Journal of Geophysical Research Atmospheres,
Journal Year:
2022,
Volume and Issue:
127(18)
Published: Aug. 19, 2022
Abstract
We
investigate
the
dependence
of
radiative
feedback
on
pattern
sea‐surface
temperature
(SST)
change
in
14
Atmospheric
General
Circulation
Models
(AGCMs)
forced
with
observed
variations
SST
and
sea‐ice
over
historical
record
from
1871
to
near‐present.
find
that
1871–1980,
Earth
warmed
feedbacks
largely
consistent
strongly
correlated
long‐term
climate
sensitivity
(diagnosed
corresponding
atmosphere‐ocean
GCM
abrupt‐4xCO2
simulations).
Post
1980,
however,
unusual
trends
tropical
Pacific
SSTs
(enhanced
warming
west,
cooling
east)
Southern
Ocean
drove
be
uncorrelated
with—and
indicating
much
lower
than—that
expected
for
CO
2
increase.
show
these
conclusions
are
not
dependent
Model
Intercomparison
Project
(AMIP)
II
data
set
used
force
AGCMs,
though
magnitude
post
1980
is
generally
smaller
nine
AGCMs
alternative
HadISST1
boundary
conditions.
quantify
a
“pattern
effect”
(defined
as
difference
between
feedback)
equal
0.48
±
0.47
[5%–95%]
W
m
−2
K
−1
time‐period
1871–2010
when
SSTs,
or
0.70
AMIP
SSTs.
Assessed
changes
Earth's
energy
budget
agree
AGCM
estimates.
Furthermore
satellite
observations
top‐of‐atmosphere
fluxes
since
1985
suggest
effect
was
particularly
strong
recent
decades
but
may
waning
2014.
Abstract
In
recent
decades,
the
warming
in
Arctic
has
been
much
faster
than
rest
of
world,
a
phenomenon
known
as
amplification.
Numerous
studies
report
that
is
either
twice,
more
or
even
three
times
fast
globe
on
average.
Here
we
show,
by
using
several
observational
datasets
which
cover
region,
during
last
43
years
nearly
four
globe,
higher
ratio
generally
reported
literature.
We
compared
observed
amplification
with
simulated
state-of-the-art
climate
models,
and
found
four-fold
over
1979–2021
an
extremely
rare
occasion
model
simulations.
The
ratios
are
consistent
each
other
if
calculated
longer
period;
however
comparison
obscured
uncertainties
before
1979.
Our
results
indicate
unlikely
event,
models
systematically
tend
to
underestimate
Quarterly Journal of the Royal Meteorological Society,
Journal Year:
2021,
Volume and Issue:
147(741), P. 4186 - 4227
Published: Sept. 24, 2021
Abstract
The
extension
of
the
ERA5
reanalysis
back
to
1950
supplements
previously
published
segment
covering
1979
present.
It
features
assimilation
additional
conventional
observations,
as
well
improved
use
early
satellite
data.
number
observations
assimilated
increases
from
53,000
per
day
in
570,000
by
end
1978.
Accordingly,
quality
improves
throughout
period,
generally
joining
seamlessly
with
fidelity
is
illustrated
accurate
depiction
North
Sea
storm
1953,
and
events
leading
first
discovery
sudden
stratospheric
warmings
1952.
Time
series
global
surface
temperature
anomalies
show
temperatures
be
relatively
stable
until
late
1970s,
agreement
other
contemporary
full‐input
this
period
independent
data
sets,
although
there
are
significant
differences
accuracy
representing
specific
regions,
Europe
being
represented
but
Australia
less
so.
variability
precipitation
month
agrees
for
all
continents,
correlations
above
90%
most
excess
70%
America,
Asia
Australia.
evolution
upper
air
temperatures,
humidities
winds
shows
smoothly
varying
behaviour,
including
tropospheric
warming
cooling,
modulated
volcanic
eruptions.
Quasi‐Biennial
Oscillation
throughout.
Aspects
upon
future
reanalyses
include
tropical
cyclone
data,
spin‐up
soil
moisture
humidity,
representation
over
Earth system science data,
Journal Year:
2020,
Volume and Issue:
12(4), P. 3469 - 3479
Published: Dec. 17, 2020
Abstract.
A
global
land–ocean
temperature
record
has
been
created
by
combining
the
Berkeley
Earth
monthly
land
field
with
spatially
kriged
version
of
HadSST3
dataset.
This
combined
product
spans
period
from
1850
to
present
and
covers
majority
Earth's
surface:
approximately
57
%
in
1850,
75
1880,
95
1960,
99.9
2015.
It
includes
average
temperatures
1∘×1∘
lat–long
grid
cells
for
each
month
when
available.
provides
a
mean
quite
similar
records
Hadley's
HadCRUT4,
NASA's
GISTEMP,
NOAA's
GlobalTemp,
Cowtan
Way
complete
homogeneous
field.
Two
versions
are
provided,
treating
areas
sea
ice
cover
as
either
air
over
or
surface
under
ice,
former
being
preferred
most
applications.
The
choice
how
assess
coverage
notable
impact
on
anomalies
past
decades
due
rapid
warming
Arctic.
Accounting
Arctic
suggests
∼
0.1
∘C
additional
global-average
rise
since
19th
century
than
series
that
do
not
capture
changes
Updated
this
dataset
will
be
presented
at
website
(http://berkeleyearth.org/data/,
last
access:
November
2020),
convenience
copy
discussed
paper
archived
is
freely
available
https://doi.org/10.5281/zenodo.3634713
(Rohde
Hausfather,
2020).
Journal of Advances in Modeling Earth Systems,
Journal Year:
2022,
Volume and Issue:
14(3)
Published: Feb. 11, 2022
Abstract
This
article
introduces
the
second
generation
CMCC
Earth
System
Model
(CMCC‐ESM2)
that
extends
a
number
of
marine
and
terrestrial
biogeochemical
processes
with
respect
to
its
CMIP5
predecessor.
In
particular,
land
biogeochemistry
was
extended
wider
set
carbon
pools
plant
functional
types,
along
prognostic
representation
nitrogen
cycle.
The
ecosystem
reshaped
toward
an
intermediate
complexity
lower
trophic
level
interactions,
including
interactive
benthic
compartment
new
formulation
heterotrophic
bacterial
population.
Details
are
provided
on
model
setup
implementation
for
different
experiments
performed
as
contribution
sixth
phase
Coupled
Intercomparison
Project.
CMCC‐ESM2
shows
equilibrium
climate
sensitivity
3.57°C
transient
response
1.97°C
which
close
CMIP6
multi‐model
averages.
evaluation
coupled
climate‐carbon
in
historical
period
against
available
observational
datasets
show
consistent
both
physical
quantities.
However,
sink
is
found
be
weaker
than
current
global
estimates
simulated
primary
production
slightly
below
satellite‐based
average
over
recent
decades.
Future
projections
coherently
prominent
warming
northern
hemisphere
intensified
precipitations
at
high
latitudes.
expected
ranges
variability
oceanic
pH
oxygen,
well
soil
storage,
compare
favorably
those
assessed
from
other
models.
Nature Climate Change,
Journal Year:
2022,
Volume and Issue:
12(4), P. 350 - 355
Published: March 14, 2022
Compound
hot–dry
events—co-occurring
hot
and
dry
extremes—frequently
cause
damages
to
human
natural
systems,
often
exceeding
separate
impacts
from
heatwaves
droughts.
Strong
increases
in
the
occurrence
of
these
events
are
projected
with
warming,
but
associated
uncertainties
remain
large
poorly
understood.
Here,
using
climate
model
ensembles,
we
show
that
mean
precipitation
trends
exclusively
modulate
future
compound
over
land.
This
occurs
because
local
warming
will
be
enough
droughts
always
coincide
at
least
moderately
extremes,
even
a
2
°C
warmer
world.
By
contrast,
weak
equivocal
sign,
depending
on
model,
region
internal
variability.
Therefore,
constraining
regional
also
constrain
events.
These
results
help
assess
frequencies
other
extremes
characterized
by
strongly
different
drivers.
Co-occurring
predicted
increase
global
warming.
Changes
extent
changes,
highlighting
importance
understanding
prepare
society
minimize
impacts.
Scientific Data,
Journal Year:
2023,
Volume and Issue:
10(1)
Published: Oct. 23, 2023
We
introduce
Version
2
of
our
widely
used
1-km
Köppen-Geiger
climate
classification
maps
for
historical
and
future
conditions.
The
(encompassing
1901-1930,
1931-1960,
1961-1990,
1991-2020)
are
based
on
high-resolution,
observation-based
climatologies,
while
the
2041-2070
2071-2099)
downscaled
bias-corrected
projections
seven
shared
socio-economic
pathways
(SSPs).
evaluated
67
models
from
Coupled
Model
Intercomparison
Project
phase
6
(CMIP6)
kept
a
subset
42
with
most
plausible
CO2-induced
warming
rates.
estimate
that
1901-1930
to
1991-2020,
approximately
5%
global
land
surface
(excluding
Antarctica)
transitioned
different
major
class.
Furthermore,
we
project
1991-2020
2071-2099,
will
transition
class
under
low-emissions
SSP1-2.6
scenario,
8%
middle-of-the-road
SSP2-4.5
13%
high-emissions
SSP5-8.5
scenario.
maps,
along
associated
confidence
estimates,
underlying
monthly
air
temperature
precipitation
data,
sensitivity
metrics
CMIP6
models,
can
be
accessed
at
www.gloh2o.org/koppen
.