Biogeosciences,
Journal Year:
2024,
Volume and Issue:
21(17), P. 3903 - 3926
Published: Sept. 4, 2024
Abstract.
The
ocean
and
the
land
biosphere
are
two
major
sinks
of
anthropogenic
carbon
at
present.
When
emissions
become
zero
temperatures
stabilize,
is
projected
to
dominant
only
global
natural
sink
carbon.
Despite
ocean's
importance
for
cycle
hence
climate,
uncertainties
about
decadal
variability
in
this
underlying
drivers
remain
large
because
observing
detecting
changes
over
time
challenging.
main
tools
that
used
provide
annually
resolved
estimates
last
decades
observation-based
pCO2
products
extrapolate
sparse
observations
space
biogeochemical
models
forced
with
atmospheric
reanalysis
data.
However,
these
(i)
limited
3
7
decades,
which
hinders
statistical
analyses
trends;
(ii)
all
based
on
same
internal
climate
state,
makes
it
impossible
separate
externally
internally
contributions
(iii)
cannot
assess
robustness
future,
especially
when
decline
or
cease
entirely.
Here,
I
use
an
ensemble
12
Earth
system
(ESMs)
from
phase
6
Coupled
Model
Intercomparison
Project
(CMIP6)
understand
trends
past,
present,
future
sink.
simulations
by
ESMs
span
period
1850
2100
include
four
different
Shared
Socioeconomic
Pathways
(SSPs),
low
high
mitigation
mitigation.
Using
ensemble,
show
80
%
can
be
explained
CO2
as
long
remains
smaller
than
4.5
Pg
C
yr−1.
remaining
20
due
heat
uptake,
result
a
loss
ocean.
exceeds
yr−1,
occurs
high-emission
SSP3-7.0
SSP5-8.5,
rises
faster,
change
accelerates,
overturning
chemical
capacity
take
up
atmosphere
reduce,
so
substantially
estimated
trends.
breakdown
relationship
both
pathways
also
implies
increase
effectively
∼1
yr−1
dec−1
pathways,
even
if
trend
continues
increase.
Previously
proposed
drivers,
such
growth
rate
CO2,
explain
specific
periods,
example,
during
exponential
growth,
but
fail
start
decrease
again.
robust
suggests
very
positive
negative
some
highly
unlikely
around
2000
likely
products.
PNAS Nexus,
Journal Year:
2024,
Volume and Issue:
3(4)
Published: March 28, 2024
Human
development
has
ushered
in
an
era
of
converging
crises:
climate
change,
ecological
destruction,
disease,
pollution,
and
socioeconomic
inequality.
This
review
synthesizes
the
breadth
these
interwoven
emergencies
underscores
urgent
need
for
comprehensive,
integrated
action.
Propelled
by
imperialism,
extractive
capitalism,
a
surging
population,
we
are
speeding
past
Earth's
material
limits,
destroying
critical
ecosystems,
triggering
irreversible
changes
biophysical
systems
that
underpin
Holocene
climatic
stability
which
fostered
human
civilization.
The
consequences
actions
disproportionately
borne
vulnerable
populations,
further
entrenching
global
inequities.
Marine
terrestrial
biomes
face
tipping
points,
while
escalating
challenges
to
food
water
access
foreshadow
bleak
outlook
security.
Against
this
backdrop
Earth
at
risk,
call
response
centered
on
decarbonization,
fostering
reciprocity
with
nature,
implementing
regenerative
practices
natural
resource
management.
We
elimination
detrimental
subsidies,
promotion
equitable
development,
transformative
financial
support
lower
income
nations.
A
paradigm
shift
must
occur
replaces
exploitative,
wealth-oriented
capitalism
economic
model
prioritizes
sustainability,
resilience,
justice.
advocate
cultural
elevates
kinship
nature
communal
well-being,
underpinned
recognition
finite
resources
interconnectedness
its
inhabitants.
imperative
is
clear:
navigate
away
from
precipice,
collectively
harness
political
will,
resources,
societal
values
steer
toward
future
where
progress
does
not
come
cost
integrity
social
equity.
Advances in Atmospheric Sciences,
Journal Year:
2024,
Volume and Issue:
41(6), P. 1001 - 1016
Published: April 17, 2024
Globally,
2023
was
the
warmest
observed
year
on
record
since
at
least
1850
and,
according
to
proxy
evidence,
possibly
of
past
100
000
years.
As
in
recent
years,
warmth
has
again
been
accompanied
with
yet
more
extreme
weather
and
climate
events
throughout
world.
Here,
we
provide
an
overview
those
2023,
details
key
background
causes
help
build
upon
our
understanding
roles
internal
variability
anthropogenic
change.
We
also
highlight
emerging
features
associated
some
these
events.
Hot
extremes
are
occurring
earlier
year,
increasingly
simultaneously
differing
parts
world
(e.g.,
concurrent
hot
Northern
Hemisphere
July
2023).
Intense
cyclones
exacerbating
precipitation
North
China
flooding
Libya
September).
Droughts
regions
California
Horn
Africa)
have
transitioned
into
flood
conditions.
Climate
show
increasing
interactions
ecosystems
via
wildfires
Hawaii
August
Canada
from
spring
autumn
2023)
sandstorms
Mongolia
April
Finally,
consider
challenges
research
that
characteristics
present
for
strategy
practice
adaptation.
Climate smart agriculture.,
Journal Year:
2024,
Volume and Issue:
1(1), P. 100003 - 100003
Published: May 3, 2024
Agriculture,
broadly
defined
to
include
crop
and
livestock
production,
forestry,
aquaculture
fishery,
represents
a
key
source
or
sink
of
greenhouse
gas
emissions.
It
is
also
vulnerable
sector
under
climate
change.
The
term
climate-smart
agriculture
has
been
widely
used
since
its
inception
in
2010,
but
no
clear
unified
understanding
scientific
meaning
exists.
Here,
we
systematically
analyzed
the
relationship
between
change
interpreted
definition
agriculture.
We
believe
that
modern
production
approach
coordinatively
promote
food
security,
mitigation
benefits
agricultural
adaptation
towards
Sustainable
Development
Goals.
In
addition,
due
worsening
global
situation,
expounded
on
urgency
major
challenges
promoting
2023
was
the
warmest
year
on
record,
influenced
by
multiple
warm
ocean
basins.
This
has
prompted
speculation
of
an
acceleration
in
surface
warming,
or
a
stronger
than
expected
influence
from
loss
aerosol
induced
cooling.
Here
we
use
recent
Green's
function-based
method
to
quantify
sea
temperature
patterns
global
anomaly,
and
compare
them
previous
record
years.
We
show
that
strong
deviation
warming
trends
is
consistent
with
previously
observed
influences,
regional
forcing.
indicates
internal
variability
contributor
exceptional
evolution,
combination
steady
anthropogenic
warming.
temperatures
fall
line
historical
trends,
anomalies
typical
El
Niño,
indicating
dominance
forcing,
according
analysis
for
isolating
contribution
various
Forecasting,
Journal Year:
2024,
Volume and Issue:
6(1), P. 187 - 203
Published: March 7, 2024
Remotely
sensed
data
play
a
crucial
role
in
monitoring
the
El
Niño/La
Niña
Southern
Oscillation
(ENSO),
which
is
an
oceanic-atmospheric
phenomenon
occurring
quasi-periodically
with
several
impacts
worldwide,
such
as
specific
biological
and
global
climate
responses.
Since
1980,
Earth
has
witnessed
three
strong
ENSO
events
(1982–1983,
1997–1998,
2015–2016).
In
September
2022,
La
entered
its
third
year
was
unlikely
to
continue
through
2024.
Instead,
since
forecasts
have
pointed
transition
from
Neutral
phase
summer
or
late
2023.
The
onset
of
Niño
occurred
around
April
2023,
it
anticipated
by
sophisticated
models
be
event
Northern
Hemisphere
winter
(December
2023–February
2024).
aim
this
study
demonstrate
ability
combination
two
new
methods
improve
accuracy
above
claim
because
apart
anomalies,
significantly
Earth’s
ecosystems
human
societies,
regulating
spread
diseases
insects
(e.g.,
malaria
dengue
fever),
influencing
nutrients,
phytoplankton
biomass,
primary
productivity.
This
done
exploring
first
previous
major
period
January
1876–July
Our
calculations
show
that
ongoing
2023–2024
will
not
strongest.
Surveys in Geophysics,
Journal Year:
2024,
Volume and Issue:
45(6), P. 1757 - 1783
Published: May 7, 2024
Abstract
Satellite
observations
from
the
Clouds
and
Earth’s
Radiant
Energy
System
show
that
energy
imbalance
has
doubled
0.5
±
0.2
Wm
−2
during
first
10
years
of
this
century
to
1.0
−
2
past
decade.
The
increase
is
result
a
0.9
0.3
absorbed
solar
radiation
(ASR)
partially
offset
by
0.4
0.25
in
outgoing
longwave
(OLR).
Despite
marked
differences
ASR
OLR
trends
hiatus
(2000–2010),
transition-to-El
Niño
(2010–2016)
post-El
(2016–2022)
periods,
net
top-of-atmosphere
flux
(NET)
remain
within
0.1
per
decade
one
another,
implying
steady
acceleration
climate
warming.
Northern
southern
hemisphere
NET
are
consistent
0.06
0.31
due
compensation
between
weak
hemispheric
trend
opposite
sign.
We
find
large
decreases
stratocumulus
middle
clouds
over
sub-tropics
low
at
mid-latitudes
primary
reasons
for
increasing
northern
(NH).
These
changes
especially
eastern
Pacific
Ocean,
coincide
with
increases
sea-surface
temperature
(SST).
decrease
cloud
fraction
higher
SSTs
NH
lead
significant
cloud-free
regions,
which
compensate
increase.
Decreases
reflection
weaker
reduction
low-cloud
account
hemisphere,
while
weak.
Changes
cover
response
SST
imply
feedback
change
yet
contribution
radiative
forcing
or
internal
variability
cannot
be
ruled
out.