Authorea (Authorea),
Journal Year:
2023,
Volume and Issue:
unknown
Published: Dec. 10, 2023
OI
630.0
nm
post-sunset
emission
enhancement
as
an
effect
of
tidal
activity
over
low-latitudesSovan
Saha1,
Duggirala
Pallamraju1,
Sunil
Kumar1,
Fazlul
I.
Laskar2,
and
Nicholas
M.
Pedatella31
Space
Atmospheric
Sciences
Division,
Physical
Research
Laboratory,
Ahmedabad,
India2Laboratory
for
Physics,
University
Colorado,
Boulder,
CO,
USA3High
Altitude
Observatory,
National
Center
Research,
USACorresponding
author:
Sovan
Saha
([email protected]).
Key
Points:·
low-latitudes
is
consistent
with
the
presence
poleward
meridional
winds.·
WACCM-X
simulated
winds
show
a
wind
reversal
during
hours,
on
occasion.·
Quarter-diurnal
tides
seem
to
play
significant
role
in
reversing
after
sunset.
Abstract:
The
airglow
variability
provides
salient
information
dynamical
changes
taking
place
upper
atmosphere
at
around
250
km.
rates
vary
ambient
electron
densities
neutral
constituents
that
are
associated
these
emissions.
On
several
occasions,
enhancements
emissions
observed
hours
measured
from
Mt.
Abu
(24.6oN,
72.7oE,
19oN
Mag),
low-latitude
location
Indian
longitudes.
These
occur
following
typical
monotonic
decrease
intensity
was
shown
be
cause
such
enhancements.
However,
climatologically,
equatorward
times.
In
this
study,
has
been
investigated
using
variation
by
Whole
Atmosphere
Community
Climate
Model
thermosphere-ionosphere
eXtension
(WACCM-X),
which
also
shows
similar
those
nightglow
emissions,
simultaneous
well.
amplitudes
phases
different
components
obtained
reveal
contribution
quarter-diurnal
hours.
change
proportional
magnitude
reversal.1.
Introduction:The
(redline)
typically
monotonically
sunset
along
incidence
solar
radiation.
intensities
continue
small
throughout
night
again
start
increasing
towards
morning
twilight
time.
one
our
recent
studies,
reported
(Saha
et
al.,
2021)
measurements
longitude
sector.
were
between
20-22
hrs
local
Firstly,
strength
pre-reversal
zonal
electric
field
possible
it
potential
bring
equatorial
off-equatorial
plasma
tropical
latitudes,
Abu.
could
not
satisfactorily
explain
observations
redline
winds,
however,
showed
they
either
or
there
cessation
direction
This
observation
explained
terms
altitudinal
movement
ionosphere
responsible
airglow.
As
contributes
ionospheric
height
2021),
thereby,
greater
reactants
dissociative
recombination
mechanism
Such
nighttime
midnight
called
temperature
maximum
(MTM)
(e.g.,
Mayr
1979;
Herrero
Spencer,
1982;
1983;
Sastri
Rao,
1993;
Colerico
1996;
Fesen,
Mesquita
2018).
Consequently,
brightness
enhanced
events
(Colerico
Mendillo,
2002).The
kinds
Meriwether
1985;
Gurubaran
1995;
Jyoti
2004;
Abdu
2006;
Kumar
2022)
electrodynamics
Pallamraju
Karan
2016;
Pallamraju,
2017;
2022).
atmospheric
waves
have
impact
altitudes
(Vadas,
2007;
Yiğit
Medevdev,
2009;
Miyoshi
2014;
Singh
Mandal
2020;
Optical
radio
techniques
used
characterize
Oliver
1994;
2014,
2019;
2023a).
Several
model
studies
carried
out,
include
lower
forcing
describe
thermospheric
quite
(Roble
Ridley,
Laskar
2013;
Liu
It
known
essential
mesosphere
thermosphere.
processes
Thayaparan,
1997;
Akmaev,
2001;
Chau
Guharay
Franke,
2011;
2018;
Pedatella
Harvey,
2022;
2023b).
generally
generated
can
propagate
thermosphere
where
eventually
dissipate
due
molecular
viscosity
thermal
diffusivity.
thermosphere,
in-situ
influence
semidiurnal
other
higher-order
seen
MTM
2002),
caused
increase
post-midnight
A
simulations
Model,
found
contribute
(Akmaev
Fang
2016).In
work,
we
free-running
version
(WACCM-X)
understand
dynamics
prevalent
low-latitudes.
Electron
km
altitude
(which
peak
nm).
Interestingly,
density
occasionally
sunset,
simulation.
Therefore,
provide
independent
confirmation
interpretation
made
earlier
work
turning
usually
wind,
2021).
question
ask
study
what
its
usual
low-latitudes?2.
Data
used:2.1.
data
(OI
emissions):An
optical
spectrograph,
High
Throughput
Imaging
Echelle
Spectrograph
(HiTIES)
(Chakrabarti
2001),
measure
nocturnal
location,
originate
region
peaking
km,
half-value
width
70
HiTIES
slit
spectra
imaged
onto
1K×1K
CCD
chip.
Image
processing
out
remove
dark
counts,
scattered
lights
arise
starlight,
zodiacal
light,
vignetting
Van-Rhijn
effects.2.2.
simulation:The
community
developed
whole
variabilities
Earth’s
atmosphere-ionosphere-thermosphere
regions
(Liu
captures
chemical,
thermodynamical,
electrodynamical,
ionization,
physical
surface
Earth
500
700
(depending
activity)
altitudes.
simulation
WACCM4/CAM4
physics,
described
Marsh
al.
(2013),
Neale
(2018).
chemistry
middle
Davis
(2023)
well
ionosphere-thermosphere
modifications
capable
providing
parameters
dynamics,
coupled
atmosphere.
analysis
hourly
free-run
WACCM-X,
day-to-day
internally
model,
constant
flux
value
unit
Ap
1
represent
moderate
geomagnetic
quiet
conditions,
pertains.
global
variations
temperatures,
study.
analysed
data.
analyses
results
discussed
below.3.
results:Typically,
ionization
stops,
but
process
ions
electrons
continues
uninterruptedly.
20
22
LT
Figure
period
Jan-Mar
years
2013
2016
thick
blue
line
given
2016.
total
72
nights
(out
185
nights)
depicted
figure.
Note
all
days
geomagnetically
Ap<20
nT.
left-side
y-axis
represents
(in
Rayleighs)
2013,
2015,
whereas,
values
right-side
year
Due
2016,
relatively
expected,
owing
reduced
number
densities.
amount
varies
depending
ranging
few
tens
Rayleigh
200
Rayleigh.
occurrence
time
does
any
dependence
seasons.
npj Climate and Atmospheric Science,
Journal Year:
2024,
Volume and Issue:
7(1)
Published: June 29, 2024
Abstract
Over
the
past
two
decades,
more
frequent
and
intense
climate
events
have
seriously
threatened
operation
of
water
transfer
projects
in
Pacific
Rim
region.
However,
role
climatic
change
driving
runoff
variations
source
areas
these
is
unclear.
We
used
tree-ring
data
to
reconstruct
changes
Hanjiang
River
since
1580
CE
representing
an
important
area
for
China’s
south-north
project.
Comparisons
with
hydroclimatic
reconstructions
southwestern
United
States
central
Chile
indicated
that
region
has
experienced
multiple
coinciding
droughts
related
ENSO
activity.
Climate
simulations
indicate
increased
likelihood
drought
occurrence
coming
decades.
The
combination
warming-induced
stresses
dynamic
El
Niño
(warming
ENSO)
patterns
a
thread
urban
agglomerations
agricultural
regions
rely
on
along
Rim.
Earth System Dynamics,
Journal Year:
2024,
Volume and Issue:
15(2), P. 191 - 213
Published: March 13, 2024
Abstract.
Stratospheric
aerosol
injection
(SAI)
comes
with
a
wide
range
of
possible
design
choices,
such
as
the
location
and
timing
injection.
Different
stratospheric
strategies
can
yield
different
climate
responses;
therefore,
understanding
outcomes
is
crucial
to
making
informed
future
decisions
on
SAI,
along
consideration
other
factors.
Yet,
date,
there
has
been
no
systematic
exploration
broad
SAI
strategies.
This
limits
ability
determine
which
effects
are
robust
across
depend
specific
choices.
study
systematically
explores
how
choice
strategy
affects
responses
in
one
model.
Here,
we
introduce
four
hemispherically
symmetric
strategies,
all
designed
maintain
same
global
mean
surface
temperature:
an
annual
at
Equator
(EQ),
equal
amounts
SO2
15°
N
S
(15N+15S),
30°
(30N+30S),
polar
that
injects
60°
only
during
spring
each
hemisphere
(60N+60S).
We
compare
these
more
complex
quantities
N,
S,
order
not
temperature
but
also
its
large-scale
horizontal
gradients.
All
five
simulated
using
version
2
Community
Earth
System
Model
middle
atmosphere
Whole
Atmosphere
Climate
model,
6,
atmospheric
component,
CESM2(WACCM6-MA),
warming
scenario,
Shared
Socioeconomic
Pathway
(SSP)2-4.5.
find
spatial
distribution
optical
depths,
efficiency,
various
responses.
In
addition,
injecting
subtropics
produces
cooling
per
unit
injection,
EQ
60N+60S
cases
requiring,
respectively,
59
%
50
than
30N+30S
case
meet
target.
Injecting
higher
latitudes
results
larger
Equator-to-pole
While
restore
Arctic
September
sea
ice,
high-latitude
effective
due
SAI-induced
occurring
preferentially
latitudes.
These
suggest
trade-offs
wherein
appear
better
or
worse,
depending
metrics
deemed
important.
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(21), P. 13665 - 13684
Published: Nov. 3, 2023
Abstract.
Despite
offsetting
global
mean
surface
temperature,
various
studies
demonstrated
that
stratospheric
aerosol
injection
(SAI)
could
influence
the
recovery
of
ozone
and
have
important
impacts
on
tropospheric
circulation,
thereby
potentially
playing
an
role
in
modulating
regional
seasonal
climate
variability.
However,
so
far,
most
assessments
such
approach
come
from
model
simulations
which
SO2
is
injected
only
a
single
location
or
set
locations.
Here
we
use
CESM2-WACCM6
SAI
under
comprehensive
strategies
achieving
same
temperature
with
different
locations
and/or
timing
injections,
namely
equatorial
injection,
annual
equal
amounts
at
15∘
N
S,
30∘
polar
strategy
injecting
60∘
S
spring
each
hemisphere.
We
demonstrate
despite
result
contrastingly
magnitudes
aerosol-induced
lower
warming,
moistening,
strengthening
jets
both
hemispheres,
changes
speed
residual
circulation.
These
tend
to
maximise
become
smaller
as
aerosols
are
away
Equator
into
subtropics
higher
latitudes.
In
conjunction
differences
direct
radiative
surface,
these
drive
extratropical
modes
variability
(Northern
Southern
Annular
modes),
including
consequences
northern
winter
climate,
intensity
tropical
Walker
Hadley
circulations,
precipitation
patterns.
Finally,
choice
also
plays
first-order
future
evolution
throughout
globe.
Overall,
our
results
contribute
increased
understanding
fine
interplay
radiative,
dynamical,
chemical
processes
driving
atmospheric
circulation
response
lay
foundation
for
designing
optimal
form
basis
multi-model
intercomparisons.
Earth s Future,
Journal Year:
2023,
Volume and Issue:
11(8)
Published: Aug. 1, 2023
Abstract
The
specifics
of
the
simulated
injection
choices
in
case
stratospheric
aerosol
injections
(SAI)
are
part
crucial
context
necessary
for
meaningfully
discussing
impacts
that
a
deployment
SAI
would
have
on
planet.
One
main
is
desired
amount
cooling
aiming
to
achieve.
Previous
simulations
usually
either
fixed
injection,
resulting
warming
being
offset,
or
specified
one
target
temperature,
so
only
dependent
underlying
trajectory
greenhouse
gases.
Here,
we
use
three
sets
achieving
different
amounts
global
mean
surface
while
following
middle‐of‐the‐road
gas
emission
trajectory:
scenario
maintains
temperatures
at
1.5°C
above
preindustrial
levels
(PI),
and
two
other
scenarios
which
achieve
additional
1.0°C
0.5°C
PI.
We
demonstrate
various
scale
proportionally
with
respect
cooling,
such
as
precipitation
changes,
changes
Atlantic
Meridional
Overturning
Circulation
Walker
Cell.
also
highlight
importance
choice
baseline
period
when
comparing
responses
another
pathway.
This
analysis
leads
policy‐relevant
discussions
around
concept
reference
altogether,
what
constitutes
relevant,
significant,
change
produced
by
SAI.
Nature Communications,
Journal Year:
2024,
Volume and Issue:
15(1)
Published: April 18, 2024
Abstract
Stratospheric
aerosol
injection
is
a
potential
method
of
climate
intervention
to
reduce
risk
as
decarbonization
efforts
continue.
However,
possible
ecosystem
impacts
from
the
strategic
design
hypothetical
scenarios
are
poorly
understood.
Two
recent
Earth
system
model
simulations
depict
policy-relevant
stratospheric
with
similar
global
temperature
targets,
but
10-year
delay
in
deployment.
Here
we
show
this
leads
distinct
ecological
profiles
through
speeds,
which
describe
rate
movement
thermal
conditions.
On
planetary
scale,
speeds
simulation
where
maintains
not
statistically
distinguishable
preindustrial
In
contrast,
rapid
reduction
following
delayed
deployment
produces
over
land
beyond
either
baseline
or
no-intervention
change
present
policy.
The
area
exposed
threshold
places
different
context
their
relative
risks.
Our
results
support
discussion
tradeoffs
and
timescales
future
scenario
decision-making.
Environmental Research Climate,
Journal Year:
2024,
Volume and Issue:
3(3), P. 035011 - 035011
Published: June 4, 2024
Abstract
Climate
change
is
a
prevalent
threat,
and
it
unlikely
that
current
mitigation
efforts
will
be
enough
to
avoid
unwanted
impacts.
One
potential
option
reduce
climate
impacts
the
use
of
stratospheric
aerosol
injection
(SAI).
Even
if
SAI
ultimately
deployed,
might
initiated
only
after
some
temperature
target
exceeded.
The
consequences
such
delay
are
assessed
herein.
This
study
compares
two
cases,
with
same
global
mean
∼1.5°
C
above
preindustrial,
but
start
dates
2035
or
‘delayed’
in
2045.
We
make
simulations
Community
Earth
System
Model
version
2
Whole
Atmosphere
Coupled
Chemistry
6
(CESM2-WACCM6),
using
under
SSP2-4.5
emissions
pathway.
find
delaying
deployment
(relative
temperature)
necessitates
lower
net
radiative
forcing
(−30%)
thus
larger
sulfur
dioxide
rates
(+20%),
even
surface
temperatures
converge,
compensate
for
extra
energy
absorbed
by
system.
Southern
hemisphere
ozone
higher
from
2050
delayed
scenario,
converges
value
later
century.
However,
many
differences
between
2045
appear
small
during
10–25
years
following
start,
although
longer
would
needed
assess
any
longer-term
this
model.
In
addition,
irreversibilities
tipping
points
triggered
period
increased
warming
may
not
adequately
represented
model
could
conclusion
real
world.
Environmental Research Climate,
Journal Year:
2024,
Volume and Issue:
3(3), P. 035012 - 035012
Published: May 29, 2024
Abstract
Stratospheric
aerosol
injection
(SAI)
would
involve
the
addition
of
sulfate
aerosols
in
stratosphere
to
reflect
part
incoming
solar
radiation,
thereby
cooling
climate.
Studies
trying
explore
impacts
SAI
have
often
focused
on
idealized
scenarios
without
explicitly
introducing
what
we
call
‘inconsistencies’
a
deployment.
A
concern
discussed
is
happen
climate
system
after
an
abrupt
termination
its
deployment,
whether
inadvertent
or
deliberate.
However,
there
much
wider
range
plausible
inconsistencies
deployment
than
that
should
be
evaluated
better
understand
associated
risks.
In
this
work,
simulate
few
representative
pre-existing
scenario:
termination,
decade-long
gradual
phase-out,
and
1
year
2
temporary
interruptions
After
examining
their
impacts,
use
these
simulations
train
emulator,
project
global
mean
temperature
response
for
broader
set
Our
work
highlights
capacity
finite
simulated
include
inform
emulator
capable
expanding
space
one
might
want
far
more
quickly
efficiently.
Geophysical Research Letters,
Journal Year:
2024,
Volume and Issue:
51(8)
Published: April 22, 2024
Abstract
Sulfur‐rich
volcanic
eruptions
happen
sporadically.
If
Stratospheric
Aerosol
Injection
(SAI)
were
to
be
deployed,
it
is
likely
that
explosive
would
during
such
a
deployment.
Here
we
use
an
ensemble
of
Earth
System
Model
simulations
show
how
changing
the
injection
strategy
post‐eruption
could
used
reduce
climate
risks
large
eruption;
are
also
modified
even
without
any
change
strategy.
For
medium‐size
eruption
(10
Tg‐SO
2
)
comparable
SAI
rate,
volcanic‐induced
cooling
reduced
if
occurs
under
SAI,
especially
artificial
sulfur
dioxide
injections
immediately
suspended.
Alternatively,
suspending
only
in
hemisphere
and
continuing
opposite
shifts
precipitation
tropical
belt
thus
mitigate
eruption‐induced
drought.
Finally,
for
much
larger
than
deployment,
changes
have
minimal
effect.
Journal of Geophysical Research Atmospheres,
Journal Year:
2025,
Volume and Issue:
130(9)
Published: May 6, 2025
Abstract
Carbonyl
sulfide
(OCS)
is
an
important
atmospheric
sulfur
species
that
plays
a
dominant
role
in
the
formation
of
(nonvolcanic)
stratospheric
sulfate
aerosol
middle
stratosphere.
Major
uncertainties
surface
sources
and
sinks
inconsistent
model
representation
vertical
transport
limit
understanding
OCS
distribution,
particularly
sparsely
sampled
upper
atmosphere.
During
2022
Asian
Summer
Monsoon
Chemical
CLimate
Impact
Project
(ACCLIP)
campaign,
situ
measurements
Upper
Troposphere
Lower
Stratosphere
(UTLS)
at
eastern
edge
summer
monsoon
anticyclone
(ASM),
showed
significant
enhancements
(>750
ppt)
near
tropopause
from
convectively
influenced
air
parcels.
Here,
we
compare
these
novel
UTLS
with
long‐term
satellite
observations
regional
to
broaden
trends
its
by
ASM.
Trajectory
analysis
identifies
northern
China
as
main
source
region
for
deep
convective
lofting
OCS‐enriched
parcels
demonstrates
ASM
entrainment
UTLS,
allowing
evaluation
global
predictions
OCS's
influence.
The
ACCLIP
data
set
provides
vital
validation
limited
vertically
resolved
anthropogenic
emissions,
which
serves
enhance
our
budget.