Abstract
Global
marine
heatwave
assessments
often
rely
on
satellite-derived
sea
surface
temperature.
However,
these
data
have
low
accuracy
in
coastal
areas,
are
unable
to
measure
sub-surface
temperatures
and
only
been
available
since
the
1980s.
Here,
we
analyse
90
years
of
situ
bottom
(30
m)
water
temperature
from
a
Finnish
monitoring
site.
Water
were
significantly
higher
between
1991–2020
than
1931–1960
1961–1990.
We
find
strong
differences
temperatures,
with
being
lower
autumn
winter
spring.
Measurements
at
seafloor
indicate
heatwaves
occurred
during
all
seasons
2016
2020,
intensities
durations
exceeding
previous
records.
Since
1990s,
an
upward
shift
baseline
increasingly
frequent
occurrence
previously
considered
as
extreme.
Our
findings
highlight
importance
long-term
choice
climatological
reference
periods
for
assessing
change.
Physiology,
Journal Year:
2019,
Volume and Issue:
34(2), P. 86 - 100
Published: Feb. 6, 2019
A
consequence
of
climate
change
is
the
increased
frequency
and
severity
extreme
heat
waves.
This
occurring
now
as
most
warmest
summers
intense
waves
ever
recorded
have
been
during
past
decade.
In
this
review,
I
describe
ways
in
which
animals
human
populations
are
likely
to
respond
heat,
suggest
how
study
those
responses,
reflect
on
importance
studies
for
countering
devastating
impacts
change.
Annual Review of Marine Science,
Journal Year:
2022,
Volume and Issue:
15(1), P. 119 - 145
Published: Aug. 17, 2022
Climatic
extremes
are
becoming
increasingly
common
against
a
background
trend
of
global
warming.
In
the
oceans,
marine
heatwaves
(MHWs)-discrete
periods
anomalously
warm
water-have
intensified
and
become
more
frequent
over
past
century,
impacting
integrity
ecosystems
globally.
We
review
synthesize
current
understanding
MHW
impacts
at
individual,
population,
community
levels.
then
examine
how
these
affect
broader
ecosystem
services
discuss
state
research
on
biological
MHWs.
Finally,
we
explore
emergent
approaches
to
predicting
occurrence
andimpacts
future
events,
along
with
adaptation
management
approaches.
With
further
increases
in
intensity
frequency
projected
for
coming
decades,
MHWs
emerging
as
pervasive
stressors
A
deeper
mechanistic
their
is
needed
better
predict
adapt
increased
activity
Anthropocene.
Nature Communications,
Journal Year:
2024,
Volume and Issue:
15(1)
Published: June 13, 2024
Abstract
With
increasingly
intense
marine
heatwaves
affecting
nearshore
regions,
foundation
species
are
coming
under
increasing
stress.
To
better
understand
their
impacts,
we
examine
responses
of
critical,
habitat-forming
(macroalgae,
seagrass,
corals)
to
in
1322
shallow
coastal
areas
located
across
85
ecoregions.
We
find
compelling
evidence
that
intense,
summer
play
a
significant
role
the
decline
globally.
Critically,
detrimental
effects
increase
towards
warm-range
edges
and
over
time.
also
identify
several
ecoregions
where
don’t
respond
heatwaves,
suggestive
some
resilience
warming
events.
Cumulative
heatwave
intensity,
absolute
temperature,
location
within
species’
range
key
factors
mediating
impacts.
Our
results
suggest
many
ecosystems
losing
species,
potentially
impacting
associated
biodiversity,
ecological
function,
ecosystem
services
provision.
Understanding
relationships
between
offers
potential
predict
impacts
critical
for
developing
management
adaptation
approaches.
Ecology Letters,
Journal Year:
2025,
Volume and Issue:
28(2)
Published: Feb. 1, 2025
ABSTRACT
Anthropogenic
activities
have
drastically
changed
environmental
conditions
worldwide,
negatively
impacting
biodiversity
and
ecosystem
services.
At
the
same
time,
majority
of
human
population
lives
in
urban
areas
that
are
greatly
altered
from
natural
habitats.
Nevertheless,
many
species
thrive
these
environments.
To
improve
our
knowledge
evolution
adaptation
anthropogenically
impacted
habitats,
we
conducted
widest
series
stress
experiments
to
date
with
three
marine
taxa:
one
mussel
two
gammarid
species.
We
compared
intraspecific
populations
protected
human‐altered
habitats
determine
their
tolerance
salinity,
temperature
partial
pressure
CO
2
water
(pCO
)
regimes.
Populations
typically
outperformed
habitat
populations,
individuals
most
being
robust.
propose
adapting
life
disturbed
environments—this
concurrently
promotes
more
resilient
rescue
but
potentially
confers
increased
invasion
risk
non‐native
Earth System Dynamics,
Journal Year:
2022,
Volume and Issue:
13(2), P. 711 - 747
Published: April 11, 2022
Abstract.
Climate
change
has
multiple
effects
on
Baltic
Sea
species,
communities
and
ecosystem
functioning
through
changes
in
physical
biogeochemical
environmental
characteristics
of
the
sea.
Associated
indirect
secondary
species
interactions,
trophic
dynamics
function
are
expected
to
be
significant.
We
review
studies
investigating
species-,
population-
ecosystem-level
abiotic
factors
that
may
due
global
climate
change,
such
as
temperature,
salinity,
oxygen,
pH,
nutrient
levels,
more
food
web
processes,
primarily
based
peer-reviewed
literature
published
since
2010.
For
phytoplankton,
clear
symptoms
prolongation
growing
season,
evident
can
explained
by
warming,
but
otherwise
vary
from
area
area.
Several
modelling
project
a
decrease
phytoplankton
bloom
spring
an
increase
cyanobacteria
blooms
summer.
The
associated
N:P
ratio
contribute
maintaining
“vicious
circle
eutrophication”.
However,
uncertainties
remain
because
some
field
claim
have
not
increased
experimental
show
responses
salinity
pH
species.
An
riverine
dissolved
organic
matter
(DOM)
also
primary
production,
relative
importance
this
process
different
sea
areas
is
well
known.
Bacteria
growth
favoured
increasing
temperature
DOM,
complex
microbial
probable.
Warming
seawater
speeds
up
zooplankton
shortens
time
lag
between
peaks,
which
lead
decreasing
spring.
In
summer,
shift
towards
smaller-sized
decline
marine
copepod
been
projected.
deep
benthic
communities,
continued
eutrophication
promotes
high
sedimentation
maintains
good
conditions
for
zoobenthos.
If
abatement
proceeds,
improving
oxygen
will
first
zoobenthos
biomass,
subsequent
sedimenting
disrupt
pelagic–benthic
coupling
decreased
biomass.
shallower
photic
systems,
heatwaves
produce
eutrophication-like
effects,
e.g.
overgrowth
bladderwrack
epiphytes,
cascade.
declines,
bladderwrack,
eelgrass
blue
mussel
decline.
Freshwater
vascular
plants
they
cannot
replace
macroalgae
rocky
substrates.
Consequently
invertebrates
fish
benefiting
macroalgal
belts
suffer.
Climate-induced
environment
favour
establishment
non-indigenous
potentially
affecting
Sea.
As
fish,
continuing
hypoxia
projected
keep
cod
stocks
low,
whereas
sprat
certain
coastal
fish.
Regime
shifts
cascading
observed
both
pelagic
systems
result
several
climatic
acting
synergistically.
Knowledge
gaps
include
projecting
future
level,
stratification
potential
rate
internal
loading,
under
forcings.
This
weakens
our
ability
how
productivity,
populations
future.
3D
models,
models
2D
distribution
would
benefit
integration,
progress
slowed
down
scale
problems
inability
consider
interactions
Experimental
work
should
better
integrated
into
empirical
get
comprehensive
view
bacteria
addition,
understand
biodiversity
Sea,
emphasis
placed
shallow
environments.
fate
depend
various
intertwined
development
society.
probably
delay
tend
its
“novel”
state.
conclude
reductions
stronger
driver
than
change.
Such
highlight
studying
interlinked
socio-ecological
system.
Frontiers in Marine Science,
Journal Year:
2022,
Volume and Issue:
8
Published: Jan. 7, 2022
Prolonged
events
of
anomalously
warm
sea
water
temperature,
or
marine
heatwaves
(MHWs),
have
major
detrimental
effects
to
ecosystems
and
the
world's
economy.
While
frequency,
duration
intensity
MHWs
been
observed
increase
in
global
oceans,
little
is
known
about
their
potential
occurrence
variability
estuarine
systems
due
limited
data
these
environments.
In
present
study
we
analyzed
a
novel
set
with
over
three
decades
continuous
situ
temperature
records
investigate
largest
most
productive
estuary
US:
Chesapeake
Bay.
occurred
on
average
twice
per
year
lasted
11
days,
resulting
22
MHW
days
bay.
Average
intensities
were
3°C,
maximum
peaks
varying
between
6
8°C,
yearly
cumulative
72°C
×
average.
Large
co-occurrence
was
different
regions
bay
(50–65%),
also
Bay
Mid-Atlantic
Bight
(40–50%).
These
large
co-occurrences,
relatively
short
lags
(2–5
days),
suggest
that
coherent
large-scale
air-sea
heat
flux
dominant
driver
this
region.
linked
climate
modes
variability:
enhancement
Upper
associated
positive
phase
Niño
1+2,
while
suppression
both
Mid
Lower
negative
phases
North
Atlantic
Oscillation,
respectively.
Finally,
as
result
long-term
warming
Bay,
significant
trends
detected
for
intensity.
If
persist,
by
end
century
will
reach
semi-permanent
state,
when
extreme
temperatures
be
half
year,
thus
could
devastating
impacts
ecosystem,
exacerbating
eutrophication,
increasing
severity
hypoxic
events,
killing
benthic
communities,
causing
shifts
species
composition
decline
important
commercial
fishery
species.
Improving
our
basic
understanding
necessary
future
predictability
guide
management
decisions
valuable
Journal of Geophysical Research Oceans,
Journal Year:
2024,
Volume and Issue:
129(3)
Published: Feb. 26, 2024
Abstract
Subsurface
impacts
associated
with
Marine
Heatwaves
(MHWs)
in
estuaries
are
not
well
understood,
largely
due
to
data
scarcity.
Using
over
three
decades
(1986–2021)
of
observations
from
several
monitoring
programs,
this
study
investigates
subsurface
temperature
and
dissolved
oxygen
(DO)
anomalies
surface
MHWs
the
Chesapeake
Bay
(CB).
Seasonal
variability
followed
a
simple
1‐D
response
heating
downward
heat
transport
diffusion
controlled
by
seasonally
variable
stratification
mixing.
Two
distinct
regimes
were
found:
thermally
stratified
spring‐summer
regime,
when
positive
confined
mixed
layer
(SML);
homogeneous
fall‐winter
regime.
Additionally,
(subsurface)
temperatures
elevated
for
months
(days
weeks)
before
after
MHWs,
indicating
individual
events
shorter
than
timescales
temperatures.
A
SML
budget
identified
air‐estuary
flux
changes
as
leading
driver
MHW
onsets
declines,
latent
being
dominant
term.
DO
anomaly
patterns
more
complex,
considerable
along‐channel
gradients.
Notable
decreases
(1–4
mg
L
−1
)
primarily
occurred
winter/spring
below
SML,
hypoxic
zone
expanded
spring
through
fall.
Only
small
fraction
these
could
be
attributed
temperature‐induced
solubility
changes,
demonstrating
that
other
physical
and/or
biogeochemical
processes
dominate
during
events.
In
CB,
concurrent
low
persistent
high
compound
on
valuable
ecosystem,
event
likely
exacerbated
climate
change.