Abstract.
Polarization
properties
of
the
fluorescence
induced
by
polarized
laser
radiation
are
widely
considered
in
laboratory
studies.
In
lidar
observations,
however,
only
total
scattered
power
is
analyzed.
this
paper
we
present
results
obtained
with
a
modified
Mie-Raman-Fluorescence
operated
at
ATOLL
observatory,
Laboratoire
d’Optique
Atmosphérique,
University
Lille,
France,
allowing
to
measure
depolarization
ratios
466
nm
(δF)
and
water
vapor
Raman
backscatter.
Measurements
were
performed
May–June
2023
during
Alberta
forest
fires
season
when
smoke
plumes
almost
continuously
transported
over
Atlantic
Ocean
towards
Europe.
During
same
period,
from
sources
also
detected
analyzed
Moscow,
General
Physics
Institute
(GPI),
5-channel
able
backscattering
438,
472,
513,
560
614
nm.
Results
demonstrate
that,
inside
boundary
layer
(BL),
urban
aerosol
maximal
438
nm,
then
it
gradually
decreases
wavelength.
show
that
maximum
spectrum
shifted
longer
wavelengths.
The
layers
observed
within
4–6
km
513
while,
upper
troposphere
(UT),
shifts
Regarding
depolarization,
its
value
typically
varies
45–55
%
range,
however
several
plume
above
10
characterized
δF
increasing
up
70
%.
Inside
BL,
ratio
was
higher
than
varied
50–70
range.
Moreover,
appears
vary
atmospheric
relative
humidity
(RH)
and,
contrast
elastic
scattering,
increases
RH.
shown
be
quite
low
(2±0.5
%)
absence
fluorescence,
because
narrowband
interference
filter
channel
selects
strongest
vibrational
lines
spectrum.
As
result,
sensitive
presence
strongly
depolarized
backscattering.
contamination
into
can
calculated
assumption
remains
constant
408–466
Atmospheric measurement techniques,
Journal Year:
2023,
Volume and Issue:
16(8), P. 2055 - 2065
Published: April 18, 2023
Abstract.
A
five-channel
fluorescence
lidar
was
developed
for
the
study
of
atmospheric
aerosol.
The
spectrum
induced
by
355
nm
laser
emission
is
analyzed
in
five
spectral
intervals
using
interference
filters.
Central
wavelengths
and
widths
these
filters
are,
respectively,
as
follows:
438
29,
472
32,
513
560
40,
614
54
nm.
relative
calibration
channels
has
been
performed
a
tungsten–halogen
lamp
with
color
temperature
2800
K.
This
new
system
operated
during
summer–autumn
2022,
when
strong
forest
fires
occurred
Moscow
region
generated
series
smoke
plumes
this
study.
Our
results
demonstrate
that,
urban
aerosol,
maximal
backscattering
observed
channel.
For
smoke,
maximum
shifted
toward
longer
wavelengths,
coefficients
472,
have
comparable
values.
Thus,
from
analysis
ratios
available
channels,
we
show
that
it
possible
to
identify
layers.
particle
classification
based
on
single-channel
capacity
(ratio
elastic
one)
limitations
at
high
humidity
(RH).
indeed
decreases
water
uptake
particles
enhances
scattering.
However,
variation
does
not
exhibit
any
dependence
RH
can
be
therefore
applied
aerosol
identification.
Optics Express,
Journal Year:
2023,
Volume and Issue:
31(13), P. 22157 - 22157
Published: May 30, 2023
Bioaerosols
play
a
significant
role
in
climate
change
and
variation
of
ecological
environment.
To
investigate
characterization
atmospheric
bioaerosols,
we
conducted
lidar
measurement
for
observing
bioaerosols
close
to
dust
sources
over
northwest
China
April,
2014.
The
developed
system
can
not
only
allowed
us
measure
the
32-channel
fluorescent
spectrum
between
343
nm
526
with
spectral
resolution
5.8
but
also
simultaneously
detect
polarisation
measurements
at
355
532
nm,
as
well
Raman
scattering
signals
387
407
nm.
According
findings,
was
able
pick
up
robust
fluorescence
signal
emitted
by
aerosols.
Especially
polluted
dust,
efficiency
could
reach
0.17.
In
addition,
single-band
typically
rises
wavelength
goes
ratio
air
pollutant
background
aerosols
is
about
4:3:8:2.
Moreover,
our
results
demonstrate
that
simultaneous
depolarization
better
distinguish
than
those
This
study
enhances
ability
laser
remote
sensing
real-time
detecting
bioaerosol
atmosphere.
Atmospheric chemistry and physics,
Journal Year:
2025,
Volume and Issue:
25(3), P. 1603 - 1615
Published: Feb. 5, 2025
Abstract.
The
fluorescence
lidar
at
the
Prokhorov
General
Physics
Institute
(Moscow)
was
utilized
to
study
smoke
transported
over
Atlantic
during
wildfire
season
from
May
September
2023.
system,
which
is
based
on
a
tripled
Nd
:
YAG
laser,
performs
measurements
across
five
spectral
intervals
centered
wavelengths
of
438,
472,
513,
560
and
614
nm.
This
configuration
enables
assessment
dependence
backscattering
broad
range
altitudes,
planetary
boundary
layer
(PBL)
middle
upper
troposphere
(MUT).
capacity
smoke,
defined
as
ratio
aerosol
laser
wavelength,
exhibits
significant
variation
in
MUT,
with
changes
up
factor
3.
likely
indicative
differences
relative
concentration
organic
compounds
within
smoke.
Analysis
more
than
40
episodes
has
enabled
an
evaluation
height
properties.
Observations
reveal
that
generally
increases
altitude,
suggesting
higher
MUT
compared
lower
troposphere.
Additionally,
consistently
show
spectra
urban
aerosol.
Urban
tends
decrease
gradually
whereas
peak
observed
513
nm
channels.
distinction
provides
effective
means
separating
technique
applied
analysis
events
where
descended
into
PBL,
demonstrating
its
utility
distinguishing
between
these
types.
Atmospheric chemistry and physics,
Journal Year:
2025,
Volume and Issue:
25(7), P. 3995 - 4011
Published: April 9, 2025
Abstract.
One
of
the
most
powerful
instruments
for
studying
aerosol
particles
and
their
interactions
with
environment
is
atmospheric
lidar.
In
recent
years,
fluorescence
lidar
has
emerged
as
a
useful
tool
identifying
due
to
its
link
biological
content.
Since
2022,
this
technique
been
implemented
in
Leipzig,
Germany.
This
paper
describes
experimental
setup
data
analysis,
special
emphasis
on
characterization
new
channel
centered
at
466
nm.
The
capabilities
are
examined
corroborated
through
several
case
studies.
Most
measurement
cases
considered
from
spring
summer
2023,
when
large
amounts
biomass-burning
huge
forest
fires
Canada
were
transported
Europe.
observed
layers
characterized.
For
wildfire
smoke,
capacity
was
typically
range
2×10-4–7
×
10−4,
which
aligns
well
values
reported
literature.
key
aspects
study
technique,
can
potentially
improve
not
only
typing
but
even
detection
particles.
an
apparently
low
load,
clearly
revealed
presence
that
detectable
traditional
elastic-backscatter
channels.
capability
discussed
detail
linked
fact
backscattering
related
only.
A
second
area
potential
distinction
between
non-activated
hydrometeors,
given
water's
inability
exhibit
fluorescence.
smoke–cirrus
suggests
influence
layer
cloud
formation,
it
seems
affect
coefficient
within
passing
time.
These
aforementioned
applications
promise
advancements
towards
more
detailed
view
aerosol–cloud
interaction
problem.
Atmospheric measurement techniques,
Journal Year:
2024,
Volume and Issue:
17(3), P. 1023 - 1036
Published: Feb. 12, 2024
Abstract.
Polarization
properties
of
the
fluorescence
induced
by
polarized
laser
radiation
are
widely
considered
in
laboratory
studies.
In
lidar
observations,
however,
only
total
backscattered
power
is
analyzed.
this
paper
we
present
results
obtained
with
a
modified
Mie–Raman–fluorescence
operated
at
ATOLL
observatory,
Laboratoire
d'Optique
Atmosphérique,
University
Lille,
France,
allowing
us
to
measure
depolarization
ratios
466
nm
(δF)
and
water
vapor
Raman
backscatter.
Measurements
were
performed
May–June
2023
during
Alberta
forest
fires
season
when
smoke
plumes
almost
continuously
transported
over
Atlantic
Ocean
towards
Europe.
During
same
period,
from
sources
also
detected
analyzed
Moscow,
General
Physics
Institute
(GPI),
five-channel
able
backscattering
438,
472,
513,
560
614
nm.
Results
demonstrate
that,
inside
planetary
boundary
layer
(PBL),
urban
aerosol
maximal
438
nm,
then
it
gradually
decreases
increase
wavelength.
The
layers
observed
within
4–6
km
height
maximum
513
while
upper
troposphere,
shifts
Regarding
ratio,
for
its
value
typically
varies
45
%–55
%
range.
ratio
408
shown
be
quite
low
(2±0.5
%)
absence
because
narrowband
interference
filter
(0.3
nm)
channel
selects
strongest
vibrational
lines
spectrum.
As
result,
sensitive
presence
strongly
depolarized
can
used
evaluation
contribution
measured
mixing
ratio.
Atmospheric measurement techniques,
Journal Year:
2024,
Volume and Issue:
17(12), P. 3625 - 3667
Published: June 18, 2024
Abstract.
A
new
four-dimensional,
multiyear,
and
near-global
climate
data
record
of
the
fine-mode
(submicrometer
in
terms
diameter)
coarse-mode
(supermicrometer
components
atmospheric
pure
dust
is
presented.
The
separation
two
modes
detected
layers
based
on
a
combination
(1)
total
pure-dust
product
provided
by
well-established
European
Space
Agency
(ESA)
“LIdar
climatology
Vertical
Aerosol
Structure”
(LIVAS)
database
(2)
component
first
step
two-step
POlarization
LIdar
PHOtometer
Networking
(POLIPHON)
technique,
developed
framework
Research
Lidar
Network
(EARLINET).
Accordingly,
extracted
as
residual
between
LIVAS
dust.
Intermediate
steps
involve
implementation
regionally
dependent
lidar-derived
lidar
ratio
values
AErosol
RObotic
NETwork
(AERONET)-based
climatological
extinction-to-volume
conversion
factors,
facilitating
backscatter
into
extinction
subsequently
mass
concentration.
decoupling
scheme
applied
to
observations
from
Cloud–Aerosol
Infrared
Pathfinder
Satellite
Observations
(CALIPSO)
at
532
nm.
final
products
consist
fine
mode
coarse
dust,
quality-assured
profiles
coefficient
nm,
concentration
for
each
components.
datasets
are
established
primarily
with
original
L2
horizontal
(5
km)
vertical
(60
m)
resolution
Orthogonal
Polarization
(CALIOP)
along
CALIPSO
orbit
path
secondly
averaged
seasonal–temporal
resolution,
1°
×
spatial
CALIPSO,
focusing
latitudinal
band
extending
70°
S
N
covering
more
than
15
years
Earth
(June
2006–December
2021).
quality
CALIPSO-based
assessed
through
use
AERONET
aerosol
optical
thickness
(AOT)
interpolated
nm
AERosol
properties
–
Dust
(AER-D)
campaign
airborne
situ
particle
size
distributions
(PSDs)
reference
during
conditions
characterized
presence.
considered
unique
respect
wide
range
potential
applications,
including
climatological,
time
series,
trend
analysis
over
extensive
geographical
domains
temporal
periods,
validation
models
reanalysis
datasets,
assimilation
activities,
investigation
role
radiation
air
quality.
Atmospheric Environment X,
Journal Year:
2024,
Volume and Issue:
22, P. 100248 - 100248
Published: March 6, 2024
Bioaerosols
are
biologically
originated
particles
in
the
atmosphere,
which
is
mainly
composed
of
bacteria,
fungi,
viruses,
pollen,
spores,
and
fragmentation
disintegration
plants
animals.
easy
to
be
spread
lower
atmosphere
cause
various
epidemic
diseases,
harmful
human
health.
The
forecasting
alert
bioaerosols
have
important
scientific
significance
reality
needs.
In
this
paper,
a
method
proposed
for
estimating
predicting
concentration
profile
atmospheric
using
fluorescence
lidar
observational
data.
Using
powerful
nonlinear
prediction
ability
artificial
neural
networks
through
repeated
training,
mathematical
model
can
established
relationship
among
environment,
meteorological
parameters,
bioaerosol
profiles.
input
parameters
temperature
humidity,
aerosol
extinction
coefficient,
backscatter
PM2.5,
PM10,
SO2,
NO2,
CO,
O3,
wind
speed,
outputs
bioaerosols.
results
with
measurement
relative
deviation
genetic
algorithm
back
propagation
(GA-BP)
network
adaptive
(AGA-BP)
were
analyzed.
indicate
that
AGA-BP
effectively
predict
distribution
bioaerosols,
predicted
concentrations
1793
×
m−3,
3088
5261
7410
m−3
9133
air
quality
superior,
fine,
mild
contamination,
middle
level
pollution
heavy
at
an
altitude
0.315
km,
respectively.
We
found
weather
much
higher
than
good
weather.
Furthermore,
was
used
profiles
under
different
conditions,
provided
new
research
Atmospheric measurement techniques,
Journal Year:
2024,
Volume and Issue:
17(11), P. 3367 - 3375
Published: June 3, 2024
Abstract.
This
study
focuses
on
the
characterization
of
aerosol
hygroscopicity
using
remote
sensing
techniques.
We
employ
a
Mie–Raman–fluorescence
lidar
(Lille
Lidar
for
Atmospheric
Study,
LILAS),
developed
at
ATOLL
platform,
Laboratoire
d'Optique
Atmosphérique,
Lille,
France,
in
combination
with
RPG-HATPRO-G5
microwave
radiometer
to
enable
continuous
and
water
vapor
monitoring.
identify
hygroscopic
growth
cases
when
an
layer
exhibits
increase
both
backscattering
coefficient
relative
humidity.
By
examining
fluorescence
coefficient,
which
remains
unaffected
by
presence
vapor,
potential
temperature,
absolute
humidity,
we
verify
homogeneity
layer.
Consequently,
change
is
solely
attributed
uptake.
The
Hänel
theory
employed
describe
evolution
humidity
introduces
γ,
depends
type.
particularity
this
method
revolves
around
use
take
into
account
correct
concentration
variations
Case
studies
conducted
29
July
9
March
2021
examine,
respectively,
urban
smoke
For
case,
γ
estimated
as
0.47
±
0.03
532
nm;
estimation
0.5
0.3.
These
values
align
those
reported
literature
particles.
Our
findings
highlight
efficiency
synergy
characterizing
hygroscopicity.
results
contribute
advance
our
understanding
atmospheric
processes,
aerosol–cloud
interactions,
climate
modeling.
Atmospheric measurement techniques,
Journal Year:
2024,
Volume and Issue:
17(13), P. 4137 - 4152
Published: July 15, 2024
Abstract.
In
the
atmosphere,
aerosols
can
originate
from
numerous
sources,
leading
to
mixing
of
different
particle
types.
This
paper
introduces
an
approach
partitioning
aerosol
mixtures
in
terms
backscattering
coefficients.
The
method
utilizes
data
collected
Mie–Raman–fluorescence
lidar,
with
primary
input
information
being
coefficient
(β),
depolarization
ratio
(δ),
and
fluorescence
capacity
(GF).
is
defined
as
at
laser
wavelength.
By
solving
a
system
equations
that
model
these
three
properties
(β,
δ
GF),
it
possible
characterize
three-component
mixture.
Specifically,
assesses
contributions
smoke,
urban,
dust
overall
532
nm.
It
important
note
(δ
GF)
may
exhibit
variations
even
within
specified
type.
To
estimate
associated
uncertainty,
we
employ
Monte
Carlo
technique,
which
assumes
GF
are
random
values
uniformly
distributed
predefined
intervals.
each
run,
solution
obtained.
Rather
than
relying
on
singular
solution,
average
computed
across
whole
set
solutions,
their
dispersion
serves
metric
for
uncertainty.
methodology
was
tested
using
observations
conducted
ATOLL
(ATmospheric
Observation
liLLe)
observatory,
Laboratoire
d'Optique
Atmosphérique,
University
Lille,
France.