncertain
because
large
spread
observations
represent
independent
against
totals
compared.
With
anticipated
improvements
observations,
arguably
emerge
powerful
tool
verifying
CH4,
GHGs.
referenced
figures
visualized
https://doi.org/10.5281/zenodo.7553800
2023).
Environmental Research Letters,
Journal Year:
2023,
Volume and Issue:
18(9), P. 094025 - 094025
Published: July 28, 2023
Abstract
Carbon
dioxide
(CO
2
)
and
methane
(CH
4
emissions
from
freshwater
ecosystems
are
predicted
to
increase
under
climate
warming.
However,
in
glacierized
regions
differ
critically
those
non-glacierized
regions.
The
potential
of
CO
CH
environments
the
Tibetan
Plateau
(TP)
were
only
recently
recognized.
Here,
first
direct
measurement
emission
fluxes
isotopic
composition
during
spring
2022
13
glacial
lakes
TP
revealed
that
previously
overlooked
sinks
due
chemical
weathering
daily
average
flux
was
−5.1
±
4.4
mmol
m
−2
d
−1
,
consumption
could
reach
38.9
Gg
C-CO
yr
by
all
TP.
This
might
be
larger
summer
when
glaciers
experience
intensive
melting,
highlighting
importance
uptake
on
global
carbon
cycle.
studied
sources
with
total
ranging
3.3
4082.5
795.6
μ
mol
.
large
range
attributed
ebullition
found
three
lakes.
Low
dissolved
organic
concentrations
oxidation
responsible
for
low
diffusive
without
ebullition.
In
addition,
groundwater
input
alter
probably
had
a
thermogenic
source;
whereas
influenced
mainly
atmospheric
input,
as
well
matter
remineralization
oxidation.
Overall,
play
an
important
role
cycle
budget,
more
detailed
microbial
studies
needed
constrain
contributions
different
pathways
production,
emissions.
Science Advances,
Journal Year:
2024,
Volume and Issue:
10(39)
Published: Sept. 27, 2024
Climate-sensitive
northern
cryosphere
inland
waters
emit
greenhouse
gases
(GHGs)
into
the
atmosphere,
yet
their
total
emissions
remain
poorly
constrained.
We
present
a
data-driven
synthesis
of
GHG
from
considering
water
body
types,
zones,
and
seasonality.
find
that
annual
are
dominated
by
carbon
dioxide
(
1149.21004.81307.5
teragrams
CO
2
;
medianQ13
)
methane
14.210.118.5
CH
4
),
while
nitrous
oxide
emission
5.4−1.412.2
gigagrams
N
O)
is
minor.
The
–equivalent
(CO
e)
1.51.31.8
or
2.32.8
petagrams
e
using
100-
20-year
global
warming
potentials,
respectively.
Rivers
64%
more
GHGs
than
lakes,
despite
having
only
one-fifth
surface
area.
continuous
permafrost
zone
contributed
half
emissions.
Annual
exceed
region’s
terrestrial
net
ecosystem
exchange,
highlighting
important
role
in
cryospheric
land-aquatic
continuum
under
climate.
Journal of Geophysical Research Biogeosciences,
Journal Year:
2023,
Volume and Issue:
128(3)
Published: March 1, 2023
Abstract
Freshwater
ecosystem
contributions
to
the
global
methane
budget
remains
most
uncertain
among
natural
sources.
With
warming
and
accompanying
carbon
release
from
thawed
permafrost
thermokarst
lake
expansion,
increase
of
emissions
could
be
large.
However,
impact
relative
importance
various
factors
related
remain
uncertain.
Based
on
diverse
characteristics
incorporated
in
modeling
observational
data,
we
calibrate
verify
a
biogeochemistry
model.
The
model
is
then
applied
estimate
examine
impacts
temperature
for
first
last
decades
21st
century
under
different
climate
scenarios.
We
find
that
current
are
24.0
±
8.4
Tg
CH
4
yr
−1
lakes
larger
than
0.1
km
2
,
accounting
11%
total
source
as
estimated
based
atmospheric
inversion.
Future
projections
RCP8.5
scenario
suggest
58%–86%
growth
lakes.
Our
sensitivity
analysis
indicates
additional
substrates
thawing
may
enhance
production
Arctic.
Warming
enhanced
oxidation
water
can
an
effective
sink
reduce
net
Environmental Science & Technology,
Journal Year:
2023,
Volume and Issue:
57(36), P. 13520 - 13529
Published: Aug. 31, 2023
Lakes
are
major
emitters
of
methane
(CH4);
however,
a
longstanding
challenge
with
quantifying
the
magnitude
emissions
remains
as
result
large
spatial
and
temporal
variability.
This
study
was
designed
to
address
issue
using
satellite
remote
sensing
advantages
coverage
resolution.
Using
Aqua/MODIS
imagery
(2003–2020)
in
situ
measured
data
(2011–2017)
eutrophic
Lake
Taihu,
we
compared
performance
eight
machine
learning
models
predict
diffusive
CH4
found
that
random
forest
(RF)
model
achieved
best
fitting
accuracy
(R2
=
0.65
mean
relative
error
21%).
On
basis
input
variables
(chlorophyll
a,
water
surface
temperature,
diffuse
attenuation
coefficient,
photosynthetically
active
radiation),
assessed
how
why
they
help
RF
model.
Overall,
these
mechanistically
controlled
emissions,
leading
capturing
well
variability
from
lake.
Additionally,
climate
warming
associated
algal
blooms
boosted
long-term
increase
via
reconstructing
historical
daily
time
series
emissions.
demonstrates
great
potential
satellites
map
lake
by
providing
spatiotemporal
continuous
data,
new
timely
insights
into
accurately
understanding
aquatic
greenhouse
gas
Freshwater Biology,
Journal Year:
2023,
Volume and Issue:
69(1), P. 143 - 156
Published: Nov. 15, 2023
Abstract
Greenhouse
gas
(GHG)
emissions
from
drained
peatlands
have
been
studied
extensively.
Considerably
less
attention
has
paid
to
the
ditches
used
drain
peatlands.
High
within‐ditch
GHG
production
and
lateral
inflow
of
GHGs
may
lead
emitting
considerable
amounts
on
landscape
scale.
We
quantified
annual
ebullitive
diffusive
methane
(CH
4
),
carbon
dioxide
(CO
2
nitrous
oxide
(N
O)
in
10
drainage
intensively
temperate
for
dairy
farming,
The
Netherlands.
Additionally,
we
assessed
water
sediment
quality
determine
proxies
via
two
emission
pathways.
mean
varied
between
3.57
60.1
g
CO
‐eq.
m
−2
day
−1
(based
a
global
warming
potential
over
100‐year
timeframe),
where
contributed
average
43%
(ranging
1.9
22.0
)
CH
16%
(0.1–16.5
total
emission.
Ebullition
made
up
nearly
half
(40%,
1.3–40.9
).
N
O
were
mostly
low.
higher
winter
months,
while
ebullition
was
during
spring
summer.
Diffusive
did
not
show
seasonal
pattern.
factor,
estimate
per
unit
area
(EF),
2144
kg
ha
year
,
which
is
times
than
tier
1
EF
reported
by
IPCC
(with
underrepresented
data),
underlining
high
variability
ditch
emissions.
Ditch
also
surrounding
indicating
that
can
be
important
scale
should
considered
included
national
greenhouse
reporting.