Environmental Research Letters,
Journal Year:
2023,
Volume and Issue:
18(6), P. 064023 - 064023
Published: May 12, 2023
Abstract
As
climate
change
advances,
there
is
a
need
to
examine
conditions
at
scales
that
are
ecologically
relevant
species.
While
microclimates
in
forested
systems
have
been
extensively
studied,
grasslands
received
little
attention
despite
the
vulnerability
of
this
endangered
biome.
We
employed
novel
combination
iButton
temperature
and
humidity
measurements,
fine-scale
spatial
observations
vegetation
topography
collected
by
unpiloted
aircraft
system,
gridded
mesoclimate
products
model
microclimate
anomalies
temperate
grasslands.
found
harbored
diverse
primary
productivity
(as
represented
normalized
difference
index),
canopy
height,
were
strong
drivers
these
anomalies.
Microclimate
heterogeneity
likely
ecological
importance
grassland
organisms
seeking
out
refugia,
thus
consider
complexity
management
conservation
biodiversity.
Global Change Biology,
Journal Year:
2021,
Volume and Issue:
28(9), P. 3110 - 3144
Published: Dec. 30, 2021
Research
in
global
change
ecology
relies
heavily
on
climatic
grids
derived
from
estimates
of
air
temperature
open
areas
at
around
2
m
above
the
ground.
These
do
not
reflect
conditions
below
vegetation
canopies
and
near
ground
surface,
where
critical
ecosystem
functions
occur
most
terrestrial
species
reside.
Here,
we
provide
maps
soil
bioclimatic
variables
a
1-km2
resolution
for
0-5
5-15
cm
depth.
were
created
by
calculating
difference
(i.e.
offset)
between
situ
measurements,
based
time
series
over
1200
pixels
(summarized
8519
unique
sensors)
across
all
world's
major
biomes,
coarse-grained
ERA5-Land
(an
atmospheric
reanalysis
European
Centre
Medium-Range
Weather
Forecasts).
We
show
that
mean
annual
differs
markedly
corresponding
gridded
temperature,
up
to
10°C
(mean
=
3.0
±
2.1°C),
with
substantial
variation
biomes
seasons.
Over
year,
soils
cold
and/or
dry
are
substantially
warmer
(+3.6
2.3°C)
than
whereas
warm
humid
environments
average
slightly
cooler
(-0.7
2.3°C).
The
observed
biome-specific
offsets
emphasize
projected
impacts
climate
near-surface
biodiversity
functioning
inaccurately
assessed
when
rather
is
used,
especially
environments.
soil-related
provided
here
an
important
step
forward
any
application
related
disciplines.
Nevertheless,
highlight
need
fill
remaining
geographic
gaps
collecting
more
measurements
microclimate
further
enhance
spatiotemporal
products
ecological
applications.
Global Change Biology,
Journal Year:
2021,
Volume and Issue:
27(23), P. 6307 - 6319
Published: Oct. 3, 2021
Ecological
research
heavily
relies
on
coarse-gridded
climate
data
based
standardized
temperature
measurements
recorded
at
2
m
height
in
open
landscapes.
However,
many
organisms
experience
environmental
conditions
that
differ
substantially
from
those
captured
by
these
macroclimatic
(i.e.
free
air)
grids.
In
forests,
the
tree
canopy
functions
as
a
thermal
insulator
and
buffers
sub-canopy
microclimatic
conditions,
thereby
affecting
biological
ecological
processes.
To
improve
assessment
of
climatic
climate-change-related
impacts
forest-floor
biodiversity
functioning,
high-resolution
grids
reflecting
forest
microclimates
are
thus
urgently
needed.
Combining
more
than
1200
time
series
situ
near-surface
with
topographical,
variables
machine
learning
model,
we
predicted
mean
monthly
offset
between
15
cm
above
surface
free-air
over
period
2000-2020
spatial
resolution
25
across
Europe.
This
was
used
to
evaluate
difference
microclimate
macroclimate
space
seasons
finally
enabled
us
calculate
annual
temperatures
for
European
understories.
We
found
air
temperatures,
being
average
2.1°C
(standard
deviation
±
1.6°C)
lower
summer
2.0°C
higher
(±0.7°C)
winter
Additionally,
our
maps
expose
considerable
variation
within
landscapes,
not
gridded
products.
The
provided
will
enable
future
model
below-canopy
processes
patterns,
well
species
distributions
accurately.
Global Change Biology,
Journal Year:
2022,
Volume and Issue:
29(6), P. 1451 - 1470
Published: Dec. 14, 2022
A
core
challenge
in
global
change
biology
is
to
predict
how
species
will
respond
future
environmental
and
manage
these
responses.
To
make
such
predictions
management
actions
robust
novel
futures,
we
need
accurately
characterize
organisms
experience
their
environments
the
biological
mechanisms
by
which
they
respond.
All
are
thermodynamically
connected
through
exchange
of
heat
water
at
fine
spatial
temporal
scales
this
can
be
captured
with
biophysical
models.
Although
mechanistic
models
based
on
ecology
have
a
long
history
development
application,
use
remains
limited
despite
enormous
promise
increasingly
accessible
software.
We
contend
that
greater
understanding
training
theory
methods
vital
expand
application.
Our
review
shows
implemented
understand
climate
impacts
species'
behavior,
phenology,
survival,
distribution,
abundance.
It
also
illustrates
types
outputs
generated,
data
inputs
required
for
different
implementations.
Examples
range
from
simple
calculations
body
temperature
particular
site
time,
more
complex
analyses
distribution
limits
projected
energy
balances,
accounting
behavior
phenology.
outline
challenges
currently
limit
widespread
application
relating
availability,
training,
lack
common
software
ecosystems.
discuss
progress
developments
could
allow
applied
many
across
large
extents
timeframes.
Finally,
highlight
uniquely
suited
solve
problems
involve
predicting
interpreting
responses
variability
extremes,
multiple
or
shifting
constraints,
abiotic
biotic
environments.
Global Ecology and Biogeography,
Journal Year:
2024,
Volume and Issue:
33(6)
Published: April 8, 2024
Abstract
Brief
introduction:
What
are
microclimates
and
why
they
important?
Microclimate
science
has
developed
into
a
global
discipline.
is
increasingly
used
to
understand
mitigate
climate
biodiversity
shifts.
Here,
we
provide
an
overview
of
the
current
status
microclimate
ecology
biogeography
in
terrestrial
ecosystems,
where
this
field
heading
next.
investigations
We
highlight
latest
research
on
interactions
between
organisms,
including
how
influence
individuals,
through
them
populations,
communities
entire
ecosystems
their
processes.
also
briefly
discuss
recent
organisms
shape
from
tropics
poles.
applications
ecosystem
management
Microclimates
important
under
change.
showcase
new
with
examples
conservation,
forestry
urban
ecology.
importance
microrefugia
conservation
promote
heterogeneity.
Methods
for
advances
data
acquisition,
such
as
novel
sensors
remote
sensing
methods.
modelling,
mapping
processing,
accessibility
modelling
tools,
advantages
mechanistic
statistical
solutions
computational
challenges
that
have
pushed
state‐of‐the‐art
field.
What's
next?
identify
major
knowledge
gaps
need
be
filled
further
advancing
investigations,
These
include
spatiotemporal
scaling
data,
mismatches
macroclimate
predicting
responses
change,
more
evidence
outcomes
management.
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.
Methods in Ecology and Evolution,
Journal Year:
2023,
Volume and Issue:
14(3), P. 885 - 897
Published: Jan. 3, 2023
Abstract
Most
statistical
models
of
microclimate
focus
on
the
difference
or
‘offset’
between
standardized
air
temperatures
(macroclimate)
and
those
a
specific
habitat
such
as
forest
understorey,
grassland
under
log.
However,
these
offsets
can
fluctuate
from
positive
to
negative
over
single
day
that
common
practice
consists
in
aggregating
data
into
daily
mean,
minimum
maximum
before
modelling
monthly
for
each
summary
statistic.
Here,
we
propose
more
parsimonious
flexible
approach
relying
just
two
parameters:
slope
equilibrium.
The
captures
linear
relationship
macroclimate,
while
equilibrium
is
point
at
which
equals
macroclimate.
Although
applicable
other
habitats,
demonstrate
relevance
our
method
by
focusing
understoreys.
We
installed
temperature
sensors
1‐m
height
inside
stands
nearby
open
grasslands
equipped
with
weather
stations,
across
13
sites
France
spanning
wide
climatic
gradient.
From
year
hourly
sensor,
established
relationships
macroclimate
using
mixed‐effects
models,
during
leaf‐on
(May–November)
leaf‐off
period
(December–April).
extracted
used
another
set
investigate
their
main
determinants.
was
chiefly
determined
stand
structure
variables
interacting
leaf‐on/leaf‐off
period:
type
(conifer
vs
broadleaf);
shade‐casting
ability;
age;
dominant
height;
stem
density;
cover
upper
lower
shrub
layer.
In
contrast,
had
no
explanatory
power
found
be
positively
related
mean
temperature,
open/forest
habitat.
introduced
here
overcomes
several
shortcomings
offsets.
By
demonstrating
vary
predictable
ways,
have
general
linkage
applied
any
location
time
if
know
(equilibrium)
buffering
amplifying
capacity
(slope).
also
warn
about
methodological
biases
due
reference
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.