Geophysical Research Letters,
Journal Year:
2020,
Volume and Issue:
47(22)
Published: Nov. 3, 2020
Abstract
Quantifying
the
volume
of
water
that
is
stored
in
subsurface
critical
to
studies
availability
ecosystems,
slope
stability,
and
water‐rock
interactions.
In
a
variety
settings,
fractured
weathered
bedrock
as
rock
moisture.
However,
few
techniques
are
available
measure
moisture
unsaturated
rock,
making
direct
estimates
storage
dynamics
difficult
obtain.
Here,
we
use
borehole
nuclear
magnetic
resonance
(NMR)
at
two
sites
seasonally
dry
California
quantify
dynamic
storage.
We
show
strong
agreement
between
NMR
derived
from
neutron
logging
mass
balance
techniques.
The
depths
up
9
m
likely
reflect
depth
extent
root
uptake.
To
our
knowledge,
these
data
first
vadose
zone
via
NMR.
Nature Geoscience,
Journal Year:
2023,
Volume and Issue:
unknown
Published: Feb. 9, 2023
The
rooting-zone
water-storage
capacity-the
amount
of
water
accessible
to
plants-controls
the
sensitivity
land-atmosphere
exchange
and
carbon
during
dry
periods.
How
capacity
varies
spatially
is
largely
unknown
not
directly
observable.
Here
we
estimate
globally
from
relationship
between
remotely
sensed
vegetation
activity,
measured
by
combining
evapotranspiration,
sun-induced
fluorescence
radiation
estimates,
cumulative
deficit
calculated
daily
time
series
precipitation
evapotranspiration.
Our
findings
indicate
plant-available
stores
that
exceed
storage
2-m-deep
soils
across
37%
Earth's
vegetated
surface.
We
find
biome-level
variations
capacities
correlate
with
observed
depth
distributions
reflect
influence
hydroclimate,
as
magnitude
annual
water-deficit
extremes.
Smaller-scale
are
linked
topography
land
use.
document
large
spatial
in
effective
root-zone
illustrate
a
tight
link
among
climatology
deficits,
rooting
its
stress.
Earth s Future,
Journal Year:
2022,
Volume and Issue:
10(3)
Published: March 1, 2022
Abstract
Global
warming
intensifies
the
hydrological
cycle
by
altering
rate
of
water
fluxes
to
and
from
terrestrial
surface,
resulting
in
an
increase
extreme
precipitation
events
longer
dry
spells.
Prior
intensification
work
has
largely
focused
on
without
joint
consideration
evaporative
demand
changes
how
plants
respond
these
changes.
Informed
state‐of‐the‐art
climate
models,
we
examine
projected
its
role
complicating
resources
management
using
a
framework
that
accounts
for
surplus
demand.
Using
metric
combines
difference
between
daily
(surplus
events)
consecutive
days
when
exceeds
(deficit
time),
show
that,
globally,
will
become
larger
(+11.5%
+18.5%
moderate
high
emission
scenarios,
respectively)
duration
them
(+5.1%;
+9.6%)
end
century,
with
largest
northern
latitudes.
The
intra‐annual
occurrence
extremes
stress
existing
infrastructure
major
river
basins,
where
over
one
third
years
during
2070–2100
under
emissions
scenario
be
hydrologically
intense
(large
increases
intensity
deficit
tripling
historical
baseline.
Larger
are
found
basins
large
reservoir
capacity
(e.g.,
Amazon,
Congo,
Danube
River
Basins),
which
have
significant
populations,
irrigate
considerable
farmland,
support
threatened
endangered
aquatic
species.
Incorporating
flexibility
into
resource
paramount
continued
intensification.
New Phytologist,
Journal Year:
2024,
Volume and Issue:
242(5), P. 1891 - 1910
Published: April 22, 2024
Plant
water
uptake
from
the
soil
is
a
crucial
element
of
global
hydrological
cycle
and
essential
for
vegetation
drought
resilience.
Yet,
knowledge
how
distribution
depth
(WUD)
varies
across
species,
climates,
seasons
scarce
relative
to
our
aboveground
plant
functions.
With
literature
review,
we
found
that
average
WUD
varied
more
among
biomes
than
functional
types
(i.e.
deciduous/evergreen
broadleaves
conifers),
illustrating
importance
hydroclimate,
especially
precipitation
seasonality,
on
WUD.
By
combining
records
rooting
with
WUD,
observed
consistently
deeper
maximum
largest
differences
in
arid
regions
-
indicating
deep
taproots
act
as
lifelines
while
not
contributing
majority
uptake.
The
most
ubiquitous
observation
was
woody
plants
switch
sources
layers
highest
availability
within
short
timescales.
Hence,
seasonal
shifts
occur
globe
when
shallow
soils
are
drying
out,
allowing
continued
transpiration
hydraulic
safety.
While
there
still
significant
gaps
understanding
consistency
ecosystems
allows
integration
existing
into
next
generation
process
models.
Abstract
Catchments,
generally
understood
as
the
drainage
areas
of
low‐order
streams,
are
often
regarded
closed
hydrologic
entities;
that
is,
precipitation
(
P
)
minus
evapotranspiration
(ET)
over
a
catchment
equates
stream
outflow
Q
r
).
Here,
we
review
evidence
catchments
can
be
leaky
due
to
groundwater
or
inflow
across
topographic
divides,
based
on
mass
balance
continent
and
several
site‐based
studies
globe.
It
appears
is
more
likely
with
combination
following
factors:
small
size,
positioned
at
either
high
low
end
steep
regional
climatic
gradient,
underlain
by
deep
permeable
substrates
extend
beyond
study
catchment,
in
drier
climate
dry
seasons
droughts.
Catchment
leakage
has
hydrological,
geochemical,
ecological
implications.
Thus,
best
framed
semiclosed
units
perched
top
larger,
hydrogeological
system
no
real
boundaries
regarding
movement
water
solutes.
This
article
categorized
under:
Science
Water
>
Hydrological
Processes
Life
Nature
Freshwater
Ecosystems
New Phytologist,
Journal Year:
2020,
Volume and Issue:
226(3), P. 666 - 671
Published: Jan. 8, 2020
Summary
The
emergence
of
critical
zone
(CZ)
science
has
provided
an
integrative
platform
for
investigating
plant
ecophysiology
in
the
context
landscape
evolution,
weathering
and
hydrology.
CZ
lies
between
top
vegetation
canopy
fresh,
chemically
unaltered
bedrock
plays
a
pivotal
role
sustaining
life.
We
consider
what
perspective
recently
brought
to
study
ecophysiology.
specifically
highlight
novel
research
demonstrating
importance
deeper
subsurface
water
nutrient
relations.
also
point
knowledge
gaps
opportunities,
emphasising,
particular,
greater
focus
on
roles
deep,
nonsoil
resources
how
those
influence
coevolve
with
plants
as
frontier
ecophysiological
research.
Scientific Reports,
Journal Year:
2020,
Volume and Issue:
10(1)
Published: Oct. 28, 2020
Abstract
Climate
change
is
anticipated
to
increase
the
frequency
and
intensity
of
droughts,
with
major
impacts
ecosystems
globally.
Broad-scale
assessments
vegetation
responses
drought
are
needed
anticipate,
manage,
potentially
mitigate
climate-change
effects
on
ecosystems.
We
quantified
sensitivity
in
Pacific
Northwest,
USA,
as
percent
reduction
greenness
under
droughts
relative
baseline
moisture
conditions.
At
a
regional
scale,
shrub-steppe
ecosystems—with
drier
climates
lower
biomass—showed
greater
than
conifer
forests.
However,
variability
was
considerable
within
biomes
mediated
by
landscape
topography,
climate,
soil
characteristics.
Drought
generally
areas
higher
elevation,
bulk
density.
Ecosystems
high
included
dry
forests
along
ecotones
shrublands,
Rocky
Mountain
subalpine
forests,
cold
upland
sagebrush
communities.
In
valley
bottoms
low
density
available
water
capacity
showed
reduced
sensitivity,
suggesting
their
potential
refugia.
These
regional-scale
drought-sensitivity
patterns
discerned
from
remote
sensing
can
complement
plot-scale
studies
plant
physiological
help
inform
climate-adaptation
planning
conditions
intensify.
Global Change Biology,
Journal Year:
2022,
Volume and Issue:
28(11), P. 3489 - 3514
Published: March 22, 2022
Abstract
In
2020,
the
Australian
and
New
Zealand
flux
research
monitoring
network,
OzFlux,
celebrated
its
20
th
anniversary
by
reflecting
on
lessons
learned
through
two
decades
of
ecosystem
studies
global
change
biology.
OzFlux
is
a
network
not
only
for
researchers,
but
also
those
‘next
users’
knowledge,
information
data
that
such
networks
provide.
Here,
we
focus
eight
across
topics
climate
variability,
disturbance
resilience,
drought
heat
stress
synergies
with
remote
sensing
modelling.
distilling
key
learned,
identify
where
further
needed
to
fill
knowledge
gaps
improve
utility
relevance
outputs
from
OzFlux.
Extreme
variability
Australia
(droughts
flooding
rains)
provides
natural
laboratory
understanding
ecosystems
in
this
time
accelerating
change.
As
evidence
worsening
fire
risk
emerges,
ability
these
recover
disturbances,
as
cyclones,
adaptation
resilience
disturbance.
Drought
heatwaves
are
common
occurrences
large
parts
region
can
tip
an
ecosystem's
carbon
budget
net
CO
2
sink
source.
Despite
responses
stress,
at
sites
show
their
rapidly
pivoting
back
strong
upon
return
favourable
conditions.
Located
under‐represented
areas,
have
potential
reducing
uncertainties
products,
provide
several
opportunities
develop
new
theories
our
models.
The
accumulated
impacts
over
last
years
highlights
value
long‐term
observations
managed
systems.
A
future
vision
includes
ongoing
newly
developed
ecophysiologists,
ecologists,
geologists,
sensors
modellers.
Hydrology and earth system sciences,
Journal Year:
2022,
Volume and Issue:
26(6), P. 1527 - 1543
Published: March 22, 2022
Abstract.
In
a
warming
climate,
periods
with
lower
than
average
precipitation
will
increase
in
frequency
and
intensity.
During
such
periods,
known
as
meteorological
droughts,
the
decline
annual
runoff
may
be
proportionally
larger
corresponding
precipitation.
Reasons
behind
this
exacerbation
of
deficit
during
dry
remain
largely
unknown,
challenges
predictability
when
occur
future
how
intense
it
be.
work,
we
tested
hypothesis
that
droughts
is
common
feature
across
climates,
driven
by
evaporation
enhancement.
We
relied
on
multidecadal
records
streamflow
for
more
200
catchment
areas
various
European
which
distinctively
show
emergence
similar
exacerbated
identified
previous
studies,
i.e.
order
−20
%
to
−40
less
what
expected
from
deficits.
The
magnitude
two
three
times
basins
located
regions
wet
regions,
qualitatively
correlated
an
+11
+33
over
characterized
energy-limited
water-limited
regimes,
respectively.
Thus,
enhanced
atmospheric
vegetation
demand
moisture
induces
nonlinear
precipitation-runoff
relationship
low-flow
results
unexpectedly
large
decrease
already
low
water
availability.
Forecasting
onset,
magnitude,
duration
these
drops
have
paramount
societal
ecological
implications,
especially
given
their
supporting
role
safeguarding
water,
food,
energy.
outcome
are
prone
climates
regimes
makes
further
understanding
its
patterns
urgent
priority
water-resource
planning
management
drier
climate.