Nature Communications,
Год журнала:
2024,
Номер
15(1)
Опубликована: Янв. 23, 2024
Abstract
Temperature
is
a
fundamental
driver
of
species
distribution
and
ecosystem
functioning.
Yet,
our
knowledge
the
microclimatic
conditions
experienced
by
organisms
inside
tropical
forests
remains
limited.
This
because
ecological
studies
often
rely
on
coarse-gridded
temperature
estimates
representing
at
2
m
height
in
an
open-air
environment
(i.e.,
macroclimate).
In
this
study,
we
present
high-resolution
pantropical
estimate
near-ground
(15
cm
above
surface)
temperatures
forests.
We
quantify
diurnal
seasonal
variability,
thus
revealing
both
spatial
temporal
microclimate
patterns.
find
that
average,
understory
are
1.6
°C
cooler
than
temperatures.
The
range
average
1.7
lower
forests,
comparison
to
conditions.
More
importantly,
demonstrate
substantial
variability
characteristics
regulated
combination
large-scale
climate
conditions,
vegetation
structure
topography,
hence
could
not
be
captured
existing
macroclimate
grids.
Our
results
contribute
quantifying
actual
thermal
ranges
provide
new
insights
into
how
these
limits
may
affected
change
disturbances.
Global Change Biology,
Год журнала:
2021,
Номер
27(11), С. 2279 - 2297
Опубликована: Март 16, 2021
Abstract
Forest
microclimates
contrast
strongly
with
the
climate
outside
forests.
To
fully
understand
and
better
predict
how
forests'
biodiversity
functions
relate
to
change,
need
be
integrated
into
ecological
research.
Despite
potentially
broad
impact
of
on
response
forest
ecosystems
global
our
understanding
within
below
tree
canopies
modulate
biotic
responses
change
at
species,
community
ecosystem
level
is
still
limited.
Here,
we
review
spatial
temporal
variation
in
result
from
an
interplay
features,
local
water
balance,
topography
landscape
composition.
We
first
stress
exemplify
importance
considering
across
landscapes.
Next,
explain
macroclimate
warming
(of
free
atmosphere)
can
affect
microclimates,
vice
versa,
via
interactions
land‐use
changes
different
biomes.
Finally,
perform
a
priority
ranking
future
research
avenues
interface
microclimate
ecology
biology,
specific
focus
three
key
themes:
(1)
disentangling
abiotic
drivers
feedbacks
microclimates;
(2)
regional
mapping
predictions
(3)
impacts
functioning
face
change.
The
availability
microclimatic
data
will
significantly
increase
coming
decades,
characterizing
variability
unprecedented
scales
relevant
biological
processes
This
revolutionize
dynamics,
implications
functions,
changes.
In
order
support
sustainable
use
forests
secure
their
services
for
generations,
cannot
ignored.
Global Change Biology,
Год журнала:
2021,
Номер
28(9), С. 3110 - 3144
Опубликована: Дек. 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 Ecology and Biogeography,
Год журнала:
2021,
Номер
30(4), С. 768 - 783
Опубликована: Фев. 15, 2021
Abstract
Motivation
More
than
half
of
Earth's
species
are
contained
in
a
mere
1.4%
its
land
area,
but
the
climates
many
these
biodiversity
hotspots
projected
to
disappear
as
consequence
anthropogenic
climate
change.
There
is
growing
recognition
that
spatio‐temporal
patterns
have
shaped
biological
diversity
over
variety
historical
time‐scales,
yet
rarely
taken
into
account
assessments
vulnerability
future
In
our
review,
we
synthesize
climatic
processes
led
diversification
and
interpret
what
this
means
context
We
demonstrate
importance
mesoclimatic
fine‐scale
topographical
heterogeneity,
combination
with
variability,
driving
speciation
maintaining
high
levels
diversity.
outline
why
features
crucial
understanding
impacts
change
discuss
how
recent
advances
predictive
modelling
enable
be
understood
better.
Location
Global.
Main
conclusions
contend
many,
although
not
all,
landscape
characteristics
create
spatial
variability
climate,
which
potentially
buffers
them
from
changes.
Temporally,
also
experienced
stable
through
evolutionary
time,
making
particularly
vulnerable
Others
more
variable
climates,
likely
provide
resilience
Thus,
order
identify
risk
for
global
biodiversity,
need
consider
carefully
influence
climate.
However,
most
still
reliant
on
data
coarse
temporal
resolution.
Higher‐resolution
forecasts
better
physiological
responses
organisms
much
needed
inform
conservation
strategies.
Global Change Biology,
Год журнала:
2021,
Номер
27(23), С. 6307 - 6319
Опубликована: Окт. 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,
Год журнала:
2022,
Номер
29(6), С. 1451 - 1470
Опубликована: Дек. 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,
Год журнала:
2024,
Номер
33(6)
Опубликована: Апрель 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.
Earth-Science Reviews,
Год журнала:
2020,
Номер
211, С. 103419 - 103419
Опубликована: Окт. 29, 2020
Effective
thermal
conductivity
of
soils
(λeff)
is
a
critical
parameter
for
agriculture,
environment
science,
and
engineering.
Functions
to
estimate
λeff
from
readily
available
soil
properties,
known
as
(STC)
schemes,
are
needed
by
land-surface
models
(LSMs),
hydrological
models,
soil-vegetation-atmosphere
transfer
(SVAT)
study
the
land
surface
energy
balance,
heat
flux,
regime
under
various
climates
geographic
regions.
The
selection
STC
scheme
can
result
in
large
differences
temperature
estimates
LSMs,
sometimes
masking
effects
climate
change.
Therefore,
accurate
critically
important
LSM
estimates.
Although
number
schemes
have
been
incorporated
no
has
systematically
evaluated
their
performance.
objectives
this
were
review
evaluate
employed
LSMs
comparing
(1)
predicted
measured
STCs
(2)
modelled
(LST)
using
Community
Land
Model
at
three
selected
sites
corresponding
LST
data
moderate
resolution
imaging
spectrometer
(MODIS).
In
total,
24
collated
38
mainstream
SVAT,
models.
They
divided
into
categories
based
on
model
types:
one
physically-based
scheme,
eight
linear/non-linear
regression
13
normalized
schemes.
We
also
include
two
that
express
function
matric
potential
(ψ,
hereafter
referred
(ψ)
schemes).
first
types
with
compiled
dataset
consisting
439
unfrozen
frozen
measurements
16
soils.
simultaneously
separate
or
independent
studies.
Results
showed
none
could
be
used
accurately
predict
all
types.
performance
largely
depended
size
(number
samples)
characteristics
(e.g.,
types)
comparison.
Some
work
well
certain
soils,
but
care
should
taken
larger
scale
applications.
simulated
varied
when
compared
MODIS
LST.
general,
performed
better
medium-
coarse-textured
than
fine-textured
However,
discrepancies
observed
estimated
different
medium
recommend
modelers
mindful
inherent
bias
hence
overall
predictions.
Orchestrated
efforts
urgently
part
hydrology,
climatology
communities
develop
more
extensive
systematic
database
development
evaluation
improved
wider
Journal of Biogeography,
Год журнала:
2022,
Номер
49(8), С. 1420 - 1442
Опубликована: Июнь 3, 2022
Climate
change
is
expected
to
impact
mountain
biodiversity
by
shifting
species
ranges
and
the
biomes
they
shape.
The
extent
regional
variation
in
these
impacts
are
still
poorly
understood,
particularly
highly
biodiverse
Andes.
Regional
syntheses
of
climate
on
vegetation
pivotal
identify
guide
research
priorities.
Here
we
review
current
data,
knowledge
uncertainties
past,
present
future