Hydrology and earth system sciences,
Journal Year:
2024,
Volume and Issue:
28(14), P. 3391 - 3433
Published: July 29, 2024
Abstract.
Hydro-pedotransfer
functions
(PTFs)
relate
easy-to-measure
and
readily
available
soil
information
to
hydraulic
properties
(SHPs)
for
applications
in
a
wide
range
of
process-based
empirical
models,
thereby
enabling
the
assessment
effects
on
hydrological,
biogeochemical,
ecological
processes.
At
least
more
than
4
decades
research
have
been
invested
derive
such
relationships.
However,
while
methods,
data
storage
capacity,
computational
efficiency
advanced,
there
are
fundamental
concerns
related
scope
adequacy
current
PTFs,
particularly
when
applied
parameterise
models
used
at
field
scale
beyond.
Most
PTF
development
process
has
focused
refining
advancing
regression
aspects
remained
largely
unconsidered.
systems
not
represented
which
built
mostly
agricultural
soils
temperate
climates.
Thus,
existing
PTFs
ignore
how
parent
material,
vegetation,
land
use,
climate
affect
processes
that
shape
SHPs.
The
Richards–Richardson
equation
limited
predicting
parameters
van
Genuchten–Mualem
functions,
despite
sufficient
evidence
demonstrating
their
shortcomings.
Another
issue
relates
diverging
scales
derivation
application,
whereby
derived
based
laboratory
measurements
often
being
regional
scales.
Scaling,
modulation,
constraining
strategies
exist
alleviate
some
these
shortcomings
mismatch
between
These
addressed
here
joint
effort
by
members
International
Soil
Modelling
Consortium
(ISMC)
Pedotransfer
Functions
Working
Group
with
aim
systematising
providing
roadmap
guiding
both
use.
We
close
10-point
catalogue
funders
researchers
guide
review
research.
Proceedings of the National Academy of Sciences,
Journal Year:
2020,
Volume and Issue:
117(34), P. 20438 - 20446
Published: Aug. 10, 2020
Significance
Over
many
millennia,
northern
peatlands
have
accumulated
large
amounts
of
carbon
and
nitrogen,
thus
cooling
the
global
climate.
shorter
timescales,
peatland
disturbances
can
trigger
losses
peat
release
greenhouses
gases.
Despite
their
importance
to
climate,
remain
poorly
mapped,
vulnerability
permafrost
warming
is
uncertain.
This
study
compiles
over
7,000
field
observations
present
a
data-driven
map
nitrogen
stocks.
We
use
these
maps
model
impact
thaw
on
find
that
will
likely
shift
greenhouse
gas
balance
peatlands.
At
present,
cool
but
anthropogenic
them
into
net
source
warming.
Remote Sensing of Environment,
Journal Year:
2019,
Volume and Issue:
237, P. 111557 - 111557
Published: Dec. 9, 2019
Models
of
atmospheric
composition
rely
on
fire
emissions
inventories
to
reconstruct
and
project
impacts
biomass
burning
air
quality,
public
health,
climate,
ecosystem
dynamics,
land-atmosphere
exchanges.
Many
such
global
use
satellite
measurements
active
fires
and/or
burned
area
from
the
Moderate
Resolution
Imaging
Spectroradiometer
(MODIS).
However,
differences
across
in
interpretation
imagery,
factors
assumed
for
different
components
smoke,
adjustments
made
small
obscured
can
result
large
regional
estimates
inventories.
Using
Google
Earth
Engine,
we
leverage
15
years
(2003–2017)
MODIS
observations
6
(2012–2017)
higher
spatial
resolution
Visible
Infrared
Radiometer
Suite
(VIIRS)
sensor
develop
metrics
quantify
five
major
sources
bias
or
uncertainty
inventories:
(1)
primary
reliance
versus
area,
(2)
cloud/haze
burden
ability
satellites
"see"
fires,
(3)
fragmentation
(4)
roughness
topography,
(5)
which
are
challenging
detect.
Based
all
these
uncertainties,
devise
comprehensive
"relative
confidence
scores,"
mapped
globally
at
0.25°
×
over
2003–2017.
We
then
focus
activity
Indonesia
as
a
case
study
analyze
how
choice
inventory
affects
model
smoke-induced
health
Equatorial
Asia.
adjoint
GEOS-Chem
chemical
transport
apply
particulate
organic
carbon
black
(OC
+
BC
smoke)
Global
Fire
Emissions
Database
(GFEDv4s),
Inventory
NCAR
(FINNv1.5),
Assimilation
System
(GFASv1.2),
Quick
Dataset
(QFEDv2.5r1),
Energetics
Research
(FEERv1.0-G1.2).
find
that
modeled
monthly
smoke
PM2.5
Singapore
2003
2016
correlates
with
observed
PM2.5,
r
ranging
0.64–0.84
depending
inventory.
during
season
(July
October)
high
intensity
(e.g.,
2006
2015),
magnitude
mean
Jul-Oct
differ
by
>20
μg
m−3
(>500%).
relative
metrics,
deduce
uncertainties
this
region
arise
primarily
small,
fragmented
landscape
very
poor
observing
conditions
due
clouds
thick
haze
time
year.
Indeed,
using
GFASv1.2,
adjusts
accounts
peatland
emissions,
is
most
consistent
Singapore,
well
Malaysia
Indonesia.
Finally,
an
online
app
called
FIRECAM
end-users
The
diagnoses
among
gauges
associated
satellite-observed
basis.
Global Change Biology,
Journal Year:
2019,
Volume and Issue:
26(3), P. 1638 - 1653
Published: Nov. 22, 2019
Abstract
Land‐use/land‐cover
change
(LULCC)
often
results
in
degradation
of
natural
wetlands
and
affects
the
dynamics
greenhouse
gases
(GHGs).
However,
magnitude
changes
GHG
emissions
from
undergoing
various
LULCC
types
remains
unclear.
We
conducted
a
global
meta‐analysis
with
database
209
sites
to
examine
effects
constructed
(CWs),
croplands
(CLs),
aquaculture
ponds
(APs),
drained
(DWs),
pastures
(PASs)
on
variability
CO
2
,
CH
4
N
O
coastal
wetlands,
riparian
peatlands.
Our
showed
that
were
net
sinks
atmospheric
sources
O,
exhibiting
capacity
mitigate
due
negative
comprehensive
warming
potentials
(GWPs;
−0.9
−8.7
t
‐eq
ha
−1
year
).
Relative
all
(except
CWs
wetlands)
decreased
uptake
by
69.7%−456.6%,
higher
increase
ecosystem
respiration
relative
slight
gross
primary
production.
The
APs
significantly
increased
compared
those
wetlands.
All
associated
emissions.
When
peatlands
converted
PASs,
increased.
CLs,
as
well
DWs
peatlands,
As
result,
PASs
led
remarkably
GWPs
65.4%−2,948.8%,
fluxes
was
mainly
sensitive
soil
water
content,
table,
salinity,
nitrogen
pH,
bulk
density.
This
study
highlights
significant
role
increasing
our
are
useful
for
improving
future
models
manipulative
experiments.