Biogeosciences,
Journal Year:
2024,
Volume and Issue:
21(2), P. 605 - 623
Published: Jan. 29, 2024
Abstract.
Climate
data
matching
the
scales
at
which
organisms
experience
climatic
conditions
are
often
missing.
Yet,
such
on
microclimatic
required
to
better
understand
climate
change
impacts
biodiversity
and
ecosystem
functioning.
Here
we
combine
a
network
of
microclimate
temperature
measurements
across
different
habitats
vertical
heights
with
novel
radiative
transfer
model
map
daily
temperatures
during
vegetation
period
10
m
spatial
resolution
Switzerland.
Our
results
reveal
strong
horizontal
variability
in
temperature,
particularly
for
maximum
5
cm
above
ground
within
topsoil.
Compared
macroclimate
as
measured
by
weather
stations
outside
forests,
diurnal
air
topsoil
ranges
inside
forests
were
reduced
up
3.0
7.8
∘C,
respectively,
while
below
trees
e.g.
hedges
solitary
trees,
this
buffering
effect
was
1.8
7.2
respectively.
We
also
found
that,
open
grasslands,
are,
average,
3.4
∘C
warmer
than
those
macroclimate,
suggesting
habitats,
heat
exposure
close
is
underestimated
when
using
macroclimatic
data.
Spatial
interpolation
achieved
hybrid
approach
based
linear
mixed-effect
models
input
from
detailed
radiation
estimates
that
account
topographic
shading,
well
other
predictor
variables
related
topography,
height.
After
accounting
effects,
patterns
primarily
driven
radiation,
effects
temperatures.
Results
block
cross-validation
revealed
predictive
accuracies
root
mean
squared
errors
ranging
1.18
3.43
minimum
being
predicted
more
accurately
overall
The
microclimate-mapping
methodology
presented
here
enables
biologically
relevant
perspective
analysing
climate–species
interactions,
expected
lead
understanding
biotic
responses
land
use
change.
Global Change Biology,
Journal Year:
2019,
Volume and Issue:
26(2), P. 1003 - 1011
Published: Oct. 22, 2019
Abstract
Most
studies
on
the
biological
effects
of
future
climatic
changes
rely
seasonally
aggregated,
coarse‐resolution
data.
Such
data
mask
spatial
and
temporal
variability
in
microclimate
driven
by
terrain,
wind
vegetation,
ultimately
bear
little
resemblance
to
conditions
that
organisms
experience
wild.
Here,
I
present
methods
for
providing
fine‐grained,
hourly
daily
estimates
current
temperature
soil
moisture
over
decadal
timescales.
Observed
climate
spatially
coherent
probabilistic
projections
weather
were
disaggregated
used
drive
empirically
calibrated
physical
models
thermal
hydrological
microclimates.
Mesoclimatic
(cold‐air
drainage,
coastal
exposure
elevation)
determined
from
surfaces
using
thin‐plate
spline
with
elevation
as
predictors.
Differences
between
micro
mesoclimate
temperatures
vegetation
ground
properties
energy
balance
equations.
Soil
was
computed
a
thin
upper
layer
an
underlying
deeper
layer,
exchange
water
these
layers
calculated
van
Genuchten
equation.
Code
processing
running
is
provided
series
R
packages.
The
applied
Lizard
Peninsula,
United
Kingdom,
provide
(100
m
grid
resolution
entire
area,
1
selected
area)
periods
1983–2017
2041–2049.
Results
indicated
there
fine‐resolution
changes,
primarily
interactions
landscape
features
trends
conditions.
High‐temporal
extremes
under
change
predicted
be
considerably
less
novel
than
estimated
aggregated
variables.
study
highlights
need
more
accurately
estimate
experienced
equips
biologists
means
do
so.
Journal of Ecology,
Journal Year:
2019,
Volume and Issue:
108(4), P. 1411 - 1425
Published: Dec. 19, 2019
Abstract
A
central
challenge
of
today's
ecological
research
is
predicting
how
ecosystems
will
develop
under
future
global
change.
Accurate
predictions
are
complicated
by
(a)
simultaneous
effects
different
drivers,
such
as
climate
change,
nitrogen
deposition
and
management
changes;
(b)
legacy
from
previous
land
use.
We
tested
whether
herb
layer
biodiversity
(i.e.
richness,
Shannon
diversity
evenness)
functional
cover,
specific
leaf
area
[SLA]
plant
height)
responses
to
environmental
change
drivers
depended
on
land‐use
history.
used
resurvey
data
192
plots
across
nineteen
European
temperate
forest
regions,
with
large
spatial
variability
in
factors.
for
interactions
between
history,
distinguishing
ancient
recent
post‐agricultural)
forests
four
drivers:
temperature,
deposition,
aridity
at
the
regional
scale
light
dynamics
plot‐scale.
Land‐use
history
significantly
modulated
signature
SLA
height).
Light
availability
was
main
driver
interacting
found
greater
cover
height
decreases
increases
decreasing
than
forests.
Furthermore,
we
increased
forests,
whereas
warming
had
strongest
effect
Interactive
were
not
found,
but
species
evenness
more
Synthesis
.
Our
results
demonstrate
that
should
be
overlooked
when
Moreover,
composition
semi‐natural
deciduous
mainly
controlled
local
canopy
characteristics,
regulating
levels
floor,
much
less
changes
(here:
warming,
aridity).
The
observed
disconnect
demonstrates
importance
assessing
both
types
increase
our
understanding
possible
impact
layer.
New Phytologist,
Journal Year:
2022,
Volume and Issue:
237(1), P. 22 - 47
Published: Oct. 14, 2022
Rising
temperatures
are
influencing
forests
on
many
scales,
with
potentially
strong
variation
vertically
across
forest
strata.
Using
published
research
and
new
analyses,
we
evaluate
how
microclimate
leaf
temperatures,
traits,
gas
exchange
vary
in
forests,
shaping
tree,
ecosystem
ecology.
In
closed-canopy
upper
canopy
leaves
exposed
to
the
highest
solar
radiation
evaporative
demand,
which
can
elevate
temperature
(Tleaf
),
particularly
when
transpirational
cooling
is
curtailed
by
limited
stomatal
conductance.
However,
foliar
traits
also
height
or
light
gradients,
partially
mitigating
protecting
against
elevation
of
Tleaf
.
Leaf
metabolism
generally
increases
vertical
gradient,
yet
differences
thermal
sensitivity
gradient
appear
modest.
Scaling
from
trees,
trees
have
higher
absolute
metabolic
capacity
growth,
more
vulnerable
drought
damaging
than
their
smaller
counterparts,
under
climate
change.
By
contrast,
understory
experience
fewer
extreme
high
's
but
mechanisms
thus
may
be
strongly
impacted
warming
some
conditions,
a
harsher
microenvironment
through
disturbance.
As
changes,
integrating
patterns
reviewed
here
into
models
will
critical
forecasting
forest-climate
feedback.
Global Change Biology,
Journal Year:
2022,
Volume and Issue:
28(24), P. 7340 - 7352
Published: Sept. 5, 2022
Current
climate
change
aggravates
human
health
hazards
posed
by
heat
stress.
Forests
can
locally
mitigate
this
acting
as
strong
thermal
buffers,
yet
potential
mediation
forest
ecological
characteristics
remains
underexplored.
We
report
over
14
months
of
hourly
microclimate
data
from
131
plots
across
four
European
countries
and
compare
these
to
open-field
controls
using
physiologically
equivalent
temperature
(PET)
reflect
perception.
slightly
tempered
cold
extremes,
but
the
strongest
buffering
occurred
under
very
hot
conditions
(PET
>35°C),
where
forests
reduced
extreme
stress
day
occurrence
84.1%.
Mature
cooled
12.1
14.5°C
PET
under,
respectively,
conditions.
Even
young
plantations
those
10°C
PET.
Forest
structure
strongly
modulated
capacity,
which
was
enhanced
increasing
stand
density,
canopy
height
closure.
Tree
species
composition
had
a
more
modest
significant
influence:
that
is,
shade-casting,
small-leaved
evergreen
amplified
cooling.
diversity
little
direct
influences,
though
indirect
effects
through
remain
possible.
in
general,
both
mature,
are
thus
reducers,
their
cooling
be
even
further
amplified,
given
targeted
(urban)
management
considers
new
insights.
Journal of Applied Ecology,
Journal Year:
2022,
Volume and Issue:
59(6), P. 1428 - 1439
Published: March 11, 2022
Abstract
Macroclimate
warming
is
affecting
ecosystems
world‐wide.
Tree
canopies,
however,
can
significantly
buffer
temperature
fluctuations,
giving
rise
to
lower
maximum
temperatures,
higher
minimum
temperatures
and
enhanced
water
availability
at
the
forest
floor.
Forests,
therefore,
act
as
refugia
for
heat‐sensitive
species
with
important
implications
climate‐change
responses
in
understorey
of
forests.
These
microclimate
offsets
have
been
well‐studied,
but
far
less
known
about
how
are
modulated
by
tree
mixing.
We
installed
air
humidity
loggers
a
multisite
diversity
experiment
quantify
role
richness
composition
on
below‐canopy
investigate
mechanisms
underlying
these
effects.
Microclimate
highly
depended
identity
Not
only
monocultures
larch
Larix
×
eurolepis
Douglas
fir
Pseudotsuga
menziesii
had
high
performance
thermal
buffering,
also
mixtures
such
birch
Betula
pendula
pine
Pinus
sylvestris
.
Indirect
effects
brought
mixing
were
found
amplify
offsets,
mostly
via
increased
canopy
cover.
Synthesis
applications
Our
findings
show
that
offsetting
depends
diversity,
buffered
microclimates
be
achieved
rapidly
young
plantations,
depending
being
planted.
Based
our
findings,
we
recommend
planting
instead
monocultures.
because
was
some
investigated
stands,
likely
increase
resilience
forests
climate
change.
Hence,
expect
long‐term
might
beneficial
buffering.
Forest
managers
policy
makers
use
finding
optimise
design
plantations
minimise
impacts
biodiversity
functioning.
Ecology Letters,
Journal Year:
2023,
Volume and Issue:
26(12), P. 2043 - 2055
Published: Oct. 3, 2023
Species
distributions
are
conventionally
modelled
using
coarse-grained
macroclimate
data
measured
in
open
areas,
potentially
leading
to
biased
predictions
since
most
terrestrial
species
reside
the
shade
of
trees.
For
forest
plant
across
Europe,
we
compared
conventional
macroclimate-based
distribution
models
(SDMs)
with
corrected
for
microclimate
buffering.
We
show
that
microclimate-based
SDMs
at
high
spatial
resolution
outperformed
and
coarser
resolution.
Additionally,
introduced
a
systematic
bias
response
curves,
which
could
result
erroneous
range
shift
predictions.
Critically
important
conservation
science,
these
were
unable
identify
warm
cold
refugia
edges
distributions.
Our
study
emphasizes
crucial
role
when
used
gain
insights
into
biodiversity
face
climate
change,
particularly
given
growing
policy
management
focus
on
worldwide.
Agricultural and Forest Meteorology,
Journal Year:
2023,
Volume and Issue:
345, P. 109828 - 109828
Published: Dec. 1, 2023
Forest
canopies
can
buffer
the
understory
against
temperature
extremes,
often
creating
cooler
microclimates
during
warm
summer
days
compared
to
temperatures
outside
forest.
The
buffering
of
maximum
in
results
from
a
combination
canopy
shading
and
air
cooling
through
soil
water
evaporation
plant
transpiration.
Therefore,
capacity
forests
depends
on
cover
moisture
content,
which
are
increasingly
affected
by
more
frequent
severe
disturbances
droughts.
extent
this
will
be
maintained
future
conditions
is
unclear
due
lack
understanding
about
relationship
between
interaction
with
topographic
settings.
We
explored
how
variability
affects
offsets
inside
forest
daily
basis,
using
data
54
sites
temperate
broadleaf
Central
Europe
over
four
climatically
different
seasons.
Daily
understories
were
average
2
°C
than
temperatures.
was
effective
when
higher,
sensitive
drier
soils
sun-exposed
slopes
high
heat
load.
Based
these
results,
soil–water
limitation
become
prevalent
under
warmer
likely
lead
changes
communities.
Thus,
our
highlight
urgent
need
include
models
predictions
microclimate,
biodiversity
tree
regeneration,
provide
precise
estimate
effects
climate
change.