Agricultural and Forest Meteorology,
Год журнала:
2021,
Номер
306, С. 108435 - 108435
Опубликована: Апрель 29, 2021
The
land
surface
models
that
provide
fluxes
of
energy
and
mass
to
the
atmosphere
in
weather
forecast
climate
typically
represent
plant
canopies
as
a
homogenous
single
layer
phytomass
without
vertical
structure
(commonly
referred
big
leaf).
This
modeling
paradigm
harkens
back
30–40-year-old
debate
about
whether
big-leaf
adequately
simulate
for
vegetated
surfaces
compared
more
complex
computationally
costly
multilayer
canopy
models.
article
revisits
scientific
debate.
We
review
early
literature
place
our
findings
context
discuss
recent
advancements
roughness
sublayer
theory,
observations
leaf
traits,
computational
methods
facilitate
use
Using
model
with
variable
resolution,
we
compare
representation
equivalent
one-layer
ask
how
well
replicates
benchmark
identify
why
differences
occur.
Comparisons
flux
tower
measurements
at
several
forest
sites
spanning
multiple
years
show
sensible
heat
flux,
latent
gross
primary
production,
friction
velocity
degrade
comparison
canopy.
For
considered,
5–10
layers
sufficiently
reproduce
observed
fluxes.
Vertical
variation
within-canopy
air
temperature,
specific
humidity,
wind
speed
alters
profile
water
potential,
which
upper
is
water-stressed
on
dry
soils,
also
causes
between
canopies.
suggest
community
should
revisit
parameterizations
used
Journal of Advances in Modeling Earth Systems,
Год журнала:
2020,
Номер
12(2)
Опубликована: Янв. 17, 2020
An
overview
of
the
Community
Earth
System
Model
Version
2
(CESM2)
is
provided,
including
a
discussion
challenges
encountered
during
its
development
and
how
they
were
addressed.
In
addition,
an
evaluation
pair
CESM2
long
preindustrial
control
historical
ensemble
simulations
presented.
These
performed
using
nominal
1°
horizontal
resolution
configuration
coupled
model
with
both
"low-top"
(40
km,
limited
chemistry)
"high-top"
(130
comprehensive
versions
atmospheric
component.
contains
many
substantial
science
infrastructure
improvements
new
capabilities
since
previous
major
release,
CESM1,
resulting
in
improved
comparison
to
CESM1
available
observations.
include
reductions
low-latitude
precipitation
shortwave
cloud
forcing
biases;
better
representation
Madden-Julian
Oscillation;
El
Niño-Southern
Oscillation-related
teleconnections;
global
land
carbon
accumulation
trend
that
agrees
well
observationally
based
estimates.
Most
tropospheric
surface
features
low-
high-top
are
very
similar
each
other,
so
these
present
configurations.
has
equilibrium
climate
sensitivity
5.1–5.3
°C,
larger
than
primarily
due
combination
relatively
small
changes
microphysics
boundary
layer
parameters.
contrast,
CESM2's
transient
response
1.9–2.0
°C
comparable
CESM1.
The
outputs
from
other
research
community,
represent
contributions
Coupled
Intercomparison
Project
Phase
6.
Journal of Advances in Modeling Earth Systems,
Год журнала:
2019,
Номер
11(12), С. 4245 - 4287
Опубликована: Окт. 19, 2019
The
Community
Land
Model
(CLM)
is
the
land
component
of
Earth
System
(CESM)
and
used
in
several
global
regional
modeling
systems.
In
this
paper,
we
introduce
model
developments
included
CLM
version
5
(CLM5),
which
default
for
CESM2.
We
assess
an
ensemble
simulations,
including
prescribed
prognostic
vegetation
state,
multiple
forcing
data
sets,
CLM4,
CLM4.5,
CLM5,
against
a
range
metrics
from
International
Benchmarking
(ILAMBv2)
package.
CLM5
includes
new
updated
processes
parameterizations:
(1)
dynamic
units,
(2)
parameterizations
structure
hydrology
snow
(spatially
explicit
soil
depth,
dry
surface
layer,
revised
groundwater
scheme,
canopy
interception
processes,
fresh
density,
simple
firn
model,
Scale
Adaptive
River
Transport),
(3)
plant
hydraulics
hydraulic
redistribution,
(4)
nitrogen
cycling
(flexible
leaf
stoichiometry,
N
optimization
photosynthesis,
carbon
costs
uptake),
(5)
crop
with
six
types
time-evolving
irrigated
areas
fertilization
rates,
(6)
urban
building
energy,
(7)
isotopes,
(8)
stomatal
physiology.
New
optional
features
include
demographically
structured
(Functionally
Assembled
Terrestrial
Ecosystem
Simulator),
ozone
damage
to
plants,
fire
trace
gas
emissions
coupling
atmosphere.
Conclusive
establishment
improvement
or
degradation
individual
variables
challenged
by
uncertainty,
parametric
structural
complexity,
but
multivariate
presented
here
suggest
general
broad
CLM4
CLM5.
New Phytologist,
Год журнала:
2020,
Номер
226(6), С. 1550 - 1566
Опубликована: Фев. 17, 2020
Summary
Recent
decades
have
been
characterized
by
increasing
temperatures
worldwide,
resulting
in
an
exponential
climb
vapor
pressure
deficit
(VPD).
VPD
has
identified
as
increasingly
important
driver
of
plant
functioning
terrestrial
biomes
and
established
a
major
contributor
recent
drought‐induced
mortality
independent
other
drivers
associated
with
climate
change.
Despite
this,
few
studies
isolated
the
physiological
response
to
high
VPD,
thus
limiting
our
understanding
ability
predict
future
impacts
on
ecosystems.
An
abundance
evidence
suggests
that
stomatal
conductance
declines
under
transpiration
increases
most
species
up
until
given
threshold,
leading
cascade
subsequent
including
reduced
photosynthesis
growth,
higher
risks
carbon
starvation
hydraulic
failure
.
Incorporation
photosynthetic
traits
‘next‐generation’
land‐surface
models
greatest
potential
for
improved
prediction
responses
at
plant‐
global‐scale,
will
yield
more
mechanistic
simulations
changing
climate.
By
providing
fully
integrated
framework
evaluation
function,
improvements
forecasting
long‐term
projections
can
be
made.
Forest
dynamics
arise
from
the
interplay
of
environmental
drivers
and
disturbances
with
demographic
processes
recruitment,
growth,
mortality,
subsequently
driving
biomass
species
composition.
However,
forest
subsequent
recovery
are
shifting
global
changes
in
climate
land
use,
altering
these
dynamics.
Changes
drivers,
disturbance
regimes
forcing
forests
toward
younger,
shorter
stands.
Rising
carbon
dioxide,
acclimation,
adaptation,
migration
can
influence
impacts.
Recent
developments
Earth
system
models
support
increasingly
realistic
simulations
vegetation
In
parallel,
emerging
remote
sensing
datasets
promise
qualitatively
new
more
abundant
data
on
underlying
consequences
for
structure.
When
combined,
advances
hold
improving
scientific
understanding
demographics
disturbances.
Risks
to
mitigation
potential
of
forests
Much
recent
attention
has
focused
on
the
trees
and
mitigate
ongoing
climate
change
by
acting
as
sinks
for
carbon.
Anderegg
et
al.
review
growing
evidence
that
forests'
is
increasingly
at
risk
from
a
range
adversities
limit
forest
growth
health.
These
include
physical
factors
such
drought
fire
biotic
factors,
including
depredations
insect
herbivores
fungal
pathogens.
Full
assessment
quantification
these
risks,
which
themselves
are
influenced
climate,
key
achieving
science-based
policy
outcomes
effective
land
management.
Science
,
this
issue
p.
eaaz7005
Journal of Advances in Modeling Earth Systems,
Год журнала:
2020,
Номер
12(4)
Опубликована: Март 11, 2020
Abstract
Land
surface
models
(LSMs)
are
a
vital
tool
for
understanding,
projecting,
and
predicting
the
dynamics
of
land
its
role
within
Earth
system,
under
global
change.
Driven
by
need
to
address
set
key
questions,
LSMs
have
grown
in
complexity
from
simplified
representations
biophysics
encompass
broad
interrelated
processes
spanning
disciplines
biophysics,
biogeochemistry,
hydrology,
ecosystem
ecology,
community
human
management,
societal
impacts.
This
vast
scope
complexity,
while
warranted
problems
designed
solve,
has
led
enormous
challenges
understanding
attributing
differences
between
LSM
predictions.
Meanwhile,
wide
range
spatial
scales
that
govern
heterogeneity,
spectrum
timescales
dynamics,
create
tractably
representing
LSMs.
We
identify
three
“grand
challenges”
development
use
LSMs,
based
around
these
issues:
managing
process
parametric
across
asked
changing
world.
In
this
review,
we
discuss
progress
been
made,
as
well
promising
directions
forward,
each
challenges.
Nature,
Год журнала:
2021,
Номер
592(7852), С. 65 - 69
Опубликована: Март 31, 2021
Abstract
Year-to-year
changes
in
carbon
uptake
by
terrestrial
ecosystems
have
an
essential
role
determining
atmospheric
dioxide
concentrations
1
.
It
remains
uncertain
to
what
extent
temperature
and
water
availability
can
explain
these
variations
at
the
global
scale
2–5
Here
we
use
factorial
climate
model
simulations
6
show
that
variability
soil
moisture
drives
90
per
cent
of
inter-annual
land
uptake,
mainly
through
its
impact
on
photosynthesis.
We
find
most
this
ecosystem
response
occurs
indirectly
as
moisture–atmosphere
feedback
amplifies
humidity
anomalies
enhances
direct
effects
stress.
The
strength
mechanism
explains
why
coupled
models
indicate
has
a
dominant
4
,
which
is
not
readily
apparent
from
surface
observational
analyses
2,5
These
findings
highlight
need
account
for
between
dryness
when
estimating
cycle
climatic
change
globally
5,7
well
conducting
field-scale
investigations
droughts
8,9
Our
results
modelled
driven
vapour
pressure
deficit
are
controlled
moisture.
Annual Review of Plant Biology,
Год журнала:
2022,
Номер
73(1), С. 673 - 702
Опубликована: Март 1, 2022
Recent
observations
of
elevated
tree
mortality
following
climate
extremes,
like
heat
and
drought,
raise
concerns
about
change
risks
to
global
forest
health.
We
currently
lack
both
sufficient
data
understanding
identify
whether
these
represent
a
trend
toward
increasing
mortality.
Here,
we
document
events
sudden
unexpected
drought
in
ecosystems
that
previously
were
considered
tolerant
or
not
at
risk
exposure.
These
underscore
the
fact
may
affect
forests
with
force
future.
use
as
examples
highlight
current
difficulties
challenges
for
realistically
predicting
such
uncertainties
future
condition.
Advances
remote
sensing
technology
greater
availably
high-resolution
data,
from
field
assessments
satellites,
are
needed
improve
prediction
responses
change.
Expected
final
online
publication
date
Annual
Review
Plant
Biology,
Volume
73
is
May
2022.
Please
see
http://www.annualreviews.org/page/journal/pubdates
revised
estimates.
Ecology Letters,
Год журнала:
2020,
Номер
23(5), С. 891 - 901
Опубликована: Март 10, 2020
Multi-year
lags
in
tree
drought
recovery,
termed
'drought
legacy
effects',
are
important
for
understanding
the
impacts
of
on
forest
ecosystems,
including
carbon
(C)
cycle
feedbacks
to
climate
change.
Despite
ubiquity
large
uncertainties
remain
regarding
mechanistic
basis
effects
and
their
importance
C
cycle.
In
this
review,
we
identify
approaches
used
study
effects,
from
rings
whole
forests.
We
then
discuss
key
knowledge
gaps
pertaining
causes
how
various
mechanisms
that
may
contribute
these
recovery
could
have
contrasting
implications
Furthermore,
conduct
a
novel
data
synthesis
find
differ
drastically
both
size
length
across
US
depending
if
they
identified
versus
gross
primary
productivity.
Finally,
highlight
promising
future
research
improve
our
capacity
model
predict
impact
health.
emphasise
holistic
view
-
tissues
forests
will
advance
stimulate
efforts
investigate
via
experimental,
observational
modelling
approaches.