State of polar climate in 2023
Advances in Climate Change Research,
Год журнала:
2024,
Номер
15(5), С. 769 - 783
Опубликована: Авг. 14, 2024
Язык: Английский
A novel method to detect the tropopause structure based on bi-Gaussian function
Опубликована: Март 26, 2024
Abstract.
The
tropopause
is
important
as
a
diagnostic
of
the
upper
troposphere
and
lower
stratosphere
structures,
with
unique
atmospheric
thermal,
dynamic
structures.
A
comprehensive
understanding
evolution
fine
structures
necessary
primary
to
further
study
complex
multi-scale
physicochemical
coupling
processes
in
stratosphere.
Utilizing
bi-Gaussian
function,
novel
method
capable
identifying
characteristic
parameters
vertical
well
providing
information
double
tropopauses
(DT)
new
improves
definition
cold
point
tropopause,
detects
one
(or
two)
most
significant
local
coldest
point(s)
mathematical
statistics
by
fitting
temperature
profiles
which
(are)
defined
height(s).
function
exhibits
remarkable
potential
for
explicating
variation
trend
profiles.
recognition
results
lapse
rate
World
Meteorological
Organization,
are
compared
detail
different
cases.
Results
indicate
that
possesses
missed
detection
false
than
because
it
not
restricted
thresholds,
even
presence
multiple
inversion
layers
at
higher
elevations.
Five-year
(from
2012
2016)
historical
radiosondes
China
revealed
occurrence
frequency
thickness
DT,
single
height,
first
second
DT
height
displayed
meridional
monotonic
variations.
(thickness)
increased
from
2.93
%
(2.61
km)
72.45
(6.84
latitude
range
[16°
N,
50°
N].
At
mid-latitudes
[30°
40°
N],
gradients
were
relatively
large,
essentially
corresponding
climatological
location
subtropical
jet
Tibetan
Plateau.
average
reported
this
approximately
1–2
km
thicker
previous
studies,
particularly
mid-high
latitudes
[45°
may
be
related
resolution
provided
various
data
sources.
structure
occurs
frequently
has
largest
gradient
mid-latitudes,
formatted
combination
poleward
advection
low-latitude
equatorward
high-latitude
In
addition,
although
thick
winter,
difference
small,
case
happens
occasionally.
Язык: Английский
Comment on egusphere-2024-345
Опубликована: Апрель 11, 2024
The
tropopause
is
important
as
a
diagnostic
of
the
upper
troposphere
and
lower
stratosphere
structures,
with
unique
atmospheric
thermal,
dynamic
structures.
A
comprehensive
understanding
evolution
fine
structures
necessary
primary
to
further
study
complex
multi-scale
physicochemical
coupling
processes
in
stratosphere.
Utilizing
bi-Gaussian
function,
novel
method
capable
identifying
characteristic
parameters
vertical
well
providing
information
double
tropopauses
(DT)
new
improves
definition
cold
point
tropopause,
detects
one
(or
two)
most
significant
local
coldest
point(s)
mathematical
statistics
by
fitting
temperature
profiles
which
(are)
defined
height(s).
function
exhibits
remarkable
potential
for
explicating
variation
trend
profiles.
recognition
results
lapse
rate
World
Meteorological
Organization,
are
compared
detail
different
cases.
Results
indicate
that
possesses
missed
detection
false
than
because
it
not
restricted
thresholds,
even
presence
multiple
inversion
layers
at
higher
elevations.
Five-year
(from
2012
2016)
historical
radiosondes
China
revealed
occurrence
frequency
thickness
DT,
single
height,
first
second
DT
height
displayed
meridional
monotonic
variations.
(thickness)
increased
from
2.93
%
(2.61
km)
72.45
(6.84
latitude
range
[16°
N,
50°
N].
At
mid-latitudes
[30°
40°
N],
gradients
were
relatively
large,
essentially
corresponding
climatological
location
subtropical
jet
Tibetan
Plateau.
average
reported
this
approximately
1–2
km
thicker
previous
studies,
particularly
mid-high
latitudes
[45°
may
be
related
resolution
provided
various
data
sources.
structure
occurs
frequently
has
largest
gradient
mid-latitudes,
formatted
combination
poleward
advection
low-latitude
equatorward
high-latitude
In
addition,
although
thick
winter,
difference
small,
case
happens
occasionally.
Язык: Английский
Comment on egusphere-2024-345
Опубликована: Апрель 17, 2024
The
tropopause
is
important
as
a
diagnostic
of
the
upper
troposphere
and
lower
stratosphere
structures,
with
unique
atmospheric
thermal,
dynamic
structures.
A
comprehensive
understanding
evolution
fine
structures
necessary
primary
to
further
study
complex
multi-scale
physicochemical
coupling
processes
in
stratosphere.
Utilizing
bi-Gaussian
function,
novel
method
capable
identifying
characteristic
parameters
vertical
well
providing
information
double
tropopauses
(DT)
new
improves
definition
cold
point
tropopause,
detects
one
(or
two)
most
significant
local
coldest
point(s)
mathematical
statistics
by
fitting
temperature
profiles
which
(are)
defined
height(s).
function
exhibits
remarkable
potential
for
explicating
variation
trend
profiles.
recognition
results
lapse
rate
World
Meteorological
Organization,
are
compared
detail
different
cases.
Results
indicate
that
possesses
missed
detection
false
than
because
it
not
restricted
thresholds,
even
presence
multiple
inversion
layers
at
higher
elevations.
Five-year
(from
2012
2016)
historical
radiosondes
China
revealed
occurrence
frequency
thickness
DT,
single
height,
first
second
DT
height
displayed
meridional
monotonic
variations.
(thickness)
increased
from
2.93
%
(2.61
km)
72.45
(6.84
latitude
range
[16°
N,
50°
N].
At
mid-latitudes
[30°
40°
N],
gradients
were
relatively
large,
essentially
corresponding
climatological
location
subtropical
jet
Tibetan
Plateau.
average
reported
this
approximately
1–2
km
thicker
previous
studies,
particularly
mid-high
latitudes
[45°
may
be
related
resolution
provided
various
data
sources.
structure
occurs
frequently
has
largest
gradient
mid-latitudes,
formatted
combination
poleward
advection
low-latitude
equatorward
high-latitude
In
addition,
although
thick
winter,
difference
small,
case
happens
occasionally.
Язык: Английский
Comment on egusphere-2024-345
Опубликована: Апрель 30, 2024
The
tropopause
is
important
as
a
diagnostic
of
the
upper
troposphere
and
lower
stratosphere
structures,
with
unique
atmospheric
thermal,
dynamic
structures.
A
comprehensive
understanding
evolution
fine
structures
necessary
primary
to
further
study
complex
multi-scale
physicochemical
coupling
processes
in
stratosphere.
Utilizing
bi-Gaussian
function,
novel
method
capable
identifying
characteristic
parameters
vertical
well
providing
information
double
tropopauses
(DT)
new
improves
definition
cold
point
tropopause,
detects
one
(or
two)
most
significant
local
coldest
point(s)
mathematical
statistics
by
fitting
temperature
profiles
which
(are)
defined
height(s).
function
exhibits
remarkable
potential
for
explicating
variation
trend
profiles.
recognition
results
lapse
rate
World
Meteorological
Organization,
are
compared
detail
different
cases.
Results
indicate
that
possesses
missed
detection
false
than
because
it
not
restricted
thresholds,
even
presence
multiple
inversion
layers
at
higher
elevations.
Five-year
(from
2012
2016)
historical
radiosondes
China
revealed
occurrence
frequency
thickness
DT,
single
height,
first
second
DT
height
displayed
meridional
monotonic
variations.
(thickness)
increased
from
2.93
%
(2.61
km)
72.45
(6.84
latitude
range
[16°
N,
50°
N].
At
mid-latitudes
[30°
40°
N],
gradients
were
relatively
large,
essentially
corresponding
climatological
location
subtropical
jet
Tibetan
Plateau.
average
reported
this
approximately
1–2
km
thicker
previous
studies,
particularly
mid-high
latitudes
[45°
may
be
related
resolution
provided
various
data
sources.
structure
occurs
frequently
has
largest
gradient
mid-latitudes,
formatted
combination
poleward
advection
low-latitude
equatorward
high-latitude
In
addition,
although
thick
winter,
difference
small,
case
happens
occasionally.
Язык: Английский
Reply on RC2
Опубликована: Июнь 19, 2024
The
tropopause
is
important
as
a
diagnostic
of
the
upper
troposphere
and
lower
stratosphere
structures,
with
unique
atmospheric
thermal,
dynamic
structures.
A
comprehensive
understanding
evolution
fine
structures
necessary
primary
to
further
study
complex
multi-scale
physicochemical
coupling
processes
in
stratosphere.
Utilizing
bi-Gaussian
function,
novel
method
capable
identifying
characteristic
parameters
vertical
well
providing
information
double
tropopauses
(DT)
new
improves
definition
cold
point
tropopause,
detects
one
(or
two)
most
significant
local
coldest
point(s)
mathematical
statistics
by
fitting
temperature
profiles
which
(are)
defined
height(s).
function
exhibits
remarkable
potential
for
explicating
variation
trend
profiles.
recognition
results
lapse
rate
World
Meteorological
Organization,
are
compared
detail
different
cases.
Results
indicate
that
possesses
missed
detection
false
than
because
it
not
restricted
thresholds,
even
presence
multiple
inversion
layers
at
higher
elevations.
Five-year
(from
2012
2016)
historical
radiosondes
China
revealed
occurrence
frequency
thickness
DT,
single
height,
first
second
DT
height
displayed
meridional
monotonic
variations.
(thickness)
increased
from
2.93
%
(2.61
km)
72.45
(6.84
latitude
range
[16°
N,
50°
N].
At
mid-latitudes
[30°
40°
N],
gradients
were
relatively
large,
essentially
corresponding
climatological
location
subtropical
jet
Tibetan
Plateau.
average
reported
this
approximately
1–2
km
thicker
previous
studies,
particularly
mid-high
latitudes
[45°
may
be
related
resolution
provided
various
data
sources.
structure
occurs
frequently
has
largest
gradient
mid-latitudes,
formatted
combination
poleward
advection
low-latitude
equatorward
high-latitude
In
addition,
although
thick
winter,
difference
small,
case
happens
occasionally.
Язык: Английский
Reply on RC1
Опубликована: Июнь 19, 2024
The
tropopause
is
important
as
a
diagnostic
of
the
upper
troposphere
and
lower
stratosphere
structures,
with
unique
atmospheric
thermal,
dynamic
structures.
A
comprehensive
understanding
evolution
fine
structures
necessary
primary
to
further
study
complex
multi-scale
physicochemical
coupling
processes
in
stratosphere.
Utilizing
bi-Gaussian
function,
novel
method
capable
identifying
characteristic
parameters
vertical
well
providing
information
double
tropopauses
(DT)
new
improves
definition
cold
point
tropopause,
detects
one
(or
two)
most
significant
local
coldest
point(s)
mathematical
statistics
by
fitting
temperature
profiles
which
(are)
defined
height(s).
function
exhibits
remarkable
potential
for
explicating
variation
trend
profiles.
recognition
results
lapse
rate
World
Meteorological
Organization,
are
compared
detail
different
cases.
Results
indicate
that
possesses
missed
detection
false
than
because
it
not
restricted
thresholds,
even
presence
multiple
inversion
layers
at
higher
elevations.
Five-year
(from
2012
2016)
historical
radiosondes
China
revealed
occurrence
frequency
thickness
DT,
single
height,
first
second
DT
height
displayed
meridional
monotonic
variations.
(thickness)
increased
from
2.93
%
(2.61
km)
72.45
(6.84
latitude
range
[16°
N,
50°
N].
At
mid-latitudes
[30°
40°
N],
gradients
were
relatively
large,
essentially
corresponding
climatological
location
subtropical
jet
Tibetan
Plateau.
average
reported
this
approximately
1–2
km
thicker
previous
studies,
particularly
mid-high
latitudes
[45°
may
be
related
resolution
provided
various
data
sources.
structure
occurs
frequently
has
largest
gradient
mid-latitudes,
formatted
combination
poleward
advection
low-latitude
equatorward
high-latitude
In
addition,
although
thick
winter,
difference
small,
case
happens
occasionally.
Язык: Английский
Reply on RC3
Опубликована: Июнь 19, 2024
The
tropopause
is
important
as
a
diagnostic
of
the
upper
troposphere
and
lower
stratosphere
structures,
with
unique
atmospheric
thermal,
dynamic
structures.
A
comprehensive
understanding
evolution
fine
structures
necessary
primary
to
further
study
complex
multi-scale
physicochemical
coupling
processes
in
stratosphere.
Utilizing
bi-Gaussian
function,
novel
method
capable
identifying
characteristic
parameters
vertical
well
providing
information
double
tropopauses
(DT)
new
improves
definition
cold
point
tropopause,
detects
one
(or
two)
most
significant
local
coldest
point(s)
mathematical
statistics
by
fitting
temperature
profiles
which
(are)
defined
height(s).
function
exhibits
remarkable
potential
for
explicating
variation
trend
profiles.
recognition
results
lapse
rate
World
Meteorological
Organization,
are
compared
detail
different
cases.
Results
indicate
that
possesses
missed
detection
false
than
because
it
not
restricted
thresholds,
even
presence
multiple
inversion
layers
at
higher
elevations.
Five-year
(from
2012
2016)
historical
radiosondes
China
revealed
occurrence
frequency
thickness
DT,
single
height,
first
second
DT
height
displayed
meridional
monotonic
variations.
(thickness)
increased
from
2.93
%
(2.61
km)
72.45
(6.84
latitude
range
[16°
N,
50°
N].
At
mid-latitudes
[30°
40°
N],
gradients
were
relatively
large,
essentially
corresponding
climatological
location
subtropical
jet
Tibetan
Plateau.
average
reported
this
approximately
1–2
km
thicker
previous
studies,
particularly
mid-high
latitudes
[45°
may
be
related
resolution
provided
various
data
sources.
structure
occurs
frequently
has
largest
gradient
mid-latitudes,
formatted
combination
poleward
advection
low-latitude
equatorward
high-latitude
In
addition,
although
thick
winter,
difference
small,
case
happens
occasionally.
Язык: Английский