Geoscientific model development,
Journal Year:
2023,
Volume and Issue:
16(16), P. 4883 - 4936
Published: Aug. 30, 2023
Abstract.
The
cycling
of
carbon
in
the
oceans
is
affected
by
feedbacks
driven
changes
climate
and
atmospheric
CO2.
Understanding
these
therefore
an
important
prerequisite
for
projecting
future
climate.
Marine
biogeochemistry
models
are
a
useful
tool
but,
as
with
any
model,
simplification
need
to
be
continually
improved.
In
this
study,
we
coupled
Finite-volumE
Sea
ice–Ocean
Model
(FESOM2.1)
Regulated
Ecosystem
version
3
(REcoM3).
FESOM2.1
update
Finite-Element
(FESOM1.4)
operates
on
unstructured
meshes.
Unlike
standard
structured-mesh
ocean
models,
mesh
flexibility
allows
realistic
representation
small-scale
dynamics
key
regions
at
affordable
computational
cost.
Compared
previous
model
FESOM1.4–REcoM2,
FESOM2.1–REcoM3
utilizes
new
dynamical
core,
based
finite-volume
discretization
instead
finite
elements,
retains
central
parts
model.
As
feature,
carbonate
chemistry,
including
water
vapour
correction,
computed
mocsy
2.0.
Moreover,
REcoM3
has
extended
food
web
that
includes
macrozooplankton
fast-sinking
detritus.
Dissolved
oxygen
also
added
tracer.
assess
biogeochemical
state
simulated
global
set-up
relatively
low
spatial
resolution
forced
JRA55-do
(Tsujino
et
al.,
2018)
reanalysis.
focus
recent
period
(1958–2021)
how
well
can
used
present-day
change
scenarios
decadal
centennial
timescales.
A
bias
ocean–atmosphere
preindustrial
CO2
flux
present
(FESOM1.4–REcoM2)
could
significantly
reduced.
addition,
efficiency
2–3
times
higher
than
FESOM1.4–REcoM2.
Overall,
it
found
skilful
modelling
applications.
Earth system science data,
Journal Year:
2025,
Volume and Issue:
17(3), P. 965 - 1039
Published: March 14, 2025
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
datasets
methodologies
quantify
five
major
components
budget
uncertainties.
Fossil
CO2
(EFOS)
are
based
on
energy
statistics
cement
production
data,
while
from
land-use
change
(ELUC)
data
bookkeeping
models.
Atmospheric
concentration
measured
directly,
its
growth
rate
(GATM)
computed
annual
changes
concentration.
The
net
uptake
by
ocean
(SOCEAN,
called
sink)
estimated
with
biogeochemistry
models
observation-based
fCO2
products
(fCO2
fugacity
CO2).
land
(SLAND,
dynamic
vegetation
Additional
lines
evidence
sinks
provided
atmospheric
inversions,
oxygen
measurements,
Earth
system
sum
all
sources
results
imbalance
(BIM),
measure
imperfect
incomplete
understanding
contemporary
cycle.
All
uncertainties
reported
as
±1σ.
For
year
2023,
EFOS
increased
1.3
%
relative
2022,
fossil
at
10.1
±
0.5
GtC
yr−1
(10.3
when
carbonation
sink
not
included),
ELUC
was
1.0
0.7
yr−1,
for
total
emission
(including
11.1
0.9
(40.6
3.2
GtCO2
yr−1).
Also,
GATM
5.9
0.2
(2.79
0.1
ppm
yr−1;
denotes
parts
per
million),
SOCEAN
2.9
0.4
SLAND
2.3
near-zero
BIM
(−0.02
averaged
over
2023
reached
419.31
ppm.
Preliminary
2024
suggest
an
increase
+0.8
(−0.2
1.7
%)
globally
2.87
ppm,
reaching
422.45
52
above
pre-industrial
level
(around
278
1750).
Overall,
mean
trend
consistently
period
1959–2023,
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)
low
agreement
between
different
methods
magnitude
flux
northern
extra-tropics,
(3)
discrepancy
sink.
This
living-data
update
documents
applied
this
most
recent
well
evolving
community
presented
work
available
https://doi.org/10.18160/GCP-2024
(Friedlingstein
et
al.,
2024).
Geophysical Research Letters,
Journal Year:
2022,
Volume and Issue:
49(14)
Published: July 2, 2022
Abstract
The
ocean
reduces
human
impact
on
the
climate
by
absorbing
and
sequestering
CO
2
.
From
1950s
to
1980s,
observations
of
pCO
related
carbon
variables
were
sparse
uncertain.
Thus,
global
biogeochemical
models
(GOBMs)
have
been
basis
for
quantifying
sink.
LDEO‐Hybrid
Physics
Data
product
(LDEO‐HPD)
interpolates
surface
data
coverage
using
GOBMs
as
priors,
applying
machine
learning
estimate
full‐coverage
corrections.
largest
component
GOBM
corrections
are
climatological.
This
is
consistent
with
recent
findings
large
seasonal
discrepancies
in
GOBMs,
but
contrasts
long‐held
view
that
interannual
variability
a
major
source
error.
supports
extension
LDEO‐HPD
back
1959,
climatology
model‐observation
misfits
prior
1982.
Consistent
previous
studies
1980
onward,
air‐sea
fluxes
1959–2020
demonstrate
response
atmospheric
growth
volcanic
eruptions.
Global Biogeochemical Cycles,
Journal Year:
2023,
Volume and Issue:
37(11)
Published: Nov. 1, 2023
Abstract
We
assess
the
Southern
Ocean
CO
2
uptake
(1985–2018)
using
data
sets
gathered
in
REgional
Carbon
Cycle
Assessment
and
Processes
Project
Phase
2.
The
acted
as
a
sink
for
with
close
agreement
between
simulation
results
from
global
ocean
biogeochemistry
models
(GOBMs,
0.75
±
0.28
PgC
yr
−1
)
p
‐observation‐based
products
(0.73
0.07
).
This
is
only
half
that
reported
by
RECCAP1
same
region
timeframe.
present‐day
net
to
first
order
response
rising
atmospheric
,
driving
large
amounts
of
anthropogenic
(C
ant
into
ocean,
thereby
overcompensating
loss
natural
atmosphere.
An
apparent
knowledge
gap
increase
since
2000,
‐products
suggesting
growth
more
than
twice
strong
uncertain
GOBMs
(0.26
0.06
0.11
0.03
Pg
C
decade
respectively).
despite
nearly
identical
trends
when
both
are
compared
at
locations
where
was
measured.
Seasonal
analyses
revealed
processes
winter
uncertainty
magnitude
outgassing,
whereas
discrepancies
fundamental
summer,
exhibit
difficulties
simulating
effects
non‐thermal
biology
mixing/circulation.
interior
accumulation
points
an
underestimate
storage
GOBMs.
Future
work
needs
link
surface
fluxes
transport,
build
long
overdue
systematic
observation
networks
push
toward
better
process
understanding
drivers
carbon
cycle.
Remote Sensing,
Journal Year:
2025,
Volume and Issue:
17(2), P. 177 - 177
Published: Jan. 7, 2025
A
good
quantitative
knowledge
of
regional
sources
and
sinks
atmospheric
carbon
dioxide
(CO2)
is
essential
for
understanding
the
global
cycle.
It
also
a
key
prerequisite
elaborating
cost-effective
national
strategies
to
achieve
goals
Paris
Agreement.
However,
available
estimates
CO2
fluxes
many
regions
world
remain
uncertain,
despite
significant
recent
progress
in
remote
sensing
terrestrial
vegetation
CO2.
In
this
study,
we
investigate
feasibility
inferring
reliable
net
ecosystem
exchange
(NEE)
using
column-averaged
dry-air
mole
fractions
(XCO2)
retrieved
from
Orbiting
Carbon
Observatory-2
(OCO-2)
observations
as
constraints
on
parameters
widely
used
Vegetation
Photosynthesis
Respiration
model
(VPRM),
which
predicts
based
indices
derived
multispectral
satellite
imagery.
We
developed
regional-scale
inverse
modeling
system
that
applies
Bayesian
variational
optimization
algorithm
optimize
VPRM
coupled
CHIMERE
chemistry
transport
involves
preliminary
transformation
input
XCO2
data
reduces
impact
boundary
conditions
inversion
results.
investigated
potential
our
by
applying
it
European
region
(that
includes,
particular,
EU
countries
UK)
warm
season
(May–September)
2021.
The
OCO-2
resulted
major
(more
than
threefold)
reduction
prior
uncertainty
NEE
estimate.
posterior
estimate
agrees
with
independent
provided
CarbonTracker
Europe
High-Resolution
(CTE-HR)
ensemble
v10
intercomparison
(MIP)
inversions.
found
improves
agreement
simulations
retrievals
Total
Column
Observing
Network
(TCCON).
Our
sensitivity
test
experiments
synthetic
indicate
would
even
if
actual
drastically
differed
their
values.
Furthermore,
be
robust
strong
biases
random
uncertainties
conditions.
Overall,
study
suggests
approach
offers
relatively
simple
way
derive
while
enhancing
applicability
where
eddy
covariance
measurements
are
scarce.
Ecological Indicators,
Journal Year:
2023,
Volume and Issue:
154, P. 110885 - 110885
Published: Sept. 1, 2023
As
China's
largest
cross-regional
urban
agglomerations,
the
middle
reaches
of
Yangtze
River
agglomerations
(MRYRUA)
possess
both
significant
societal
carbon
source
volume
and
ecological
sequestration
capacity.
Nevertheless,
with
uncontrolled
expansion
energy
consumption
activities
industry
migration
from
eastern
coastal
regions
to
inland
cities,
budget
pattern
territorial
space
is
increasingly
unbalanced
in
MRYRUA.
To
achieve
low-carbon
regulation,
this
study
utilized
land
use
data
31
cities
within
MRYRUA
establish
a
"carbon
source-carbon
sink"
quantification
spatiotemporal
exploration
model,
revealing
spatial-temporal
variation
budgets
2005
2020.
Furthermore,
we
developed
balance
indicator
analysis
system
by
employing
offset
rate
(COR),
productivity
(CP),
Gini
coefficient,
support
coefficient
(ESC),
economic
contribution
(ECC),
functional
zoning
was
performed.
Finally,
using
GM
(1,1)
derived
for
2050
explored
differentiated
regulatory
mechanisms
under
perspective.
The
results
indicated
that:
(1)
MRYRUA's
have
increased
annually,
displaying
spatial
distribution
highest
values
central
region,
followed
northwest,
lowest
southeast
near
water
bodies.
differentiation
effects
manifest
as
an
east–west
axial
development
trend,
clustering
demonstrating
propensity
outward
dispersion
northern
hot
spot
radiation
core.
(2)
COR
has
consistently
remained
below
10%
decreased
while
CP
shown
yearly
increase
at
accelerating
rate.
ESC
ECC
exhibit
evident
heterogeneity
among
cities.
In
response
emission
benefits
carrying
capacity
reflected
indicators,
each
city
classified
into
zones,
intensity
control
sink
high-carbon
optimization
zones.
(3)
From
2020
2050,
polarization
trend
continues
intensify.
Subsequently,
established
mechanism.
This
mechanism
strengthens
leading
role
zones
green
transition,
moderately
retains
solid
fixation
capabilities,
promotes
transition
research
findings
provide
scientific
basis
formulating
planning
policies
neutrality
Global Sustainability,
Journal Year:
2023,
Volume and Issue:
7
Published: Jan. 1, 2023
Abstract
Non-technical
summary
We
identify
a
set
of
essential
recent
advances
in
climate
change
research
with
high
policy
relevance,
across
natural
and
social
sciences:
(1)
looming
inevitability
implications
overshooting
the
1.5°C
warming
limit,
(2)
urgent
need
for
rapid
managed
fossil
fuel
phase-out,
(3)
challenges
scaling
carbon
dioxide
removal,
(4)
uncertainties
regarding
future
contribution
sinks,
(5)
intertwinedness
crises
biodiversity
loss
change,
(6)
compound
events,
(7)
mountain
glacier
loss,
(8)
human
immobility
face
risks,
(9)
adaptation
justice,
(10)
just
transitions
food
systems.
Technical
The
Intergovernmental
Panel
on
Climate
Change
Assessment
Reports
provides
scientific
foundation
international
negotiations
constitutes
an
unmatched
resource
researchers.
However,
assessment
cycles
take
multiple
years.
As
to
cross-
interdisciplinary
understanding
diverse
communities,
we
have
streamlined
annual
process
synthesize
significant
advances.
collected
input
from
experts
various
fields
using
online
questionnaire
prioritized
10
key
insights
relevance.
This
year,
focus
on:
overshoot
urgency
scale-up
joint
governance
accelerated
amidst
present
succinct
account
these
insights,
reflect
their
implications,
offer
integrated
policy-relevant
messages.
science
synthesis
communication
effort
is
also
basis
report
contributing
elevate
every
year
time
United
Nations
Conference.
Social
media
highlight
–
more
than
200
experts.
Ocean-Land-Atmosphere Research,
Journal Year:
2024,
Volume and Issue:
3
Published: Jan. 1, 2024
The
chemical
oxygen
demand
(COD)
is
an
essential
indicator
of
organic
pollution
that
represents
the
amount
bulk
carbon
in
water.
COD
strongly
correlated
with
nutrient
cycles
and
other
pollutants
environment,
but
it
has
a
limited
ability
to
quantify
(OC),
which
large
proportion
made
up
refractory
dissolved
(RDOC)
potential
sink.
Moreover,
biodegradability
OC
terms
its
fate
destination
should
be
explored,
as
well
how
this
reflected
by
COD.
Methods
based
on
particle
size,
spectroscopy,
isotopic
tracing
are
expected
help
deciphering
bioavailability
COD-responsive
explore
processes
biogeochemical
cycles.
As
pressure
environment
from
anthropogenic
inputs
increases,
understanding
associated
will
developing
more
precise
scientific
indicators
for
environmental
monitoring
identifying
new
tools
increase
knowledge
cycle.
In
review,
we
discuss
application,
scope,
means,
advances
measurement.
Based
data
literature,
estimate
global
RDOC
stock
assess
impact
cycle
offshore
bays.
This
review
presents
insights
into
behavior
aquatic
environments
pathway
ocean
negative
emissions
expanding
role
sink
offset
effect
emissions.
Journal of Geophysical Research Atmospheres,
Journal Year:
2023,
Volume and Issue:
128(14)
Published: July 10, 2023
Abstract
The
magnitude
and
distribution
of
China's
terrestrial
carbon
sink
remain
uncertain
due
to
insufficient
observational
constraints;
satellite
column‐average
dry‐air
mole
fraction
dioxide
(XCO
2
)
retrievals
may
fill
some
this
gap.
Here,
we
estimate
using
atmospheric
inversions
the
Orbiting
Carbon
Observatory
(OCO‐2)
XCO
within
different
platforms,
including
Global
Assimilation
System
(GCAS)
v2,
Copernicus
Atmosphere
Monitoring
Service,
OCO‐2
Model
Inter‐comparison
Project
(MIP).
We
find
that
they
consistently
place
largest
net
biome
production
(NBP)
in
south
on
an
annual
basis
compared
northeast
other
main
agricultural
areas
during
peak
growing
season,
coinciding
well
with
forests
crops,
respectively.
Moreover,
mean
seasonal
cycle
amplitude
NBP
is
obviously
larger
than
biosphere
model
simulations
slightly
greater
surface
CO
inversions.
More
importantly,
constrained
temperate,
tropical,
subtropical
monsoon
climate
zones,
better
inter‐model
consistency
at
a
sub‐regional
scale
situ
simulations.
In
addition,
China
for
2015–2019
be
between
0.34
(GCASv2)
0.47
±
0.16
PgC/yr
(median
std;
v10
MIP),
indicate
impacts
extremes
(e.g.,
2019
drought)
interannual
variations
NBP.
Our
results
suggest
assimilating
crucial
improving
our
understanding
regime.
Annual Review of Earth and Planetary Sciences,
Journal Year:
2024,
Volume and Issue:
52(1), P. 467 - 493
Published: Jan. 18, 2024
The
Paris
Agreement
calls
for
emissions
reductions
to
limit
climate
change,
but
how
will
the
carbon
cycle
change
if
it
is
successful?
land
and
oceans
currently
absorb
roughly
half
of
anthropogenic
emissions,
this
fraction
decline
in
future.
amount
that
can
be
released
before
mitigated
depends
on
ocean
terrestrial
ecosystems
absorb.
Policy
based
model
projections,
observations
theory
suggest
effects
emerging
today's
increase
tipping
points
may
crossed.
Warming
temperatures,
drought,
a
slowing
growth
rate
CO2
itself
reduce
sinks
create
new
sources,
making
sequestration
forests,
soils,
other
aquatic
vegetation
more
difficult.
Observations,
data-assimilative
models,
prediction
systems
are
needed
managing
ongoing
long-term
changes
after
achieving
net-zero
emissions.
▪International
agreements
call
stabilizing
at
1.5°
above
preindustrial,
while
world
already
seeing
damaging
extremes
below
that.▪If
stabilized
near
target,
driving
force
most
slow,
feedbacks
from
warmer
continue
cause
sources.▪Once
reduced
net
zero,
cycle-climate
require
support
active
management
maintain
storage.