Research Square (Research Square),
Journal Year:
2021,
Volume and Issue:
unknown
Published: June 29, 2021
Abstract
Surface
velocity
observations
of
the
eastern
part
Tsugaru
Strait
made
by
high-frequency
radar
revealed
frequent
occurrence
frontal
waves
along
axis
Warm
Current
in
2017–2019.
The
current
(maximum
zonal
meridional
direction)
disturbed
north–south
direction
with
period
~
13.7
days
that
is
dominant
timescale
tide
modulation
strait,
addition
to
27.3
days.
amplitude
fluctuation
increased
downstream
direction,
from
neck
channel
(~
141.0°E)
outlet
strait
adjacent
Pacific
Ocean
141.5°E).
propagation
speed
disturbance
was
slower
than
due
surface
advection
especially
seasons
when
stratification
developed,
and
agreed
well
estimated
theory
based
on
two-layer
baroclinic
instability
model
except
for
winter.
at
141.5°E)
could
cause
short-term
(from
20
1
month)
variations
an
anticyclonic
gyre
developed
east
summer
autumn
reported
previous
studies.
Environmental Research,
Journal Year:
2023,
Volume and Issue:
244, P. 115691 - 115691
Published: May 19, 2023
Environmental
changes
such
as
seasonality,
decadal
oscillation,
and
anthropogenic
forcing
may
shape
the
dynamics
of
lower
trophic-level
organisms.
In
this
study,
9-years
(2010-2018)
monitoring
data
on
microscopic
protists
diatoms
dinoflagellates,
environmental
variables
were
analyzed
to
clarify
relationships
between
plankton
local/synoptic
changes.
We
found
that
time-series
temperature
increased
in
May,
whereas
it
decreased
August
November.
Nutrients
(e.g.,
phosphate)
remained
unchanged
August,
November
from
2010
2018.
The
partial
pressure
CO
Frontiers in Marine Science,
Journal Year:
2023,
Volume and Issue:
10
Published: Sept. 27, 2023
An
approach
was
developed
to
help
evaluate
and
predict
the
combined
effects
of
ocean
acidification
deoxygenation
on
calcifying
organisms
along
coast
Japan.
The
Coastal
Regional
Ocean
COmmunity
(CROCO)
modeling
system
set
up
couple
Modeling
System
(ROMS)
Pelagic
Interaction
Scheme
for
Carbon
Ecosystem
Studies
(PISCES)
biogeochemical
model
used
reproduce
physical
biochemical
processes
in
area
around
Miyako
Bay,
Iwate
Prefecture,
Future
scenario
cases
were
also
up,
which
initial
boundary
conditions
based
Projection
(FORP)
simulations.
Present
day
simulations
able
general
features
observed
parameters,
except
some
rapid
decreases
salinity,
pH
aragonite
saturation
state
(Ω
arag
).
This
suggests
that
more
local
factors
have
not
been
introduced
into
model,
such
as
submarine
groundwater
discharge,
may
be
involved,
or
river
inputs
underestimated.
Results
future
projections
suggest
a
significant
impact
global
warming
worst
case
climate
change
under
Representative
Concentration
Pathway
(RCP)
8.5
scenario.
In
particular,
it
is
feared
values
Ω
would
critical
level
<
1.1)
throughout
year,
decreased
larval
shell
lengths
malformation
experimentally
locally
grown
Haliotis
discus
hannai
(Ezo
Abalone)
species.
However,
these
findings
true
different
coastal
locality,
this
study
highlights
continues
stress
importance
developing
setups
capable
incorporating
both
regional
affecting
deoxygenation.
Progress in Earth and Planetary Science,
Journal Year:
2022,
Volume and Issue:
9(1)
Published: Oct. 15, 2022
Abstract
The
eastern
part
of
the
Tsugaru
Strait
(located
at
~
41.5°
N)
is
a
remarkable
region
coastal
flow
system
around
Japan
due
to
Warm
Current
(TgWC),
an
intensive
eastward
current
that
flows
over
its
complex
topography
and
exhibits
marked
tidal
variation.
TgWC
has
jetlike
structure
demonstrates
drastic
seasonal
changes
in
path
vertical
structure.
Using
high-resolution
dataset
obtained
from
high-frequency
radar
(HFR)
data
assimilation
experiment
(JCOPE-T
DA),
we
focused
on
frontal
variation,
which
shorter
than
timescale,
along
axis
relation
meanders
jet.
We
found
variations
with
multiple
timescales
between
1
14
days,
especially
summer
autumn.
14-day
occurrence
west
side
Strait,
was
consistent
variation
strait.
zonal
scale
meander
estimated
by
HFR
matched
several
times
larger
internal
deformation
radius,
JCOPE-T
DA
outputs
showed
crest
such
greater
depths
progresses
surface.
also
suggested
instabilities,
indicating
potential
kinetic
energy
conversion
mean
eddy
field.
propagation
speed
several-day
two-layer
baroclinic
instability.
relatively
high
coherence
wind
autumn,
during
time
strait
switched
easterly
westerly.
These
imply
effect
north–south
water
mass
mixing
strait,
including
rapid
acidification
intensification
stratification.
Progress in Earth and Planetary Science,
Journal Year:
2022,
Volume and Issue:
9(1)
Published: Oct. 22, 2022
Abstract
The
2011
off
the
Pacific
coast
of
Tohoku
Earthquake
occurred
southern
Sanriku,
Japan,
on
March
11
and
generated
strong
shaking
huge
tsunami
along
entire
eastern
Tohoku.
mainshock
numerous
large
aftershocks
caused
mass-wasting
sedimentation
events
continental
shelf,
slope,
trench
bottom.
To
investigate
impacts
deep-sea
bottom-water
environment
we
conducted
shipboard
surveys
up
to
~
2000
dbar
during
2011–2018
long-term
monitoring
seafloor
slope
using
a
station
(~
1000
dbar)
Otsuchi
Bay
2012–2018.
high
turbidity
(maximum
6%)
was
observed
for
bottom
water
deeper
than
500
area
Sanriku
This
by
sporadic
sediment
resuspension
induced
frequent
aftershocks.
Furthermore,
dissolved
oxygen
concentrations
in
layer
from
1500
dropped
significantly
about
10%
after
earthquake,
while
nutrients
inorganic
carbon
showed
no
significant
changes
but
exhibited
wide
variations.
associated
with
increase
phosphate,
carbon,
methane,
as
well
decrease
those
nitrate.
suggests
that
remineralization
suspended
organic
matter
resulting
respiration
denitrification
microbial
communities
earthquake
chemical
properties
bottom-water.
change
maintained
due
continued
likely
variations
phosphate.
There
are
two
peaks
concentration
isotope
ratio
methane
near
hypocenter,
which
were
advected
isopycnal
surfaces
27.38σ
θ
(1000
27.56σ
(1500
dbar).
source
shallower
peak
input
is
considered
be
shallow
Graphical
abstract
Abstract.
The
pH
of
coastal
seawater
varies
based
on
several
local
forcings,
such
as
water
circulation,
terrestrial
inputs,
and
biological
processes,
these
forcings
can
change
along
with
global
climate
change.
Understanding
the
mechanism
variation
in
each
area
is
thus
important
for
a
realistic
future
projection
that
considers
changes
forcings.
From
2020
to
2021,
we
performed
parallel
year-round
observations
related
ocean
parameters
at
five
stations
around
Japanese
coast
(Miyako
Bay,
Shizugawa
Kashiwazaki
Coast,
Hinase
Archipelago,
Ohno
Strait)
understand
characteristics
short-term
variations
their
Annual
variability
(~1
standard
deviation)
aragonite
saturation
state
(Ωara)
were
0.05–0.09
0.25–0.29,
respectively,
three
areas
low
anthropogenic
loadings
Bay),
while
it
increased
0.16–0.21
0.52–0.58,
two
medium
(Hinase
Archipelago
Strait
Seto
Inland
Sea).
Statistical
assessment
temporal
various
timescales
revealed
most
annual
variabilities
both
Ωara
derived
by
timescale
<
10
days,
rather
than
seasonal-scale
variation.
Our
analyses
further
illustrated
was
caused
thermodynamic
processes
equally
contributed
Ωara.
observed
results
showed
acidification
1.5
occurred
occasionally
Miyako
Bays,
frequently
Strait.
Most
acidified
events
low-salinity
events.
amplitude
linearly
correlated
salinity
variation,
its
regression
coefficient
time
high
freshwater
input
positively
nutrient
concentration
main
river
flows
into
area.
Abstract.
The
pH
of
coastal
seawater
varies
based
on
several
local
forcings,
such
as
water
circulation,
terrestrial
inputs,
and
biological
processes,
these
forcings
can
change
along
with
global
climate
change.
Understanding
the
mechanism
variation
in
each
area
is
thus
important
for
a
realistic
future
projection
that
considers
changes
forcings.
From
2020
to
2021,
we
performed
parallel
year-round
observations
related
ocean
parameters
at
five
stations
around
Japanese
coast
(Miyako
Bay,
Shizugawa
Kashiwazaki
Coast,
Hinase
Archipelago,
Ohno
Strait)
understand
characteristics
short-term
variations
their
Annual
variability
(~1
standard
deviation)
aragonite
saturation
state
(Ωara)
were
0.05–0.09
0.25–0.29,
respectively,
three
areas
low
anthropogenic
loadings
Bay),
while
it
increased
0.16–0.21
0.52–0.58,
two
medium
(Hinase
Archipelago
Strait
Seto
Inland
Sea).
Statistical
assessment
temporal
various
timescales
revealed
most
annual
variabilities
both
Ωara
derived
by
timescale
<
10
days,
rather
than
seasonal-scale
variation.
Our
analyses
further
illustrated
was
caused
thermodynamic
processes
equally
contributed
Ωara.
observed
results
showed
acidification
1.5
occurred
occasionally
Miyako
Bays,
frequently
Strait.
Most
acidified
events
low-salinity
events.
amplitude
linearly
correlated
salinity
variation,
its
regression
coefficient
time
high
freshwater
input
positively
nutrient
concentration
main
river
flows
into
area.
Abstract.
The
pH
of
coastal
seawater
varies
based
on
several
local
forcings,
such
as
water
circulation,
terrestrial
inputs,
and
biological
processes,
these
forcings
can
change
along
with
global
climate
change.
Understanding
the
mechanism
variation
in
each
area
is
thus
important
for
a
realistic
future
projection
that
considers
changes
forcings.
From
2020
to
2021,
we
performed
parallel
year-round
observations
related
ocean
parameters
at
five
stations
around
Japanese
coast
(Miyako
Bay,
Shizugawa
Kashiwazaki
Coast,
Hinase
Archipelago,
Ohno
Strait)
understand
characteristics
short-term
variations
their
Annual
variability
(~1
standard
deviation)
aragonite
saturation
state
(Ωara)
were
0.05–0.09
0.25–0.29,
respectively,
three
areas
low
anthropogenic
loadings
Bay),
while
it
increased
0.16–0.21
0.52–0.58,
two
medium
(Hinase
Archipelago
Strait
Seto
Inland
Sea).
Statistical
assessment
temporal
various
timescales
revealed
most
annual
variabilities
both
Ωara
derived
by
timescale
<
10
days,
rather
than
seasonal-scale
variation.
Our
analyses
further
illustrated
was
caused
thermodynamic
processes
equally
contributed
Ωara.
observed
results
showed
acidification
1.5
occurred
occasionally
Miyako
Bays,
frequently
Strait.
Most
acidified
events
low-salinity
events.
amplitude
linearly
correlated
salinity
variation,
its
regression
coefficient
time
high
freshwater
input
positively
nutrient
concentration
main
river
flows
into
area.