Environmental Science & Technology Letters,
Journal Year:
2024,
Volume and Issue:
11(7), P. 738 - 745
Published: June 21, 2024
Semivolatile
and
intermediate
volatility
organic
compounds
(S/IVOCs)
are
known
as
crucial
precursors
of
secondary
aerosols
(SOA),
yet
their
specific
contributions
to
SOA
in
urban
areas
remain
unclear.
Here,
we
investigate
the
real-time
formation
from
ambient
air
summer
Beijing
utilizing
an
oxidation
flow
reactor
(OFR),
coupled
with
aerosol
proton-transfer-reaction
mass
spectrometers.
Our
results
show
that
maximum
photochemical
OFR
reached
2.9
μg
m–3
at
∼1.5
days
age.
Primary
OA
less
oxidized
oxygenated
experience
loss
high
ages
(>3
days)
OFR,
whereas
more
continues
enhancement,
indicating
role
heterogeneous
processes
highly
aged
SOA.
Closure
studies
demonstrate
estimated
contribute
50.0
±
17.3%
measured
The
relatively
low
contribution
(10.3
5.2%)
IVOCs
emphasizes
importance
unmeasured
S/IVOCs
formation.
Furthermore,
illustrate
impact
heat
waves
on
by
enhancing
biogenic
emissions
summer.
Weather and Climate Dynamics,
Journal Year:
2024,
Volume and Issue:
5(1), P. 323 - 343
Published: March 1, 2024
Abstract.
Extreme
heatwaves
are
one
of
the
most
impactful
natural
hazards,
posing
risks
to
human
health,
infrastructure,
and
ecosystems.
Recent
theoretical
observational
studies
have
suggested
that
vertical
temperature
structure
during
limits
magnitude
near-surface
heat
through
convective
instability.
In
this
study,
we
thus
examine
in
detail
three
recent
record-shattering
heatwaves,
Pacific
Northwest
(PNW)
heatwave
2021,
western
Russian
(RU)
2010,
European
UK
(UK)
2022,
by
decomposing
anomalies
(T′)
entire
tropospheric
column
above
surface
into
contributions
from
advection,
adiabatic
warming
cooling,
diabatic
processes.
All
exhibited
bottom-heavy
yet
vertically
deep
positive
T′
extending
throughout
troposphere.
Importantly,
though,
underlying
physical
processes
varied
greatly
within
each
heatwave,
as
well
across
distinct
reflecting
diverse
synoptic
storylines
these
events.
The
PNW
was
strongly
influenced
an
upstream
cyclone
associated
warm
conveyor
belt,
which
amplified
extreme
quasi-stationary
ridge
generated
substantial
mid-
upper-tropospheric
advection
heating.
some
contrast,
RU
caused
while
it
modest
latent
heating
only
early
phase
respective
ridge.
Adiabatic
notably
contributed
positively
lower-tropospheric
all
but
lowermost
200–300
hPa.
Near
surface,
negligible
heatwave.
Moreover,
there
is
clear
evidence
amplification
downward
propagation
whereby
maximum
coincided
with
arrival
boundary
layer.
Additionally,
widespread
ageing
over
course
events
fully
consistent
notion
domes,
air
recirculates
accumulates
heat.
Our
results
for
first
time
document
four-dimensional
functioning
anticyclone–heatwave
couplets
terms
cooling
or
warming,
suggest
a
complex
interplay
between
large-scale
dynamics,
moist
convection,
layer
ultimately
determines
temperatures
heatwaves.
Weather and Climate Extremes,
Journal Year:
2023,
Volume and Issue:
40, P. 100569 - 100569
Published: May 4, 2023
This
study
describes
the
climatological
characteristics
of
regional
heat
waves
(HWs)
over
southern
South
America
(SSA)
for
warm
seasons
(October–March)
1979–2018
based
on
daily
maximum
temperature
series
from
131
weather
stations.
Clustering
stations
with
high
co-occurrence
simultaneous
HW
days
is
employed
to
identify
events
five
homogeneous
regions:
northern,
central-eastern
and
SSA
regions,
central
Argentina,
Chile.
When
all
regions
are
considered,
we
find
a
mean
frequency
∼4
HWs
per
year.
Transitional
(northern
SSA,
Argentina)
characterised
by
longer,
albeit
less
intense,
than
southernmost
region
(southern
SSA),
whereas
Chile
display
lowest
duration,
intensity
extension.
By
aggregating
these
single
attributes
into
combined
severity
index,
ranking
historical
has
been
obtained,
March
1980
event
standing
as
most
severe
one
SSA.
The
assessment
long-term
changes
reveals
significant
increases
in
Argentina
only.
Trends
also
dependent,
only
where
increased
significantly.
We
report
similarities
differences
synoptic
circulation
patterns
associated
events.
Southern
have
distinctive
signatures,
related
extratropical
high-pressure
systems
blocking
westerly
flow.
In
remaining
anomalies
Atlantic
or
Pacific
(central
Chile)
High,
intensification
northerly
low-level
flow
thermal
lows
American
Low
Level
Jet
Regional
often
migrate
northern
following
displacement/intensification
which
partially
explains
similarity
their
patterns.
Proceedings of the National Academy of Sciences,
Journal Year:
2024,
Volume and Issue:
121(49)
Published: Nov. 26, 2024
Multiple
recent
record-shattering
weather
events
raise
questions
about
the
adequacy
of
climate
models
to
effectively
predict
and
prepare
for
unprecedented
impacts
on
human
life,
infrastructure,
ecosystems.
Here,
we
show
that
extreme
heat
in
several
regions
globally
is
increasing
significantly
faster
magnitude
than
what
state-of-the-art
have
predicted
under
present
warming
even
after
accounting
their
regional
summer
background
warming.
Across
all
global
land
area,
underestimate
positive
trends
exceeding
0.5
°C
per
decade
widening
upper
tail
surface
temperature
distributions
by
a
factor
four
compared
reanalysis
data
exhibit
lower
fraction
overall.
To
lesser
degree,
also
observed
strong
contraction
tails
some
areas,
while
moderate
are
well
reproduced
perspective.
Our
results
highlight
need
better
understand
model
drivers
rapidly
mitigate
greenhouse
gas
emissions
avoid
further
harm
from
unexpected
events.
Environmental Science & Technology Letters,
Journal Year:
2024,
Volume and Issue:
11(7), P. 738 - 745
Published: June 21, 2024
Semivolatile
and
intermediate
volatility
organic
compounds
(S/IVOCs)
are
known
as
crucial
precursors
of
secondary
aerosols
(SOA),
yet
their
specific
contributions
to
SOA
in
urban
areas
remain
unclear.
Here,
we
investigate
the
real-time
formation
from
ambient
air
summer
Beijing
utilizing
an
oxidation
flow
reactor
(OFR),
coupled
with
aerosol
proton-transfer-reaction
mass
spectrometers.
Our
results
show
that
maximum
photochemical
OFR
reached
2.9
μg
m–3
at
∼1.5
days
age.
Primary
OA
less
oxidized
oxygenated
experience
loss
high
ages
(>3
days)
OFR,
whereas
more
continues
enhancement,
indicating
role
heterogeneous
processes
highly
aged
SOA.
Closure
studies
demonstrate
estimated
contribute
50.0
±
17.3%
measured
The
relatively
low
contribution
(10.3
5.2%)
IVOCs
emphasizes
importance
unmeasured
S/IVOCs
formation.
Furthermore,
illustrate
impact
heat
waves
on
by
enhancing
biogenic
emissions
summer.