Review of Policy Research,
Journal Year:
2021,
Volume and Issue:
38(6), P. 732 - 753
Published: Sept. 16, 2021
Abstract
Entering
the
knowledge
society
and
mobilizing
science
technology
are
critical
for
emerging
countries
(ECs)
to
address
important
challenges
of
promote
long‐term
economic
growth.
Natural
laboratories
(NLs)
geographical
or
geophysical
singularities
that
provide
comparative
advantages
leverage
ECs
scientific
research
international
collaboration.
Based
on
empirical
evidence
learning
experiences
from
five
NLs
in
Chile,
we
propose
foundations
a
conceptual
framework
public
policies
based
their
possible
implementation
ECs.
Scientific
may
local,
national,
global
societal
while
decentralizing
activities,
encouraging
transdisciplinary
territories,
anticipating
effects
climate
change,
protecting
biodiversity
promoting
partnerships
alignment
with
2030
Sustainable
Development
Goals.
Journal of Geophysical Research Atmospheres,
Journal Year:
2019,
Volume and Issue:
124(13), P. 7098 - 7146
Published: June 25, 2019
Abstract
New
particle
formation
(NPF)
represents
the
first
step
in
complex
processes
leading
to
of
cloud
condensation
nuclei.
Newly
formed
nanoparticles
affect
human
health,
air
quality,
weather,
and
climate.
This
review
provides
a
brief
history,
synthesizes
recent
significant
progresses,
outlines
challenges
future
directions
for
research
relevant
NPF.
developments
include
emergence
state‐of‐the‐art
instruments
that
measure
prenucleation
clusters
newly
nucleated
down
about
1
nm;
systematic
laboratory
studies
multicomponent
nucleation
systems,
including
collaborative
experiments
conducted
Cosmics
Leaving
Outdoor
Droplets
chamber
at
CERN;
observations
NPF
different
types
forests,
extremely
polluted
urban
locations,
coastal
sites,
polar
regions,
high‐elevation
sites;
improved
theories
parameterizations
account
atmospheric
models.
The
lack
understanding
fundamental
chemical
mechanisms
responsible
aerosol
growth
under
diverse
environments,
effects
SO
2
NO
x
on
NPF,
contribution
anthropogenic
organic
compounds
It
is
also
critical
develop
can
detect
composition
particles
from
3
20
nm
improve
represent
over
wide
range
conditions
precursor,
temperature,
humidity.
Journal of Advances in Modeling Earth Systems,
Journal Year:
2019,
Volume and Issue:
11(12), P. 4323 - 4351
Published: Dec. 1, 2019
Abstract
The
Community
Earth
System
Model
version
2
(CESM2)
includes
three
main
atmospheric
configurations:
the
Atmosphere
6
(CAM6)
with
simplified
chemistry
and
a
organic
aerosol
(OA)
scheme,
CAM6
comprehensive
tropospheric
stratospheric
representation
(CAM6‐chem),
Whole
Climate
(WACCM6).
Both,
CAM6‐chem
WACCM6
include
more
secondary
aerosols
(SOA)
approach
using
Volatility
Basis
Set
(VBS)
scheme
prognostic
aerosols.
This
paper
describes
different
OA
schemes
available
in
configurations
of
CESM2
discusses
differences
burden
resulting
climate
forcings.
Derived
trends
differ
due
to
formation
approaches.
Regional
Aerosol
Optical
Depth
larger
values
occur
over
SOA
source
regions.
Stronger
increasing
between
1960
2015
compared
are
biogenic
emissions
aligned
surface
temperatures.
Using
further
leads
improved
comparisons
aircraft
observations
≈143
Tg/yr.
We
use
identify
contributions
from
biogenic,
fossil
fuel,
biomass
burning
emissions,
quantify
amounts
these
sources.
Increasing
result
Biogenic
at
least
two
thirds
total
burden.
In
addition,
fuel
become
important,
largest
Southeast
Asia.
estimated
anthropogenic
forcing
for
1995–2010
conditions
is
−0.43
W/m
,
mostly
direct
effect.
Atmospheric chemistry and physics,
Journal Year:
2021,
Volume and Issue:
21(11), P. 8455 - 8478
Published: June 3, 2021
Abstract.
The
atmospheric
processes
under
polluted
environments
involving
interactions
of
anthropogenic
pollutants
and
natural
emissions
lead
to
the
formation
various
complex
secondary
products.
Therefore,
characterization
oxygenated
organic
compounds
in
urban
areas
remains
a
pivotal
issue
our
understanding
evolution
carbon.
Here,
we
describe
measurements
an
iodide
chemical
ionization
time-of-flight
mass
spectrometer
installed
with
Filter
Inlet
for
Gases
AEROsols
(FIGAERO-I-CIMS)
both
gas
phase
particle
at
site
Guangzhou,
typical
megacity
southern
China,
during
autumn
2018.
Abundant
containing
two
five
oxygen
atoms
were
observed,
including
acids,
multi-functional
typically
emitted
from
biomass
burning,
oxidation
products
biogenic
hydrocarbons
aromatics.
Photochemistry
played
dominant
roles
gaseous
acids
isoprene-derived
nitrates,
while
nighttime
chemistry
contributed
significantly
monoterpene-derived
nitrates
inorganics.
Nitrogen-containing
occupied
significant
fraction
total
signal
phases,
elevated
fractions
higher
molecular
weights.
Measurements
by
FIGAERO-I-CIMS
explained
24
±
0.8
%
aerosol
measured
(AMS),
increased
more
aged
aerosol.
systematical
interpretation
spectra
area
Guangzhou
provides
holistic
view
numerous
atmosphere,
which
can
serve
as
reference
future
field
regions.
Tellus B,
Journal Year:
2022,
Volume and Issue:
74(1), P. 24 - 24
Published: March 25, 2022
This
review
presents
how
the
boreal
and
tropical
forests
affect
atmosphere,
its
chemical
composition,
function,
further
that
affects
climate
and,
in
return,
ecosystems
through
feedback
processes.
Observations
from
key
tower
sites
standing
out
due
to
their
long-term
comprehensive
observations:
The
Amazon
Tall
Tower
Observatory
Central
Amazonia,
Zotino
Siberia,
Station
Measure
Ecosystem-Atmosphere
Relations
at
Hyytiäla
Finland.
is
complemented
by
short-term
observations
networks
large
experiments.
discusses
atmospheric
chemistry
observations,
aerosol
formation
processing,
physiochemical
aerosol,
cloud
condensation
nuclei
properties
finds
surprising
similarities
important
differences
two
ecosystems.
concentrations
are
similar,
particularly
concerning
main
components,
both
dominated
an
organic
fraction,
while
ecosystem
has
generally
higher
of
inorganics,
influence
long-range
transported
air
pollution.
emissions
biogenic
volatile
compounds
isoprene
monoterpene
regions,
respectively,
being
precursors
fraction.
modeling
studies
show
change
deforestation
such
carbon
hydrological
cycles
Amazonia
changing
neutrality
precipitation
downwind.
In
Africa,
so
far
maintaining
sink.
It
urgent
better
understand
interaction
between
these
major
ecosystems,
climate,
which
calls
for
more
observation
sites,
providing
data
on
water,
carbon,
other
biogeochemical
cycles.
essential
finding
a
sustainable
balance
forest
preservation
reforestation
versus
potential
increase
food
production
biofuels,
critical
services
global
stability.
Reducing
warming
vital
forests.
ACS Earth and Space Chemistry,
Journal Year:
2019,
Volume and Issue:
3(12), P. 2646 - 2658
Published: Oct. 31, 2019
Isoprene-derived
secondary
organic
aerosol
(SOA)
is
mainly
formed
through
acid-catalyzed
reactive
uptake
of
isoprene-derived
epoxydiols
(IEPOX)
onto
sulfate
particles.
The
effect
IEPOX-derived
SOA
on
the
physicochemical
properties
existing
aerosols
and
resulting
capacity
for
further
formation
remains
unclear.
This
study
systematically
examined
influences
phase
state,
morphology,
acidity
pre-existing
particles,
as
well
their
implications
reactivity
evolution
these
By
combining
thermodynamic
viscosity
modeling,
our
predictions
show
that
change
drastically
after
IEPOX
uptake,
with
becoming
less
acidic
(increasing
by
up
to
1.5
pH
units)
more
viscous
7
orders
magnitude,
thereby
significantly
reducing
diffusion
time
scale
molecules
inside
Decreased
increased
co-contribute
a
self-limiting
where
newly
inhibits
additional
multiphase
chemical
reactions
IEPOX.
relative
contribution
inhibitory
versus
depends
initial
ratio
IEPOX-to-inorganic
aerosol,
which
differs
between
geographic
regions.
Moreover,
reduced
kinetic
limitation
leading
lower
hydronium
ions
slower
mixing
times
may
impede
other
processes
SOA.
highlights
important
interconnections
physical
particles
come
from
interactions
inorganic
components,
jointly
influence
atmospheric
aerosols.
Atmospheric chemistry and physics,
Journal Year:
2019,
Volume and Issue:
19(19), P. 12749 - 12766
Published: Oct. 11, 2019
Abstract.
Atmospheric
organic
nitrate
(ON)
is
thought
to
play
a
crucial
role
in
the
formation
potential
of
ozone
and
aerosol,
which
are
leading
air
pollutants
concern
across
world.
Limited
fundamental
knowledge
understanding
life
cycles
ON
currently
hinder
ability
quantitatively
assess
its
impacts
on
these
pollutants.
Although
hydrolysis
considered
an
important
loss
mechanism
based
prior
field
measurement
studies,
this
process
for
atmospherically
relevant
has
not
been
well
constrained
by
laboratory
studies.
In
comprehensive
study,
we
investigated
chemical
composition
particulate
(pON)
formed
from
oxidation
α-pinene
β-pinene
hydroxyl
(OH⚫)
radicals
(NO3⚫).
For
pON
that
undergoes
hydrolysis,
lifetime
determined
be
no
more
than
30
min
all
systems
explored.
This
significantly
shorter
those
reported
previous
chamber
studies
(i.e.,
3–6
h)
but
consistent
with
bulk
solution
0.02–8.8
h).
The
discrepancy
appears
stem
choice
proxy
used
estimate
lifetime.
measured
hydrolyzable
fractions
(FH)
+
OH⚫,
NO3⚫,
NO3⚫
23
%–32
%,
27
%–34
9
%–17
%–15
respectively.
While
very
low
FH
system
expected
OH⚫
surprisingly
lower
predicted
past
Overall,
as
obtained
study
serve
experimentally
parameters
required
regional
global
transport
models
accurately
evaluate
nitrogen
budget
aerosol.
Proceedings of the National Academy of Sciences,
Journal Year:
2020,
Volume and Issue:
117(41), P. 25344 - 25351
Published: Sept. 28, 2020
Significance
The
high-altitude
tropics
constitute
one
of
the
world’s
largest
aerosol
reservoirs,
which
may
significantly
affect
clouds,
radiation,
and
hydrological
cycle
by
delivering
seeds
on
clouds
form
to
lower
altitudes
maintaining
stratospheric
background.
However,
formation
mechanisms
these
aerosols
remain
a
scientific
mystery.
Through
systematic
experiment-based
model
representation
organic
chemistry
new
particle
(NPF)
combined
with
constraints
from
field
measurements,
we
demonstrate
that
NPF
driven
extremely
low
volatility
organics
formed
biogenic
emissions
plays
key
role
in
producing
large
number
observed
Amazon.
This
mechanism
likely
also
prevailed
during
preindustrial
times
hence
modulate
anthropogenic
forcing
above
baseline.