Decreased Air‐Sea CO2 ${\mathbf{\text{CO}}}_{\mathbf{2}}$ Flux During the Persistent Marine Heatwaves in the Yellow Sea and East China Sea
G Ren,
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Rong Na,
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Shaoqing Zhang
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et al.
Journal of Geophysical Research Oceans,
Journal Year:
2025,
Volume and Issue:
130(4)
Published: April 1, 2025
Abstract
Marine
heatwaves
(MHWs)
exert
a
significant
influence
on
marine
ecosystem,
especially
in
marginal
seas
where
carbonate
processes
are
intricately
linked
to
temperature
variations.
However,
how
MHWs
affect
the
seas,
such
as
Yellow
Sea
(YS)
and
East
China
(ECS),
remains
unclear.
Here,
we
employ
physical‐biogeochemical
model
simulate
aiming
systematically
quantify
impacts
of
persistent
(PMHWs)
air‐sea
flux
()
anomaly
YS
ECS.
Results
reveal
that
due
reduced
wind
speed
elevated
during
PMHWs,
ocean
reservoir
experiences
dramatic
decrease.
In
summer
when
releases
CO
2
atmosphere,
suppressed
outgassing
induced
by
decreased
counteracts
resulted
from
high
temperature.
winter,
both
factors
suppress
absorption
atmosphere
ocean.
addition,
spatial
pattern
is
dominated
partial
pressure
surface
water
().
While
thermal
effects
have
contribution
61%
33%
ECS
positive
anomaly,
non‐thermal
primarily
driven
alkalinity
play
more
vital
role
amplifying
(61%
90%
respectively).
Furthermore,
horizontal
advection
emerges
dominant
process
modulating
variations
ECS,
with
72
±
17%
75
60%
respectively.
These
findings
underscore
importance
understanding
physical
mechanisms
behind
PMHWs
analyzing
its
ecological
within
coastal
environments.
Language: Английский
Marine Heatwave and Terrestrial Drought Reduced CO2 Uptake in the East China Sea in 2022
Remote Sensing,
Journal Year:
2024,
Volume and Issue:
16(5), P. 849 - 849
Published: Feb. 29, 2024
Against
the
background
of
climate
warming,
marine
heatwaves
(MHWs)
and
terrestrial
drought
events
have
become
increasingly
frequent
in
recent
decades.
However,
combined
effects
MHWs
on
CO2
uptake
marginal
seas
are
still
unclear.
The
East
China
Sea
(ECS)
experienced
an
intense
long-lasting
MHW
accompanied
by
extreme
Changjiang
basin
summer
2022.
In
this
study,
we
employed
multi-source
satellite
remote
sensing
products
to
reveal
patterns,
magnitude,
potential
drivers
flux
changes
ECS
resulting
from
compounding
extremes.
reduced
17.0%
(1.06
Tg
C)
latter
half
2022
River
plume
region
shifted
a
sink
source
(releasing
0.11
July-September.
majority
ECS,
positive
sea
surface
temperature
(SST)
anomaly
during
diminished
solubility
seawater,
thereby
reducing
uptake.
Moreover,
reduction
nutrient
input
associated
with
drought,
which
is
unfavorable
phytoplankton
growth,
further
capacity
Meanwhile,
doubled
for
offshore
waters
continental
shelf
July-September
2022,
indicating
complexity
heterogeneity
impacts
climatic
seas.
This
study
great
significance
improving
estimation
results
fluxes
understanding
sea–air
exchanges
against
global
change.
Language: Английский
A mapped dataset of surface ocean acidification indicators in large marine ecosystems of the United States
Scientific Data,
Journal Year:
2024,
Volume and Issue:
11(1)
Published: July 2, 2024
Abstract
Mapped
monthly
data
products
of
surface
ocean
acidification
indicators
from
1998
to
2022
on
a
0.25°
by
spatial
grid
have
been
developed
for
eleven
U.S.
large
marine
ecosystems
(LMEs).
The
were
constructed
using
observations
the
Surface
Ocean
CO
2
Atlas,
co-located
properties,
and
two
types
machine
learning
algorithms:
Gaussian
mixture
models
organize
LMEs
into
clusters
similar
environmental
variability
random
forest
regressions
(RFRs)
that
trained
applied
within
each
cluster
spatiotemporally
interpolate
observational
data.
products,
called
RFR-LMEs,
averaged
regional
timeseries
summarize
status
in
coastal
waters,
showing
domain-wide
carbon
dioxide
partial
pressure
increase
1.4
±
0.4
μatm
yr
−1
pH
decrease
0.0014
0.0004
.
RFR-LMEs
evaluated
via
comparisons
discrete
shipboard
data,
fixed
timeseries,
other
mapped
chemistry
products.
Regionally
RFR-LME
are
provided
online
through
NOAA
National
Marine
Ecosystem
Status
web
portal.
Language: Английский
High‐Resolution Neural Network Demonstrates Strong CO2 Source‐Sink Juxtaposition in the Coastal Zone
Journal of Geophysical Research Oceans,
Journal Year:
2024,
Volume and Issue:
129(7)
Published: July 1, 2024
Abstract
The
role
of
coastal
oceans
in
regulating
atmospheric
carbon
dioxide
remains
poorly
quantified
and
understood.
Here,
we
use
a
two‐step
neural
network
approach
to
generate
estimates
from
sparse
observational
data
the
Northeast
Pacific
Ocean
at
an
unprecedented
spatial
resolution
1/12°
with
coverage
nearshore
(0–25
km
offshore).
We
compiled
partial
pressure
(
p
CO
2
)
observations
as
well
range
predictor
variables
including
satellite‐based
physical
oceanographic
reanalysis
products.
With
representing
processes
affecting
,
created
non‐linear
relationships
interpolate
1998
2019.
Compared
situ
shipboard
mooring
observations,
our
product
captures
broad
patterns
seasonal
cycle
variability
well.
A
sensitivity
analysis
identifies
that
parameters
responsible
for
network's
ability
capture
regional
are
associated
mechanistic
processes,
mixed
layer
deepening,
mesoscale
eddies,
gyre
upwelling.
Using
wind
speed
calculated
air‐sea
fluxes.
report
anticorrelation
between
annual
flux
its
amplitude
relationship
driven
by
circulation,
opposing
upwelling/relaxation
versus
downwelling,
effects
winter
mixing
primary
productivity.
show
inclusion
net
outgassing
fluxes
lowers
overall
flux.
Overall,
results
suggest
region
is
sink
(−0.7
mol
m
−2
yr
−1
trends
indicating
increasing
oceanic
uptake
due
strong
connectivity
subsurface
waters.
Language: Английский
Seasonality of pCO2 and air-sea CO2 fluxes in the Central Labrador Sea
Frontiers in Marine Science,
Journal Year:
2024,
Volume and Issue:
11
Published: Oct. 25, 2024
The
Labrador
Sea
in
the
subpolar
North
Atlantic
is
known
for
its
large
air-to-sea
CO
2
fluxes,
which
can
be
around
40%
higher
than
other
regions
of
intense
ocean
uptake
like
Eastern
Pacific
and
within
Northwest
Atlantic.
This
region
also
a
hot-spot
storage
anthropogenic
.
Deep
water
formed
here,
so
that
dissolved
gas
by
surface
directly
connects
to
deeper
waters,
helping
determine
how
much
atmospheric
may
sequestered
(or
released)
deep
ocean.
Currently,
Central
acts
as
year-round
sink
,
with
intensification
driven
biological
production
spring
lasting
through
summer
fall.
Observational
estimates
air-sea
fluxes
rely
upon
very
limited,
scattered
data
distinct
lack
wintertime
observations.
Here,
we
compile
observations
p
from
moorings
underway
measurements,
including
previously
unreported
data,
between
2000
2020,
create
baseline
seasonal
climatology
Sea.
used
reference
compare
against
observational-based
statistical
regional
collection
global
products.
comparison
reveals
systematic
differences
representation
cycle
uncertainties
magnitude
fluxes.
analysis
paramount
importance
long-term,
seasonally-resolved
coverage
this
order
accurately
quantify
size
present
sensitivity
climate
perturbations.
Language: Английский
Enhanced Net Community Production With Sea Ice Loss in the Western Arctic Ocean Uncovered by Machine‐Learning‐Based Mapping
Geophysical Research Letters,
Journal Year:
2024,
Volume and Issue:
51(22)
Published: Nov. 23, 2024
Abstract
In
the
Arctic
Ocean
(AO),
net
community
production
()
has
displayed
spatially
heterogeneous
responses
to
sea
ice
reduction
and
associated
environmental
changes.
Using
a
random
forest
machine
learning
model
trained
with
>42,000
in
situ
measurements
concurrent,
collocated
predictors,
we
reconstructed
19
years
of
8‐day,
6‐km
maps.
During
2015–2021,
integrated
between
late‐May
early‐September
over
western
AO
was
per
year,
interannual
variations
positively
tracking
open
water
area.
While
relationship
area
quasi‐linear
at
high
latitudes,
strong
nonlinearity
detected
on
inflow
shelf.
The
highlights
that
increase
resulted
from
gain
could
be
compounded
by
sea‐ice
loss
induced
ecosystem
adjustments.
Additional
retrospective
analysis
for
2003–2014
suggests
potential
long‐term
export
efficiency
loss.
Language: Английский