Environmental Research Letters,
Journal Year:
2019,
Volume and Issue:
14(12), P. 123006 - 123006
Published: Sept. 18, 2019
This
review
addresses
the
causes
of
observed
climate
variations
across
industrial
period,
from
1750
to
present.
It
focuses
on
long-term
changes,
both
in
response
external
forcing
and
variability
ocean
atmosphere.
A
synthesis
results
attribution
studies
based
palaeoclimatic
reconstructions
covering
recent
few
centuries
20th
century,
instrumental
data
shows
how
greenhouse
gases
began
cause
warming
since
beginning
industrialization,
causing
trends
that
are
attributable
by
1900
proxy-based
temperature
reconstructions.
Their
influence
increased
over
time,
dominating
trends.
However,
other
forcings
have
caused
substantial
deviations
this
emerging
trend:
volcanic
eruptions
strong
cooling
following
a
period
unusually
heavy
activity,
such
as
early
19th
century;
or
during
periods
low
early-to-mid
century.
Anthropogenic
aerosol
most
likely
masked
some
global
especially
accelerated
increase
sulphate
emissions
starting
around
1950.
Based
modelling
studies,
has
also
influenced
regional
temperatures,
changes
monsoons
imprinted
Atlantic
variability.
Multi-decadal
atmospheric
modes
can
variability,
apparent
for
example
North
Oscillation,
Long-term
precipitation
more
difficult
attribute
due
spatial
sparseness
noisiness
but
pattern
station
supports
model
simulated
with
it,
predictions.
The
led
significant
differences
daily
as,
example,
visible
long
European
data.
Extreme
events
historical
record
provide
valuable
samples
possible
extreme
their
mechanisms.
Journal of Climate,
Journal Year:
2017,
Volume and Issue:
30(20), P. 8179 - 8205
Published: July 19, 2017
Abstract
The
monthly
global
2°
×
Extended
Reconstructed
Sea
Surface
Temperature
(ERSST)
has
been
revised
and
updated
from
version
4
to
5.
This
update
incorporates
a
new
release
of
ICOADS
3.0
(R3.0),
decade
near-surface
data
Argo
floats,
estimate
centennial
sea
ice
HadISST2.
A
number
choices
in
aspects
quality
control,
bias
adjustment,
interpolation
have
substantively
revised.
resulting
ERSST
estimates
more
realistic
spatiotemporal
variations,
better
representation
high-latitude
SSTs,
ship
SST
biases
are
now
calculated
relative
accurate
buoy
measurements,
while
the
long-term
trend
remains
about
same.
Progressive
experiments
undertaken
highlight
effects
each
change
source
analysis
technique
upon
final
product.
reconstructed
is
systematically
decreased
by
0.077°C,
as
reference
switched
ERSSTv4
modern
ERSSTv5.
Furthermore,
SSTs
0.1°–0.2°C
using
concentration
HadISST2
over
HadISST1.
Changes
arising
remaining
innovations
mostly
important
at
small
space
time
scales,
primarily
having
an
impact
where
when
input
observations
sparse.
Cross
validations
verifications
with
independent
show
that
updates
incorporated
ERSSTv5
improved
spatial
variability
oceans,
magnitude
El
Niño
La
Niña
events,
decadal
nature
changes
1930s–40s
observation
instruments
changed
rapidly.
Both
long-
(1900–2015)
short-term
(2000–15)
trends
remain
significant
ERSSTv4.
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
Reviews of Geophysics,
Journal Year:
2020,
Volume and Issue:
58(4)
Published: July 22, 2020
We
assess
evidence
relevant
to
Earth's
equilibrium
climate
sensitivity
per
doubling
of
atmospheric
CO2,
characterized
by
an
effective
S.
This
includes
feedback
process
understanding,
the
historical
record,
and
paleoclimate
record.
An
S
value
lower
than
2
K
is
difficult
reconcile
with
any
three
lines
evidence.
The
amount
cooling
during
Last
Glacial
Maximum
provides
strong
against
values
greater
4.5
K.
Other
in
combination
also
show
that
this
relatively
unlikely.
use
a
Bayesian
approach
produce
probability
density
function
(PDF)
for
given
all
evidence,
including
tests
robustness
difficult-to-quantify
uncertainties
different
priors.
66%
range
2.6–3.9
our
Baseline
calculation
remains
within
2.3–4.5
under
tests;
corresponding
5–95%
ranges
are
2.3–4.7
K,
bounded
2.0–5.7
(although
such
high-confidence
should
be
regarded
more
cautiously).
indicates
stronger
constraint
on
reported
past
assessments,
lifting
low
end
range.
narrowing
occurs
because
agree
judged
largely
independent
confidence
understanding
processes
combining
identify
promising
avenues
further
S,
particular
using
comprehensive
models
address
limitations
traditional
forcing-feedback
paradigm
interpreting
changes.
Journal of Geophysical Research Atmospheres,
Journal Year:
2019,
Volume and Issue:
124(12), P. 6307 - 6326
Published: May 23, 2019
Abstract
We
outline
a
new
and
improved
uncertainty
analysis
for
the
Goddard
Institute
Space
Studies
Surface
Temperature
product
version
4
(GISTEMP
v4).
Historical
spatial
variations
in
surface
temperature
anomalies
are
derived
from
historical
weather
station
data
ocean
ships,
buoys,
other
sensors.
Uncertainties
arise
measurement
uncertainty,
changes
coverage
of
record,
systematic
biases
due
to
technology
shifts
land
cover
changes.
Previously
published
estimates
GISTEMP
included
only
effect
incomplete
coverage.
Here,
we
update
this
term
using
currently
available
distributions
source
data,
state‐of‐the‐art
reanalyses,
incorporate
independently
processing,
homogenization,
structural
biases.
The
resulting
95%
uncertainties
near
0.05
°C
global
annual
mean
last
50
years
increase
going
back
further
time
reaching
0.15
1880.
In
addition,
quantify
benefits
inherent
interpolation
averaging
method.
use
total
estimate
probability
each
record
year
actually
be
true
(to
that
date)
conclude
with
87%
likelihood
2016
was
indeed
hottest
instrumental
period
(so
far).
Journal of Geophysical Research Atmospheres,
Journal Year:
2020,
Volume and Issue:
126(3)
Published: Dec. 15, 2020
Abstract
We
present
a
new
version
of
the
Met
Office
Hadley
Centre/Climatic
Research
Unit
global
surface
temperature
data
set,
HadCRUT5.
HadCRUT5
presents
monthly
average
near‐surface
anomalies,
relative
to
1961–1990
period,
on
regular
5°
latitude
by
longitude
grid
from
1850
2018.
is
combination
sea‐surface
(SST)
measurements
over
ocean
ships
and
buoys
air
weather
stations
land
surface.
These
have
been
sourced
updated
compilations
adjustments
applied
mitigate
impact
changes
in
SST
measurement
methods
revised.
Two
variants
produced
for
use
different
applications.
The
first
represents
anomaly
locations
where
are
available.
second,
more
spatially
complete,
variant
uses
Gaussian
process
based
statistical
method
make
better
available
observations,
extending
estimates
into
regions
which
underlying
informative.
Each
provided
as
200‐member
ensemble
accompanied
additional
uncertainty
information.
revised
input
sets
analysis
results
greater
warming
course
whole
record.
In
recent
years,
increased
an
improved
representation
Arctic
understanding
evolving
biases
ships.
updates
result
consistency
with
other
independent
sets,
despite
their
approaches
set
construction,
further
increase
confidence
our
seen.
Global Biogeochemical Cycles,
Journal Year:
2019,
Volume and Issue:
33(3), P. 318 - 342
Published: Feb. 5, 2019
Abstract
Atmospheric
methane
grew
very
rapidly
in
2014
(12.7
±
0.5
ppb/year),
2015
(10.1
0.7
2016
(7.0
and
2017
(7.7
at
rates
not
observed
since
the
1980s.
The
increase
burden
began
2007,
with
mean
global
mole
fraction
remote
surface
background
air
rising
from
about
1,775
ppb
2006
to
1,850
2017.
Simultaneously
13
C/
12
C
isotopic
ratio
(expressed
as
δ
CH4
)
has
shifted,
now
trending
negative
for
more
than
a
decade.
causes
of
methane's
recent
are
therefore
either
change
relative
proportions
(and
totals)
emissions
biogenic
thermogenic
pyrogenic
sources,
especially
tropics
subtropics,
or
decline
atmospheric
sink
methane,
both.
Unfortunately,
limited
measurement
data
sets,
it
is
currently
possible
be
definitive.
climate
warming
impact
over
past
decade,
if
continued
>5
ppb/year
coming
decades,
sufficient
challenge
Paris
Agreement,
which
requires
sharp
cuts
burden.
However,
anthropogenic
relatively
large
thus
offer
attractive
targets
rapid
reduction,
essential
Agreement
aims
attained.
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