Journal of Environmental Quality,
Год журнала:
2022,
Номер
51(5), С. 899 - 915
Опубликована: Апрель 22, 2022
The
subtropical
region
of
Brazil
is
home
to
33%
the
soybean
[Glycine
max
(L.)
Merr.]
growing
area
and
90%
wheat
(Tritucum
aestivum
L.)
this
country.
A
soybean-wheat
succession
with
fallow
between
crops
used
in
about
11%
cultivated
area.
No
study
has
quantified
CO2
fluxes
annual
region.
Hence,
analyzed
seasonality
exchange
(net
ecosystem
[NEE])
a
2015/2016
wheat-soybean
commercial
farm
located
Carazinho,
Rio
Grande
do
Sul
State,
Brazil.
eddy
covariance
method
was
estimate
C
balance
system.
NEE
partitioned
gross
primary
productivity
respiration
understand
dynamics
these
during
year
succession.
Considering
net
photosynthesis
season,
both
absorbed
from
atmosphere
(NEE
wheat:
-347
±
4
g
m-2
;
soybean:
-242
3
).
periods
seasons,
however,
acted
as
source
156
2
,
reducing
by
27%.
For
1
yr,
biome
-50
yr-1
.
results
obtained
here
demonstrate
that
sink
under
specific
climatic
conditions
field
management
practices
long
period
limited
agroecosystem
becoming
more
efficient
sink.
Earth system science data,
Год журнала:
2022,
Номер
14(12), С. 5463 - 5488
Опубликована: Дек. 15, 2022
Abstract.
Accurate
high-resolution
actual
evapotranspiration
(ET)
and
gross
primary
production
(GPP)
information
is
essential
for
understanding
the
large-scale
water
carbon
dynamics.
However,
substantial
uncertainties
exist
in
current
ET
GPP
datasets
China
because
of
insufficient
local
ground
measurements
used
model
constraint.
This
study
utilizes
a
water–carbon
coupled
model,
Penman–Monteith–Leuning
Version
2
(PML-V2),
to
estimate
500
m
at
daily
scale.
The
parameters
PML-V2(China)
were
well
calibrated
against
observations
26
eddy
covariance
flux
towers
across
nine
plant
functional
types
China,
indicated
by
Nash–Sutcliffe
efficiency
(NSE)
0.75
root
mean
square
error
(RMSE)
0.69
mm
d−1
ET,
respectively,
NSE
0.82
RMSE
1.71
g
C
m−2
GPP.
estimates
get
small
Bias
6.28
%
high
water-balance
annual
10
major
river
basins
China.
Further
evaluations
suggest
that
newly
developed
product
better
than
other
typical
products
(MOD16A2,
SEBAL,
GLEAM,
MOD17A2H,
VPM,
EC-LUE)
estimating
both
Moreover,
accurately
monitors
intra-annual
variations
croplands
with
dual-cropping
system.
new
data
showed
that,
during
2001–2018,
use
experienced
significant
(p<0.001)
increase
(8.99
yr−2
0.02
mm−1
H2O
yr−1,
respectively),
but
non-significant
(p>0.05)
(0.43
yr−2).
indicates
vegetation
exhibits
huge
potential
sequestration
little
cost
resources.
provides
great
opportunity
academic
communities
various
agencies
scientific
studies
applications,
freely
available
https://doi.org/10.11888/Terre.tpdc.272389
(Zhang
He,
2022).
Summary
A
new
proliferation
of
optical
instruments
that
can
be
attached
to
towers
over
or
within
ecosystems,
‘proximal’
remote
sensing,
enables
a
comprehensive
characterization
terrestrial
ecosystem
structure,
function,
and
fluxes
energy,
water,
carbon.
Proximal
sensing
bridge
the
gap
between
individual
plants,
site‐level
eddy‐covariance
fluxes,
airborne
spaceborne
by
providing
continuous
data
at
high‐spatiotemporal
resolution.
Here,
we
review
recent
advances
in
proximal
for
improving
our
mechanistic
understanding
plant
processes,
model
development,
validation
current
upcoming
satellite
missions.
We
provide
best
practices
availability
metadata
sensing:
spectral
reflectance,
solar‐induced
fluorescence,
thermal
infrared
radiation,
microwave
backscatter,
LiDAR.
Our
paper
outlines
steps
necessary
making
these
streams
more
widespread,
accessible,
interoperable,
information‐rich,
enabling
us
address
key
ecological
questions
unanswerable
from
space‐based
observations
alone
and,
ultimately,
demonstrate
feasibility
technologies
critical
local
global
ecology.
Global Change Biology,
Год журнала:
2021,
Номер
27(16), С. 3923 - 3938
Опубликована: Май 2, 2021
Abstract
Soil
respiration
(Rs),
the
efflux
of
CO
2
from
soils
to
atmosphere,
is
a
major
component
terrestrial
carbon
cycle,
but
poorly
constrained
regional
global
scales.
The
soil
database
(SRDB)
compilation
in
situ
Rs
observations
around
globe
that
has
been
consistently
updated
with
new
measurements
over
past
decade.
It
unclear
whether
addition
data
versions
produced
better‐constrained
estimates.
We
compared
two
SRDB
(v3.0
n
=
5173
and
v5.0
10,366)
determine
how
additional
influenced
annual
sum,
spatial
patterns
associated
uncertainty
(1
km
resolution)
using
machine
learning
approach.
A
quantile
regression
forest
model
parameterized
SRDBv3
yielded
sum
88.6
Pg
C
year
−1
,
29.9
(mean
absolute
error)
57.9
(standard
deviation)
whereas
parameterization
SRDBv5
96.5
30.2
average
73.4
.
Empirically
estimated
heterotrophic
(Rh)
v3
v5
were
49.9–50.2
50.1)
53.3–53.5
53.4)
respectively.
SRDBv5’s
inclusion
underrepresented
regions
(e.g.,
Asia,
Africa,
South
America)
resulted
overall
higher
uncertainty.
largest
differences
between
models
different
SRDVB
arid/semi‐arid
regions.
still
biased
toward
northern
latitudes
temperate
zones,
so
we
tested
an
optimized
distribution
measurements,
which
96.4
±
21.4
lower
These
results
support
current
estimates
highlight
biases
influence
interpretation
provide
insights
for
design
environmental
networks
improve
global‐scale
Biogeosciences,
Год журнала:
2022,
Номер
19(3), С. 559 - 583
Опубликована: Фев. 2, 2022
Abstract.
Large
changes
in
the
Arctic
carbon
balance
are
expected
as
warming
linked
to
climate
change
threatens
destabilize
ancient
permafrost
stocks.
The
eddy
covariance
(EC)
method
is
an
established
technique
quantify
net
losses
and
gains
of
between
biosphere
atmosphere
at
high
spatiotemporal
resolution.
Over
past
decades,
a
growing
network
terrestrial
EC
tower
sites
has
been
across
Arctic,
but
comprehensive
assessment
network's
representativeness
within
heterogeneous
region
still
lacking.
This
creates
additional
uncertainties
when
integrating
flux
data
sites,
for
example
upscaling
fluxes
constrain
pan-Arctic
budgets
therein.
study
provides
inventory
(here
>
=
60∘
N)
which
also
made
available
online
(https://cosima.nceas.ucsb.edu/carbon-flux-sites/,
last
access:
25
January
2022).
Our
database
currently
comprises
120
only
83
listed
active,
just
these
active
remain
operational
throughout
winter.
To
map
this
network,
we
evaluated
similarity
environmental
conditions
observed
locations
those
larger
domain
based
on
18
bioclimatic
edaphic
variables.
allows
us
assess
general
level
ecosystem
domain,
while
not
necessarily
reflecting
greenhouse
gas
rates
directly.
We
define
two
metrics
score:
one
that
measures
whether
location
represented
by
with
similar
characteristics
(ER1)
second
if
minimum
representation
statistically
rigorous
extrapolation
met
(ER4).
find
half
least
tower,
third
enough
towers
allow
reliable
extrapolation.
When
consider
methane
measurements
or
year-round
(including
wintertime)
measurements,
values
drop
about
1/5
1/10
respectively.
With
majority
located
Fennoscandia
Alaska,
regions
were
assigned
highest
representativeness,
large
parts
Siberia
patches
Canada
classified
underrepresented.
Across
mountainous
particularly
poorly
current
observation
network.
tested
three
different
strategies
identify
new
site
upgrades
existing
optimally
enhance
While
15
can
improve
20
%,
upgrading
few
10
capture
during
wintertime
their
respective
ER1
coverage
28
%
33
%.
targeted
improvement
could
be
shown
clearly
superior
unguided
selection
therefore
leading
substantial
improvements
relatively
small
investments.
Nature Communications,
Год журнала:
2022,
Номер
13(1)
Опубликована: Апрель 1, 2022
Abstract
The
terrestrial
carbon
cycle
is
a
major
source
of
uncertainty
in
climate
projections.
Its
dominant
fluxes,
gross
primary
productivity
(GPP),
and
respiration
(in
particular
soil
respiration,
R
S
),
are
typically
estimated
from
independent
satellite-driven
models
upscaled
situ
measurements,
respectively.
We
combine
carbon-cycle
flux
estimates
partitioning
coefficients
to
show
that
historical
global
GPP
irreconcilable.
When
we
estimate
based
on
measurements
some
assumptions
about
:GPP
ratios,
found
the
resulted
values
(bootstrap
mean
$${149}_{-23}^{+29}$$
149−23+29
Pg
C
yr
−1
)
significantly
higher
than
most
reported
literature
(
$${113}_{-18}^{+18}$$
11318
).
Similarly,
imply
(Rs
,
bootstrap
$${68}_{-8}^{+10}$$
68810
statistically
inconsistent
with
published
$${87}_{-8}^{+9}$$
879
although
recent,
higher,
narrowing
this
gap.
Furthermore,
ratios
spatial
averages
ratio
calculated
individual
sites
as
well
CMIP6
model
results.
This
discrepancy
has
implications
for
our
understanding
turnover
times
sensitivity
change.
Future
efforts
should
reconcile
discrepancies
associated
calculations
Rs
improve
budget.
Abstract
Wetlands
cover
a
small
portion
of
the
world,
but
have
disproportionate
influence
on
global
carbon
(C)
sequestration,
dioxide
and
methane
emissions,
aquatic
C
fluxes.
However,
underlying
biogeochemical
processes
that
affect
wetland
pools
fluxes
are
complex
dynamic,
making
measurements
challenging.
Over
decades
research,
many
observational,
experimental,
analytical
approaches
been
developed
to
understand
quantify
C.
Sampling
range
in
their
representation
from
short
long
timeframes
local
landscape
spatial
scales.
This
review
summarizes
common
cutting-edge
methodological
for
quantifying
We
first
define
each
major
provide
rationale
importance
dynamics.
For
approach,
we
clarify
what
component
is
measured
its
temporal
representativeness
constraints.
describe
practical
considerations
such
as
where
when
an
approach
typically
used,
who
can
conduct
(expertise,
training
requirements),
how
conducted,
including
equipment
complexity
costs.
Finally,
key
covariates
ancillary
enhance
interpretation
findings
facilitate
model
development.
The
protocols
measure
soil,
water,
vegetation,
gases
also
relevant
related
disciplines
ecology.
Improved
quality
consistency
data
collection
reporting
across
studies
will
help
reduce
uncertainties
develop
management
strategies
use
wetlands
nature-based
climate
solutions.
Abstract
Wetlands
are
responsible
for
20%–31%
of
global
methane
(CH
4
)
emissions
and
account
a
large
source
uncertainty
in
the
CH
budget.
Data‐driven
upscaling
fluxes
from
eddy
covariance
measurements
can
provide
new
independent
bottom‐up
estimates
wetland
emissions.
Here,
we
develop
six‐predictor
random
forest
model
(UpCH4),
trained
on
119
site‐years
flux
data
43
freshwater
sites
FLUXNET‐CH4
Community
Product.
Network
patterns
site‐level
annual
means
mean
seasonal
cycles
were
reproduced
accurately
tundra,
boreal,
temperate
regions
(Nash‐Sutcliffe
Efficiency
∼0.52–0.63
0.53).
UpCH4
estimated
146
±
TgCH
y
−1
2001–2018
which
agrees
closely
with
current
land
surface
models
(102–181
overlaps
top‐down
atmospheric
inversion
(155–200
).
However,
diverged
both
types
spatial
pattern
dynamics
tropical
We
conclude
that
has
potential
to
produce
realistic
extra‐tropical
will
improve
more
data.
To
reduce
upscaled
estimates,
researchers
could
prioritize
along
humid‐to‐arid
climate
gradients,
major
rainforest
basins
(Congo,
Amazon,
SE
Asia),
into
monsoon
(Bangladesh
India)
savannah
(African
Sahel)
be
paired
improved
knowledge
extent
these
regions.
The
monthly
products
gridded
at
0.25°
available
via
ORNL
DAAC
(
https://doi.org/10.3334/ORNLDAAC/2253