arXiv (Cornell University),
Journal Year:
2023,
Volume and Issue:
unknown
Published: Jan. 1, 2023
In
this
study
we
perform
online
sea
ice
bias
correction
within
a
GFDL
global
ice-ocean
model.
For
this,
use
convolutional
neural
network
(CNN)
which
was
developed
in
previous
(Gregory
et
al.,
2023)
for
the
purpose
of
predicting
concentration
(SIC)
data
assimilation
(DA)
increments.
An
initial
implementation
CNN
shows
systematic
improvements
SIC
biases
relative
to
free-running
model,
however
large
summertime
errors
remain.
We
show
that
these
residual
can
be
significantly
improved
with
augmentation
approach,
sequential
and
DA
corrections
are
applied
new
simulation
over
training
period.
This
then
provides
set
refine
weights
network.
propose
machine-learned
scheme
could
utilized
generating
conditions,
also
real-time
seasonal-to-subseasonal
forecasts.
Abstract.
We
review
how
the
international
modelling
community,
encompassing
Integrated
Assessment
models,
global
and
regional
Earth
system
climate
impact
have
worked
together
over
past
few
decades,
to
advance
understanding
of
change
its
impacts
on
society
environment,
support
policy.
then
recommend
a
number
priority
research
areas
for
coming
~6
years
(i.e.
until
~2030),
timescale
that
matches
newly
starting
activities
encompasses
IPCC
7th
Report
(AR7)
2nd
UNFCCC
Global
Stocktake.
Progress
in
these
will
significantly
our
increase
quality
utility
science
emphasize
need
continued
improvement
of,
ability
simulate,
coupled
change.
There
is
an
urgent
investigate
plausible
pathways
emission
scenarios
realize
Paris
Climate
Targets,
including
overshoot
1.5
°C
2
targets,
before
later
returning
them.
System
models
(ESMs)
be
capable
thoroughly
assessing
such
warming
overshoots,
particular,
efficacy
negative
CO2
actions
reducing
atmospheric
driving
cooling.
An
improved
assessment
long-term
consequences
stabilizing
at
or
above
pre-industrial
temperatures
also
required.
ESMs
run
CO2-emission
mode,
more
fully
represent
-
carbon
cycle
feedbacks.
Regional
downscaling
should
use
forcing
data
from
simulations,
so
projections
are
as
realistic
possible.
accurate
simulation
observed
record
remains
key
requirement
does
metrics,
Effective
Sensitivity.
For
adaptation,
guidance
potential
changes
extremes
modes
variability
develop
in,
demand.
Such
improvements
most
likely
realized
through
combination
increased
model
resolution
parameterizations.
propose
deeper
collaboration
across
efforts
targeting
process
realism
coupling,
enhanced
resolution,
parameterization
improvement,
data-driven
Machine
Learning
methods.
With
respect
sampling
future
uncertainty,
between
approaches
large
ensembles
those
focussed
statistical
emulation
attention
paid
High
Impact
Low
Likelihood
(HILL)
outcomes.
In
risk
exceeding
critical
tipping
points
during
overshoot.
comprehensive
change,
arising
directly
specific
mitigation
actions,
it
important
detailed,
disaggregated
information
Models
(IAMs)
used
generate
available
models.
Conversely,
methods
developed
incorporate
societal
responses
into
scenario
development.
Finally,
new
data,
scientific
advances,
proposed
this
article
not
possible
without
development
maintenance
robust,
globally
connected
infrastructure
ecosystem.
This
must
easily
accessible
useable
all
communities
world,
allowing
community
engaged
developing
delivering
knowledge
Authorea (Authorea),
Journal Year:
2024,
Volume and Issue:
unknown
Published: June 24, 2024
Due
to
their
limited
resolution,
numerical
ocean
models
need
be
interpreted
as
representing
filtered
or
averaged
equations.
How
interpret
in
terms
of
formally
equations,
however,
is
not
always
clear,
particularly
the
case
hybrid
generalized
vertical
coordinate
models.
We
derive
hydrostatic
Boussinesq
equations
coordinates
for
an
arbitrary
thickness
weighted-average.
then
consider
various
special
cases
and
discuss
extent
which
are
consistent
with
existing
model
formulations.
As
previously
discussed,
momentum
depth-coordinate
best
Eulerian
averages
(i.e.,
taken
at
fixed
depth),
while
tracer
can
either
thickness-weighted
isopycnal
averages.
Instead
we
find
that
no
averaging
fully
formulations
parameterizations
semi-Lagrangian
discretizations
Perhaps
most
natural
interpretation
assume
average
follows
model’s
surfaces.
However,
generally
coordinate-following
averages,
would
require
“coordinate-aware”
account
changing
nature
eddy
changes.
Alternatively,
variables
(thickness-weighted)
independent
being
used
discretization.
Existing
models,
usually
these
interpretations.
what
changes
needed
achieve
consistency.
Journal of Advances in Modeling Earth Systems,
Journal Year:
2024,
Volume and Issue:
16(10)
Published: Oct. 1, 2024
Abstract
Ocean
mesoscale
eddies
are
often
poorly
represented
in
climate
models,
and
therefore,
their
effects
on
the
large
scale
circulation
must
be
parameterized.
Traditional
parameterizations,
which
represent
bulk
effect
of
unresolved
eddies,
can
improved
with
new
subgrid
models
learned
directly
from
data.
Zanna
Bolton
(2020),
https://doi.org/10.1029/2020gl088376
(ZB20)
applied
an
equation‐discovery
algorithm
to
reveal
interpretable
expression
parameterizing
momentum
fluxes
by
through
components
velocity‐gradient
tensor.
In
this
work,
we
implement
ZB20
parameterization
into
primitive‐equation
GFDL
MOM6
ocean
model
test
it
two
idealized
configurations
significantly
different
dynamical
regimes
topography.
The
original
was
found
generate
excessive
numerical
noise
near
grid
scale.
We
propose
filtering
approaches
avoid
issues
additionally
enhance
strength
large‐scale
energy
backscatter.
filtered
parameterizations
led
climatological
mean
state
distributions,
compared
current
state‐of‐the‐art
backscatter
parameterizations.
scale‐aware
and,
consequently,
used
a
single
value
non‐dimensional
scaling
coefficient
for
range
resolutions.
successful
application
parameterize
offers
promising
opportunity
reduce
long‐standing
biases
global
simulations
future
studies.
Journal of Advances in Modeling Earth Systems,
Journal Year:
2024,
Volume and Issue:
16(12)
Published: Dec. 1, 2024
Abstract
Due
to
their
limited
resolution,
numerical
ocean
models
need
be
interpreted
as
representing
filtered
or
averaged
equations.
How
interpret
in
terms
of
formally
equations,
however,
is
not
always
clear,
particularly
the
case
hybrid
generalized
vertical
coordinate
models,
which
limits
our
ability
model
results
and
develop
parameterizations
for
unresolved
eddy
contributions.
We
here
derive
hydrostatic
Boussinesq
equations
coordinates
an
arbitrary
thickness‐weighted
average.
then
consider
various
special
cases
discuss
extent
are
consistent
with
existing
formulations.
As
previously
discussed,
momentum
depth‐coordinate
best
Eulerian
averages
(i.e.,
taken
at
fixed
depth),
while
tracer
can
either
isopycnal
averages.
Instead
we
find
that
no
averaging
fully
formulations
semi‐Lagrangian
discretizations
such
MOM6.
A
coordinate‐following
average
would
require
“coordinate‐aware”
account
changing
nature
changes.
Alternatively,
variables
(thickness‐weighted)
averages,
independent
being
used
discretization.
Existing
these
interpretations,
which,
respectively,
a
three‐dimensional
divergence‐free
advection
form‐stress
parameterization
arXiv (Cornell University),
Journal Year:
2023,
Volume and Issue:
unknown
Published: Jan. 1, 2023
In
this
study
we
perform
online
sea
ice
bias
correction
within
a
GFDL
global
ice-ocean
model.
For
this,
use
convolutional
neural
network
(CNN)
which
was
developed
in
previous
(Gregory
et
al.,
2023)
for
the
purpose
of
predicting
concentration
(SIC)
data
assimilation
(DA)
increments.
An
initial
implementation
CNN
shows
systematic
improvements
SIC
biases
relative
to
free-running
model,
however
large
summertime
errors
remain.
We
show
that
these
residual
can
be
significantly
improved
with
augmentation
approach,
sequential
and
DA
corrections
are
applied
new
simulation
over
training
period.
This
then
provides
set
refine
weights
network.
propose
machine-learned
scheme
could
utilized
generating
conditions,
also
real-time
seasonal-to-subseasonal
forecasts.