Abstract.
Stratospheric
aerosols
are
long-lived
and
play
a
critical
role
in
the
global
radiation
budget.
Over
past
decade,
contributions
to
stratospheric
from
different
sources
have
changed
due
weaker
volcanic
activity
more
frequent
wildfire
events.
However,
long-term
observations
of
monitoring
major
emission
events
remain
insufficient,
particularly
at
middle
low
latitudes.
In
this
study,
we
analyze
vertical
distribution,
optical
properties,
radiative
forcing
using
ground-based
polarization
lidar
Wuhan
(30.5°
N,
114.4°
E)
2010
2021.
The
aerosol
depth
(sAOD)
generally
stabilized
around
0.0023
without
significant
annual
variation.
Several
cases
wildfire-induced
smoke
were
observed.
Volcanic
Nabro
(2011)
Raikoke
(2019)
eruptions
(both
boreal
summer)
increased
sAOD
4.8
times
background
level
during
stratospheric-quiescent
period
(January
2013
August
2017).
Tracers
Canadian
summer
2017
was
observed
twice:
19–21
km
on
14–17
September
20–23
28–31
October,
with
plume-isolated
AOD
0.002–0.010
particle
linear
depolarization
ratio
δp
0.14–0.18,
indicating
dominance
non-aged
particles.
During
these
summertime
events,
injected
captured
by
large-scale
Asian
monsoon
anticyclone
(AMA),
confining
transport
pathway
mid-latitude
Asia.
On
8–9
November
2020,
plumes
originating
California
October
2020
appeared
16–17
km,
0.007
mean
0.13.
Regarding
seasonal
variation,
cold
half-year
(0.0026)
is
24
%
larger
than
warm
(0.0021)
stronger
meridional
tropics
-0.05
W·m-2
-0.28
when
largely
injected.
These
findings
contribute
our
understanding
patterns
over
Asia
serve
as
important
database
for
validation
model
outputs.
Remote Sensing,
Journal Year:
2023,
Volume and Issue:
15(24), P. 5734 - 5734
Published: Dec. 15, 2023
Dust
plays
a
very
important
role
in
the
Earth’s
climate
system
by
its
direct
and
indirect
effects.
Deserts
northwestern
China
contribute
large
amount
of
dust
particles,
both
inland
outside,
while
vertical
distribution
transport
mechanism
still
have
many
uncertainties.
Using
Level
3
cloud-free
monthly
aerosol
products
Cloud–Aerosol
Lidar
Infrared
Pathfinder
Satellite
Observations
(CALIPSO)
from
2007
to
2020,
we
analyzed
spatial
temporal
variations
features
for
polluted
aerosols
over
surrounding
areas.
The
results
show
that
Taklimakan
Desert
(TD)
Thar
(TRD)
always
act
as
high-value
centers
optical
depth
(DOD),
(PDOD)
are
located
eastern
China,
Sichuan
Basin
Indian
subcontinent.
DOD
shows
an
increasing
trend
most
areas,
PDOD
presents
significant
decrease
increase
central
India,
respectively.
largest
appears
spring
TD
Gobi
(GD),
summer
is
TRD.
Although
dusts
TRD
concentrated
below
4
km,
they
may
be
higher
TD.
Most
confined
under
2
km.
input
Tibetan
Plateau
(TP)
could
come
occurs
mostly
summer,
South
Asia
subcontinent
contained
boundary
layer
winter,
but
extend
much
which
favors
their
into
southwestern
China.
apparent
seasonality.
Its
top
reaches
level
base
stays
at
similar
height
all
seasons.
thickest
spring.
overlapping
layers
present
different
patterns
regions,
suggests
diverse
mixture
processes
pollutants.
Finally,
compared
found
influences
meteorological
factors,
such
wind
field,
precipitation,
on
sources
other
Atmosphere,
Journal Year:
2023,
Volume and Issue:
14(7), P. 1102 - 1102
Published: June 30, 2023
Profiles
of
aerosols
and
cloud
layers
have
been
investigated
over
a
high-altitude
urban
atmosphere
in
the
eastern
Himalayas
India,
for
first
time,
using
Raman
LIDAR.
The
study
was
conducted
post-monsoon
season
Darjeeling
(latitude
27°01′
N
longitude
88°36′
E,
2200
masl),
tourist
destination
north-eastern
India.
In
addition
to
characterization
atmospheric
boundary
layer
detection,
profile
water
vapor
mixing
ratio
has
also
analyzed.
Effects
dynamics
studied
vertical
profiles
normalized
standard
deviation
RCS
along
with
ratio.
aerosol
optical
characteristics
below
above
Atmospheric
Boundary
Layer
(ABL)
region
were
separately,
interrelation
their
microphysical
properties
synoptic
meteorological
parameters.
backscatter
coefficient
extinction
found
range
from
7.15×10−10
m−1
sr−1
3.01×10−5
1.02×10−5
2.28×10−3
m−1,
respectively.
LIDAR
varies
between
3.9
78.39
sr
all
altitudes.
variation
linear
depolarization
0.19
0.32
indicates
dominance,
non-spherical
particles.
periodicity
observed
different
parameters
may
be
indicative
wave
phenomena.
Cloud
parameters,
such
as
scattering
coefficients,
top
bottom
height,
depth
phases,
evaluated.
A
co-located
Micro
Rain
Radar
used
life
cycle
study.
As
major
natural
disasters
in
grassland
areas,
fires
and
dust
events
seriously
threaten
human
safety,
property,
animal
husbandry.
Furthermore,
these
phenomena
may
be
mutually
reinforcing,
which
can
lead
to
more
severe
cascading
disasters.
However,
few
studies
have
been
on
the
mechanisms
of
fire
disaster
chain.
Therefore,
we
selected
Dornod
aimag
(province),
a
typical
temperate
grassland,
as
study
area
analyzed
spatiotemporal
variation
patterns
weather,
well
effect
weather
based
MCD64A1
Burnt
Area
data
SYNOP
data.
The
mechanism
was
further
investigated
using
MOD13A3
vegetation
index
product
ERA5
wind
speed,
direction,
precipitation
results
revealed
that
varied
spatially
across
area.
occurred
mainly
spring
(April
May),
summer
(June),
autumn
(October),
while
(March
May).
Moreover,
autumn,
winter,
cumulative
(both
days
area)
substantially
affected
total
storm
days,
particularly
days.
Additionally,
higher
2014
resulted
coverage
fuel
winter
2014,
even
2015.
result,
higher,
larger
from
September
April
2015,
leading
considerable
increase
May
This
has
important
implications
for
prevention
mitigation,
ecological
environmental
protection,
sustainable
development
grasslands.
Abstract.
Stratospheric
aerosols
are
long-lived
and
play
a
critical
role
in
the
global
radiation
budget.
Over
past
decade,
contributions
to
stratospheric
from
different
sources
have
changed
due
weaker
volcanic
activity
more
frequent
wildfire
events.
However,
long-term
observations
of
monitoring
major
emission
events
remain
insufficient,
particularly
at
middle
low
latitudes.
In
this
study,
we
analyze
vertical
distribution,
optical
properties,
radiative
forcing
using
ground-based
polarization
lidar
Wuhan
(30.5°
N,
114.4°
E)
2010
2021.
The
aerosol
depth
(sAOD)
generally
stabilized
around
0.0023
without
significant
annual
variation.
Several
cases
wildfire-induced
smoke
were
observed.
Volcanic
Nabro
(2011)
Raikoke
(2019)
eruptions
(both
boreal
summer)
increased
sAOD
4.8
times
background
level
during
stratospheric-quiescent
period
(January
2013
August
2017).
Tracers
Canadian
summer
2017
was
observed
twice:
19–21
km
on
14–17
September
20–23
28–31
October,
with
plume-isolated
AOD
0.002–0.010
particle
linear
depolarization
ratio
δp
0.14–0.18,
indicating
dominance
non-aged
particles.
During
these
summertime
events,
injected
captured
by
large-scale
Asian
monsoon
anticyclone
(AMA),
confining
transport
pathway
mid-latitude
Asia.
On
8–9
November
2020,
plumes
originating
California
October
2020
appeared
16–17
km,
0.007
mean
0.13.
Regarding
seasonal
variation,
cold
half-year
(0.0026)
is
24
%
larger
than
warm
(0.0021)
stronger
meridional
tropics
-0.05
W·m-2
-0.28
when
largely
injected.
These
findings
contribute
our
understanding
patterns
over
Asia
serve
as
important
database
for
validation
model
outputs.