TEOS-10 Equations for the Lifted Condensation Level (LCL) and Climatic Feedback of Marine Clouds
Published: March 20, 2024
At
an
energy
flux
imbalance
of
about
1
W
m–2,
the
ocean
is
storing
90
%
heat
accumulating
by
global
warming.
However,
neither
causes
nor
responsible
geophysical
processes
are
sufficiently
well
understood.
More
detailed
investigations
different
phenomena
contributing
to
oceanic
balance
warranted.
Here,
role
low-level
marine
clouds
in
air-sea
interaction
analysed.
TEOS-10,
International
Thermodynamic
Equation
State
Seawater
–
2010,
exploited
for
a
rigorous
thermodynamic
description
climatic
trend
Lifted
Condensation
Level
(LCL)
troposphere.
Rising
Sea-Surface
Temperature
(SST)
at
constant
Relative
Humidity
(RH)
elevating
clouds,
cooling
cloud
base
and
reducing
downward
thermal
radiation.
This
LCL
feedback
effect
negative
counteracting
current
SST
292
K,
net
radiative
from
surface
estimated
24
m–2.
Per
degree
increase,
this
expected
be
enhanced
almost
0.5
The
relevant
ocean’s
may
thermodynamically
rigorously
modelled
terms
TEOS-10
equations.
height
serve
as
remotely
measured,
sensitive
estimate
sea
relative
fugacity,
or
conventional
humidity.
Language: Английский
Globaler Klimawandel und die Energiewende
Mario Hoppema,
No information about this author
Carsten Fichter,
No information about this author
Richard Zahoransky
No information about this author
et al.
Energietechnik,
Journal Year:
2025,
Volume and Issue:
unknown, P. 77 - 115
Published: Jan. 1, 2025
TEOS-10 Equations for Determining the Lifted Condensation Level (LCL) and Climatic Feedback of Marine Clouds
Oceans,
Journal Year:
2024,
Volume and Issue:
5(2), P. 312 - 351
Published: May 28, 2024
At
an
energy
flux
imbalance
of
about
1
W
m−2,
the
ocean
stores
90%
heat
accumulating
by
global
warming.
However,
neither
causes
this
nor
responsible
geophysical
processes
are
sufficiently
well
understood.
More
detailed
investigations
different
phenomena
contributing
to
oceanic
balance
warranted.
Here,
role
low-level
marine
clouds
in
air–sea
interaction
is
analysed.
TEOS-10,
International
Thermodynamic
Equation
State
Seawater—2010,
exploited
for
a
rigorous
thermodynamic
description
climatic
trends
lifted
condensation
level
(LCL)
troposphere.
Rising
sea
surface
temperature
(SST)
at
constant
relative
humidity
(RH)
elevating
clouds,
cooling
cloud
base,
and
reducing
downward
thermal
radiation.
This
LCL
feedback
effect
negative
counteracts
current
mean
SST
292
K,
net
radiative
from
base
estimated
be
24
m−2.
Per
degree
increase,
expected
enhanced
almost
0.5
The
relevant
ocean’s
may
rigorously
thermodynamically
modelled
terms
TEOS-10
equations.
height
serve
as
remotely
measured,
sensitive
estimate
surface’s
fugacity,
or
conventional
humidity.
Language: Английский
The Impact of Marine Heatwaves on Isotherm Displacement and Tuna Distribution in Vanuatu
Climate,
Journal Year:
2024,
Volume and Issue:
12(11), P. 181 - 181
Published: Nov. 8, 2024
Marine
heatwaves
(MHWs)
have
intensified
in
frequency,
duration,
and
severity
over
recent
decades.
These
events,
defined
by
unusually
warm
sea
surface
temperatures
(SSTs),
can
cause
significant
ecological
impacts.
This
is
particularly
so
for
Pacific
Island
countries,
such
as
Vanuatu,
where
communities
rely
on
marine
resources
their
food
livelihoods.
A
common
response
to
MHWs
the
movement
of
oceanic
species
cooler
waters.
Predicting
shifts
through
monitoring
SST
isotherms
help
identify
thermal
boundaries
that
favor.
study
explores
connection
between
MHWs,
isotherm
movement,
tuna
abundance
Vanuatu.
The
displacement
28
°C
was
analyzed
across
three
major
MHW
events
(2008–2009,
2016,
2021–2022).
It
found
with
longer
duration
greater
intensity
caused
more
displacement.
Additionally,
El
Niño–Southern
Oscillation
had
an
important
influence
formation
movement.
effects
these
displacements
distribution
varied
events.
ability
monitor
could
be
effective
instrument
prediction
areas
suppressed
or
abundant
activity
used
aid
proactive
management
security
fishery
sectors.
Language: Английский
TEOS-10 and the climatic relevance of ocean–atmosphere interaction
Ocean science,
Journal Year:
2024,
Volume and Issue:
20(5), P. 1367 - 1402
Published: Oct. 29, 2024
Abstract.
Unpredicted
observations
in
the
climate
system,
such
as
recent
excessive
ocean
warming,
are
often
lacking
immediate
causal
explanations
and
challenging
numerical
models.
As
a
highly
advanced
mathematical
tool,
Thermodynamic
Equation
of
Seawater
–
2010
(TEOS-10)
was
established
by
international
bodies
an
interdisciplinary
standard
is
recommended
for
use
geophysics,
as,
particular,
research.
From
its
very
beginning,
development
TEOS-10
supported
Ocean
Science
through
publishing
successive
stages
results.
Here,
history
properties
briefly
reviewed.
With
focus
on
air–sea
interface,
selected
current
problems
research
discussed,
tutorial
examples
possible
associated
context
presented,
topics
related
to
heat
content,
latent
heat,
rate
marine
evaporation;
sea
spray
aerosol;
or
climatic
effects
low-level
clouds.
Appended
this
article,
list
publications
their
metrics
provided
illustrating
uptake
scientific
community,
along
with
some
continued
activities,
addressing
still
pending,
connected
issues
uniform
definitions
uncertainties
relative
humidity,
seawater
salinity,
pH.
This
article
dedicated
jubilee
celebrating
20
years
Science.
also
memory
Wolfgang
Wagner,
who
sadly
unexpectedly
passed
away
12
August
2024.
His
contributions
truly
indispensable
constituents;
essential
co-author
various
documents
articles.
He
will
be
deeply
missed.
All
rivers
run
into
sea;
yet
not
full;
unto
place
from
whence
come,
thither
they
return
again.
The
King
James
Bible:
Ecclesiastes,
450–150
BCE
wraps
up
waters
his
clouds,
clouds
do
burst
under
weight.
Holy
New
International
Version,
Job
26:8
Of
air,
part
receiving
rising
higher.
So,
evaporated
water
lifted
above
lower
air.
Leonardo
da
Vinci:
Primo
libro
delle
acque,
Codex
Arundel,
ca.
1508
Two-thirds
Sun's
energy
falling
Earth's
surface
needed
vaporize
…
source
gigantic
steam
engine.
Heinrich
Hertz:
Energiehaushalt
der
Erde,
1885
sea-surface
interaction
obviously
significant
quantity
simulating
climate.
Andrew
Gilchrist
Klaus
Hasselmann:
Climate
Modelling,
1986
Earth
ultimately
determined
temperatures
oceans.
Donald
Rapp:
Assessing
Change,
2014
Language: Английский