Global Change Biology,
Journal Year:
2016,
Volume and Issue:
23(5), P. 1763 - 1773
Published: Nov. 7, 2016
Comparisons
among
ecosystem
models
or
dynamics
along
environmental
gradients
commonly
rely
on
metrics
that
integrate
different
processes
into
a
useful
diagnostic.
Terms
such
as
age,
turnover,
residence,
and
transit
times
are
often
used
for
this
purpose;
however,
these
terms
variably
defined
in
the
literature
many
cases,
calculations
ignore
assumptions
implicit
their
formulas.
The
aim
of
opinion
piece
was
i)
to
make
evident
discrepancies
incorrect
use
formulas,
ii)
highlight
recent
results
simplify
may
help
avoid
confusion,
iii)
propose
adoption
simple
less
ambiguous
terms.
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).
Journal of Advances in Modeling Earth Systems,
Journal Year:
2020,
Volume and Issue:
12(4)
Published: March 11, 2020
Abstract
Land
surface
models
(LSMs)
are
a
vital
tool
for
understanding,
projecting,
and
predicting
the
dynamics
of
land
its
role
within
Earth
system,
under
global
change.
Driven
by
need
to
address
set
key
questions,
LSMs
have
grown
in
complexity
from
simplified
representations
biophysics
encompass
broad
interrelated
processes
spanning
disciplines
biophysics,
biogeochemistry,
hydrology,
ecosystem
ecology,
community
human
management,
societal
impacts.
This
vast
scope
complexity,
while
warranted
problems
designed
solve,
has
led
enormous
challenges
understanding
attributing
differences
between
LSM
predictions.
Meanwhile,
wide
range
spatial
scales
that
govern
heterogeneity,
spectrum
timescales
dynamics,
create
tractably
representing
LSMs.
We
identify
three
“grand
challenges”
development
use
LSMs,
based
around
these
issues:
managing
process
parametric
across
asked
changing
world.
In
this
review,
we
discuss
progress
been
made,
as
well
promising
directions
forward,
each
challenges.
Nature Communications,
Journal Year:
2019,
Volume and Issue:
10(1)
Published: Sept. 18, 2019
Satellite
observations
show
that
leaf
area
index
(LAI)
has
increased
globally
since
1981,
but
the
impact
of
this
vegetation
structural
change
on
global
terrestrial
carbon
cycle
not
been
systematically
evaluated.
Through
process-based
diagnostic
ecosystem
modeling,
we
find
increase
in
LAI
alone
was
responsible
for
12.4%
accumulated
sink
(95
±
5
Pg
C)
from
1981
to
2016,
whereas
other
drivers
CO2
fertilization,
nitrogen
deposition,
and
climate
(temperature,
radiation,
precipitation)
contributed
47.0%,
1.1%,
-28.6%
sink,
respectively.
The
legacy
effects
past
changes
these
prior
are
remaining
65.5%
2016.
These
results
refine
attribution
land
various
would
help
constrain
prognostic
models
often
have
large
uncertainties
simulating
their
impacts
cycle.
Geoscientific model development,
Journal Year:
2016,
Volume and Issue:
9(8), P. 2853 - 2880
Published: Aug. 25, 2016
Abstract.
Coordinated
experimental
design
and
implementation
has
become
a
cornerstone
of
global
climate
modelling.
Model
Intercomparison
Projects
(MIPs)
enable
systematic
robust
analysis
results
across
many
models,
by
reducing
the
influence
ad
hoc
differences
in
model
set-up
or
boundary
conditions.
As
it
enters
its
6th
phase,
Coupled
Project
(CMIP6)
grown
significantly
scope
with
documentation
individual
simulations
delegated
to
science
communities.
The
Climate–Carbon
Cycle
(C4MIP)
takes
responsibility
for
design,
documentation,
carbon
cycle
feedbacks
interactions
simulations.
These
are
potentially
large
play
leading-order
contribution
determining
atmospheric
composition
response
human
emissions
CO2
setting
targets
stabilize
avoid
dangerous
change.
For
over
decade,
C4MIP
coordinated
coupled
climate–carbon
simulations,
this
paper
we
describe
that
will
be
formally
part
CMIP6.
While
community
created
also
fit
within
wider
CMIP
activity,
conform
some
common
standards
including
diagnostic
requests,
designed
complement
core
experiments
known
as
Diagnostic,
Evaluation
Characterization
Klima
(DECK).
three
key
strands
scientific
motivation
requested
satisfy
their
needs:
(1)
pre-industrial
historical
(formally
set
CMIP6
experiments)
evaluation,
(2)
idealized
partially
1
%
per
year
increases
diagnosis
feedback
strength
components,
(3)
future
scenario
project
how
Earth
system
respond
anthropogenic
activity
21st
century
beyond.
This
documents
detail
these
explains
rationale
planned
analysis,
describes
up
run
Particular
attention
is
paid
conditions,
input
data,
output
diagnostics.
It
important
modelling
groups
participating
adhere
closely
possible
design.
Environmental Science & Technology,
Journal Year:
2016,
Volume and Issue:
50(23), P. 13123 - 13133
Published: Nov. 16, 2016
We
present
a
gridded
inventory
of
US
anthropogenic
methane
emissions
with
0.1°
×
spatial
resolution,
monthly
temporal
and
detailed
scale-dependent
error
characterization.
The
is
designed
to
be
consistent
the
2016
Environmental
Protection
Agency
(EPA)
Inventory
Greenhouse
Gas
Emissions
Sinks
(GHGI)
for
2012.
EPA
available
only
as
national
totals
different
source
types.
use
wide
range
databases
at
state,
county,
local,
point
level
disaggregate
allocate
distribution
individual
Results
show
large
differences
EDGAR
v4.2
global
commonly
used
priori
estimate
in
inversions
atmospheric
observations.
derive
grid-dependent
statistics
types
from
comparison
Defense
Fund
(EDF)
regional
Northeast
Texas.
These
are
independently
verified
by
California
Measurement
(CALGEM)
grid-resolved
emission
inventory.
Our
gridded,
time-resolved
provides
an
improved
basis
inversion
observations
interpret
results
terms
underlying
processes.
Geoscientific model development,
Journal Year:
2017,
Volume and Issue:
10(6), P. 2141 - 2156
Published: June 6, 2017
Abstract.
Wetland
emissions
remain
one
of
the
principal
sources
uncertainty
in
global
atmospheric
methane
(CH4)
budget,
largely
due
to
poorly
constrained
process
controls
on
CH4
production
waterlogged
soils.
Process-based
estimates
wetland
and
their
associated
uncertainties
can
provide
crucial
prior
information
for
model-based
top-down
emission
estimates.
Here
we
construct
a
model
ensemble
use
chemical
transport
models
(WetCHARTs
version
1.0).
Our
0.5°
×
resolution
is
based
satellite-derived
surface
water
extent
precipitation
reanalyses,
nine
heterotrophic
respiration
simulations
(eight
carbon
cycle
data-constrained
terrestrial
analysis)
three
temperature
dependence
parameterizations
period
2009–2010;
an
extended
subset
solely
analysis
derived
2001–2015.
We
incorporate
mean
full
ensembles
into
GEOS-Chem
compare
against
measurements
CH4;
performance
(site-level
zonal
anomaly
residuals)
compares
favourably
published
scenarios.
find
that
decomposition
rates
together
account
more
than
80
%
dominant
timing,
magnitude
seasonal
variability
emissions,
although
:
C
significant
contributor
variations
mid-latitude
emissions.
The
combination
satellite,
provides
physically
informed
structural
priori
critical
fluxes.
Specifically,
our
enhanced
error
covariance
structure,
as
well
means
using
posterior
flux
quantitatively
constrain
biogeochemical
Earth system science data,
Journal Year:
2021,
Volume and Issue:
13(8), P. 3927 - 3950
Published: Aug. 11, 2021
Abstract.
The
terrestrial
forest
carbon
pool
is
poorly
quantified,
in
particular
regions
with
low
inventory
capacity.
By
combining
multiple
satellite
observations
of
synthetic
aperture
radar
(SAR)
backscatter
around
the
year
2010,
we
generated
a
global,
spatially
explicit
dataset
above-ground
live
biomass
(AGB;
dry
mass)
stored
forests
spatial
resolution
1
ha.
Using
an
extensive
database
110
897
AGB
measurements
from
field
plots,
show
that
patterns
and
magnitude
are
well
captured
our
map
exception
regional
uncertainties
high-carbon-stock
>250
Mg
ha−1,
where
retrieval
was
effectively
based
on
single
observation.
With
total
global
522
Pg,
estimate
lower
than
most
estimates
published
literature
(426–571
Pg).
Nonetheless,
increases
knowledge
distribution
compared
to
Global
Forest
Resources
Assessment
(FRA)
by
Food
Agriculture
Organization
(FAO)
highlights
impact
country's
national
capacity
accuracy
statistics
reported
FRA.
We
also
reassessed
previous
remote
sensing
maps
identified
major
biases
data,
up
120
%
value
tropical
forests,
subtropics
temperate
zone.
Because
high
level
detail
overall
reliability
patterns,
likely
have
significant
impacts
climate,
carbon,
socio-economic
modelling
schemes
provides
crucial
baseline
future
stock
change
estimates.
available
at
https://doi.org/10.1594/PANGAEA.894711
(Santoro,
2018).