Science,
Journal Year:
2025,
Volume and Issue:
387(6740), P. 1291 - 1295
Published: March 20, 2025
Terrestrial
sequestration
of
carbon
has
mitigated
≈30%
anthropogenic
emissions.
However,
its
distribution
across
different
pools,
live
or
dead
biomass
and
soil
sedimentary
organic
carbon,
remains
uncertain.
Analyzing
global
observational
datasets
changes
in
terrestrial
we
found
that
≈35
±
14
gigatons
(GtC)
have
been
sequestered
on
land
between
1992
2019,
whereas
changed
by
≈1
7
GtC.
Global
vegetation
models
instead
imply
mostly
biomass.
We
identify
key
processes
not
included
most
can
explain
this
discrepancy.
Most
gains
are
as
nonliving
matter
thus
more
persistent
than
previously
appreciated,
with
a
substantial
fraction
linked
to
human
activities
such
river
damming,
wood
harvest,
garbage
disposal
landfills.
Earth system science data,
Journal Year:
2022,
Volume and Issue:
14(11), P. 4811 - 4900
Published: Nov. 11, 2022
Abstract.
Accurate
assessment
of
anthropogenic
carbon
dioxide
(CO2)
emissions
and
their
redistribution
among
the
atmosphere,
ocean,
terrestrial
biosphere
in
a
changing
climate
is
critical
to
better
understand
global
cycle,
support
development
policies,
project
future
change.
Here
we
describe
synthesize
data
sets
methodologies
quantify
five
major
components
budget
uncertainties.
Fossil
CO2
(EFOS)
are
based
on
energy
statistics
cement
production
data,
while
from
land-use
change
(ELUC),
mainly
deforestation,
land
use
bookkeeping
models.
Atmospheric
concentration
measured
directly,
its
growth
rate
(GATM)
computed
annual
changes
concentration.
The
ocean
sink
(SOCEAN)
estimated
with
biogeochemistry
models
observation-based
products.
(SLAND)
dynamic
vegetation
resulting
imbalance
(BIM),
difference
between
total
biosphere,
measure
imperfect
understanding
contemporary
cycle.
All
uncertainties
reported
as
±1σ.
For
year
2021,
EFOS
increased
by
5.1
%
relative
2020,
fossil
at
10.1
±
0.5
GtC
yr−1
(9.9
when
carbonation
included),
ELUC
was
1.1
0.7
yr−1,
for
emission
(including
sink)
10.9
0.8
(40.0
2.9
GtCO2).
Also,
GATM
5.2
0.2
(2.5
0.1
ppm
yr−1),
SOCEAN
0.4
SLAND
3.5
0.9
BIM
−0.6
(i.e.
sources
were
too
low
or
sinks
high).
atmospheric
averaged
over
2021
reached
414.71
ppm.
Preliminary
2022
suggest
an
increase
+1.0
(0.1
1.9
%)
globally
reaching
417.2
ppm,
more
than
50
above
pre-industrial
levels
(around
278
ppm).
Overall,
mean
trend
consistently
period
1959–2021,
but
discrepancies
up
1
persist
representation
semi-decadal
variability
fluxes.
Comparison
estimates
multiple
approaches
observations
shows
(1)
persistent
large
uncertainty
estimate
emissions,
(2)
agreement
different
methods
magnitude
flux
northern
extratropics,
(3)
discrepancy
strength
last
decade.
This
living
update
documents
used
this
new
progress
cycle
compared
previous
publications
set.
presented
work
available
https://doi.org/10.18160/GCP-2022
(Friedlingstein
et
al.,
2022b).
Earth system science data,
Journal Year:
2023,
Volume and Issue:
15(12), P. 5301 - 5369
Published: Nov. 30, 2023
Abstract.
Accurate
assessment
of
anthropogenic
carbon
dioxide
(CO2)
emissions
and
their
redistribution
among
the
atmosphere,
ocean,
terrestrial
biosphere
in
a
changing
climate
is
critical
to
better
understand
global
cycle,
support
development
policies,
project
future
change.
Here
we
describe
synthesize
data
sets
methodology
quantify
five
major
components
budget
uncertainties.
Fossil
CO2
(EFOS)
are
based
on
energy
statistics
cement
production
data,
while
from
land-use
change
(ELUC),
mainly
deforestation,
bookkeeping
models.
Atmospheric
concentration
measured
directly,
its
growth
rate
(GATM)
computed
annual
changes
concentration.
The
ocean
sink
(SOCEAN)
estimated
with
biogeochemistry
models
observation-based
fCO2
products.
(SLAND)
dynamic
vegetation
Additional
lines
evidence
land
sinks
provided
by
atmospheric
inversions,
oxygen
measurements,
Earth
system
resulting
imbalance
(BIM),
difference
between
total
biosphere,
measure
imperfect
incomplete
understanding
contemporary
cycle.
All
uncertainties
reported
as
±1σ.
For
year
2022,
EFOS
increased
0.9
%
relative
2021,
fossil
at
9.9±0.5
Gt
C
yr−1
(10.2±0.5
when
carbonation
not
included),
ELUC
was
1.2±0.7
yr−1,
for
emission
(including
sink)
11.1±0.8
(40.7±3.2
yr−1).
Also,
GATM
4.6±0.2
(2.18±0.1
ppm
yr−1;
denotes
parts
per
million),
SOCEAN
2.8±0.4
SLAND
3.8±0.8
BIM
−0.1
(i.e.
sources
marginally
too
low
or
high).
averaged
over
2022
reached
417.1±0.1
ppm.
Preliminary
2023
suggest
an
increase
+1.1
(0.0
2.1
%)
globally
reaching
419.3
ppm,
51
above
pre-industrial
level
(around
278
1750).
Overall,
mean
trend
consistently
period
1959–2022,
near-zero
overall
imbalance,
although
discrepancies
up
around
1
persist
representation
semi-decadal
variability
fluxes.
Comparison
estimates
multiple
approaches
observations
shows
following:
(1)
persistent
large
uncertainty
estimate
emissions,
(2)
agreement
different
methods
magnitude
flux
northern
extra-tropics,
(3)
discrepancy
strength
last
decade.
This
living-data
update
documents
applied
this
most
recent
well
evolving
community
presented
work
available
https://doi.org/10.18160/GCP-2023
(Friedlingstein
et
al.,
2023).
Nature Communications,
Journal Year:
2023,
Volume and Issue:
14(1)
Published: Feb. 10, 2023
Significant
efforts
have
been
invested
to
restore
mangrove
forests
worldwide
through
reforestation
and
afforestation.
However,
blue
carbon
benefit
has
not
compared
between
these
two
silvicultural
pathways
at
the
global
scale.
Here,
we
integrated
results
from
direct
field
measurements
of
over
370
restoration
sites
around
world
show
that
(reestablishing
mangroves
where
they
previously
colonized)
had
a
greater
storage
potential
per
hectare
than
afforestation
(establishing
mangrove).
Greater
accumulation
was
mainly
attributed
favorable
intertidal
positioning,
higher
nitrogen
availability,
lower
salinity
most
sites.
Reforestation
all
physically
feasible
areas
in
deforested
regions
could
promote
uptake
671.5-688.8
Tg
CO2-eq
globally
40-year
period,
60%
more
afforesting
same
area
on
tidal
flats
(more
marginal
sites).
Along
with
avoiding
conflicts
habitat
conversion,
should
be
given
priority
when
designing
nature-based
solutions
for
mitigating
climate
change.
Annual Review of Environment and Resources,
Journal Year:
2022,
Volume and Issue:
47(1), P. 317 - 341
Published: July 25, 2022
The
ocean
holds
vast
quantities
of
carbon
that
it
continually
exchanges
with
the
atmosphere
through
air-sea
interface.
Because
its
enormous
size
and
relatively
rapid
exchange
atmosphere,
controls
atmospheric
CO
2
concentration
thereby
Earth's
climate
on
timescales
tens
to
thousands
years.
This
review
examines
basic
functions
ocean's
cycle,
demonstrating
inventory
is
determined
primarily
by
mass
ocean,
chemical
speciation
in
seawater,
action
solubility
biological
pumps
draw
into
deeper
layers,
where
can
be
sequestered
for
decades
millennia.
also
plays
a
critical
role
moderating
impacts
change
absorbing
an
amount
equivalent
about
25%
anthropogenic
emissions
over
past
several
decades.
However,
this
leads
acidification
reduces
buffering
capacity
future
ability
take
up
.
closes
look
at
uncertain
cycle
scientific
challenges
uncertainty
brings.
Earth system science data,
Journal Year:
2023,
Volume and Issue:
15(2), P. 963 - 1004
Published: March 7, 2023
Abstract.
Accurate
accounting
of
emissions
and
removals
CO2
is
critical
for
the
planning
verification
emission
reduction
targets
in
support
Paris
Agreement.
Here,
we
present
a
pilot
dataset
country-specific
net
carbon
exchange
(NCE;
fossil
plus
terrestrial
ecosystem
fluxes)
stock
changes
aimed
at
informing
countries'
budgets.
These
estimates
are
based
on
“top-down”
NCE
outputs
from
v10
Orbiting
Carbon
Observatory
(OCO-2)
modeling
intercomparison
project
(MIP),
wherein
an
ensemble
inverse
groups
conducted
standardized
experiments
assimilating
OCO-2
column-averaged
dry-air
mole
fraction
(XCO2)
retrievals
(ACOS
v10),
situ
measurements
or
combinations
these
data.
The
MIP
combined
with
“bottom-up”
fuel
lateral
fluxes
to
estimate
stocks,
which
impacted
by
anthropogenic
natural
drivers.
flux
change
reported
annually
(2015–2020)
as
both
global
1∘
×
gridded
country-level
available
download
Committee
Earth
Observation
Satellites'
(CEOS)
website:
https://doi.org/10.48588/npf6-sw92
(Byrne
et
al.,
2022).
Across
experiments,
obtain
increases
median
stocks
3.29–4.58
Pg
yr−1
(0.90–1.25
C
yr−1).
This
result
broad
across
northern
extratropics,
while
tropics
generally
have
losses
but
considerable
regional
variability
differences
between
experiments.
We
discuss
state
science
tracking
using
top-down
methods,
including
current
limitations
future
developments
towards
monitoring
systems.
Nature,
Journal Year:
2023,
Volume and Issue:
623(7986), P. 329 - 333
Published: Oct. 4, 2023
Mountain
uplift
and
erosion
have
regulated
the
balance
of
carbon
between
Earth's
interior
atmosphere,
where
prior
focus
has
been
placed
on
role
silicate
mineral
weathering
in
CO2
drawdown
its
contribution
to
stability
climate
a
habitable
state1-5.
However,
can
also
release
as
rock
organic
(OCpetro)
is
oxidized
at
near
surface6,7;
this
important
geological
flux
remained
poorly
constrained3,8.
We
use
trace
element
rhenium
combination
with
spatial
extrapolation
model
quantify
across
global
river
catchments3,9.
find
[Formula:
see
text]
megatons
annually
from
OCpetro
near-surface
rocks,
rivalling
or
even
exceeding
by
scale10.
Hotspots
are
found
mountain
ranges
high
rates
exposing
fine-grained
sedimentary
rock,
such
eastern
Himalayas,
Rocky
Mountains
Andes.
Our
results
demonstrate
that
far
inert
causes
regions
be
net
sources
sinks
CO2.
This
raises
questions,
not
yet
fully
studied,
how
drive
long-term
cycle
contribute
fine
fluxes
biosphere
lithosphere2,11.