Abstract.
Peatland
restoration
and
rehabilitation
action
has
become
more
widely
acknowledged
as
a
necessary
response
to
mitigating
climate
change
risks
improving
global
carbon
storage.
ecosystems
require
timespans
on
the
order
of
decades
thus
cannot
be
dependent
upon
shorter-term
monitoring
often
carried
out
in
research
projects.
Hydrological
assessments
using
geospatial
tools
provide
basis
for
planning
works
well
analysing
associated
environmental
influences.
“Restoration”
encompasses
applications
pre-
post-restoration
scenarios
both
bogs
fens,
across
range
impact
fields.
The
aim
this
scoping
review
is
identify,
describe,
categorise
current
process-based
modelling
uses
peatlands
investigate
applicability
appropriateness
eco-
and/or
hydrological
models
northern
peatland
restoration.
Two
literature
searches
were
conducted
Web
Science
entire
database
September
2022
August
2023.
Of
final
211
papers
included
review,
their
categorised
according
review’s
interests
7
distinct
categories
aggregating
papers’
themes
model
outputs.
Restoration
site
context
was
added
by
identifying
234
unique
study
locations
from
full
which
catalogued
analysed
against
raster
data
Köppen-Geiger
classification
scheme.
A
majority
sites
temperate
oceanic
zones
or
humid
continental
experiencing
snow.
Over
one
five
unnamed
likely
single-use.
top
three
most-used
these
models,
based
frequency
use
locations,
LPJ,
ecosys,
DigiBog,
that
order.
Key
emerging
topics
covered
included:
development
bog
growth
perspective;
prioritisation
GHG
emissions
dynamics
part
policymaking;
importance
spatial
connectivity
within
alongside
represent
heterogeneous
systems;
prevalence
remote
sensing
machine
learning
techniques
predict
progress
with
little
physical
intervention.
This
provides
valuable
application
ecohydrological
determining
strategies
evaluating
post-intervention
over
time.
International Journal of Remote Sensing,
Journal Year:
2024,
Volume and Issue:
45(18), P. 6372 - 6394
Published: Aug. 30, 2024
Peatlands
play
a
pivotal
role
in
global
carbon
cycling
and
the
conservation
of
biodiversity
even
though
they
cover
small
fraction
Earth's
terrestrial
surface.
These
ecosystems
are,
however,
increasingly
vulnerable
due
to
climate
change
impacts
anthropogenic
activities,
leading
significant
degradation
many
areas.
This
review
compiles
analyses
various
studies
that
employ
remote
sensing
for
comprehensive
peatland
mapping
monitoring.
Remote
offers
detailed
insights
into
critical
features,
including
classification
vegetation,
assessment
water
table
dynamics,
vegetation
condition
diversity
estimation
stocks.
Furthermore,
delineates
utility
monitoring
recovery
processes
restored
peatlands,
highlighting
scarcity
long-term
studies.
It
also
emphasizes
potential
integrating
hyperspectral,
multispectral
SAR
data
as
well
cross-scale
analyses.
Concluding
with
future
directions,
underscores
necessity
enhanced
upscaling
techniques,
integration
multi-sensor
application
modelling
enrich
our
understanding
management
ecosystems.
Land,
Journal Year:
2024,
Volume and Issue:
13(5), P. 581 - 581
Published: April 27, 2024
Draining
peatlands
to
create
agricultural
land
has
been
the
norm
in
Europe,
but
context
of
climate
change
and
loss
biodiversity,
these
rich
ecosystems
may
reactivate
their
functions
as
greenhouse
gas
sinks
retreat
spaces
for
animals
plants.
Against
this
background,
National
Moor
Rewetting
Strategy
was
put
into
effect
Germany
2023,
together
with
Natural
Climate
Protection
Action
Plan.
This
article
examines
methodology
peatland
rewetting
from
scientific,
administrative,
social,
technical
perspectives.
The
focuses
on
an
example
moor
central
Germany:
Rathsbruch
near
municipality
Zerbst,
Saxony-Anhalt.
To
illustrate
importance
projects
degraded
peatlands,
five
scenarios
different
target
soil
water
levels
were
considered,
associated
emissions
calculated
a
period
years.
For
planning
solution,
estimate
medium-to-long-term
development
habitat
types
made
based
current
use
dynamics
typical
habitat.
results
area
showed
that
increasing
level
steps
1,
0.8,
or
0.5
m
no
significant
influence
reducing
CO2
situation,
while
depth
0.3
slight
influence.
When
raised
0.1
below
surface
(Scenario
5),
reduction
observed.
avoided
costs
due
environmental
damage
show
benefits
multiply
every
decimeter
increase.
rising
groundwater
extensification
favor
establishment
local
biotopes.
means
two
biggest
man-made
problems
(extinction
species
change)
can
be
reduced.
Therefore,
research
is
applicable
recultivation
work
at
municipal
regional
beyond
within
framework
EU
restoration
policy.
Biogeosciences,
Journal Year:
2024,
Volume and Issue:
21(13), P. 3143 - 3163
Published: July 9, 2024
Abstract.
Peatland
restoration
and
rehabilitation
action
has
become
more
widely
acknowledged
as
a
necessary
response
to
mitigating
climate
change
risks
improving
global
carbon
storage.
ecosystems
require
time
spans
of
the
order
decades
and,
thus,
cannot
be
dependent
upon
shorter-term
monitoring
often
carried
out
in
research
projects.
Hydrological
assessments
using
geospatial
tools
provide
basis
for
planning
works
well
analysing
associated
environmental
influences.
“Restoration”
encompasses
applications
pre-restoration
post-restoration
scenarios
both
bogs
fens,
across
range
impact
fields.
The
aim
this
scoping
review
is
identify,
describe,
categorize
current
process-based
modelling
uses
peatlands
investigate
applicability
appropriateness
ecohydrological
and/or
hydrological
models
northern
peatland
restoration.
Two
literature
searches
were
conducted
entire
Web
Science
database
September
2022
August
2023.
Of
final
211
papers
included
review,
their
categorized
according
review's
interests
seven
distinct
categories
aggregating
papers'
themes
model
outputs.
Restoration
site
context
was
added
by
identifying
229
unique
study
locations
from
full
database,
which
catalogued
analysed
against
raster
data
Köppen–Geiger
classification
scheme.
A
majority
sites
temperate
oceanic
zones
or
humid
continental
that
experienced
snow.
Over
one
five
unnamed
likely
intended
single
use.
Key
emerging
topics
covered
following:
development
bog
growth
perspective,
prioritization
greenhouse
gas
(GHG)
emissions
dynamics
part
policymaking,
importance
spatial
connectivity
within
alongside
represent
heterogeneous
systems,
increased
prevalence
remote
sensing
machine
learning
techniques
predict
progress
with
little
physical
intervention.
Models
are
presented
application
broader
ecosystem
organized
most
least
complex.
This
provides
valuable
determining
strategies
evaluating
post-intervention
over
time.
European Journal of Soil Science,
Journal Year:
2024,
Volume and Issue:
75(4)
Published: July 1, 2024
Abstract
Peat
makes
up
approximately
a
quarter
of
Scotland's
soil
by
area.
Healthy,
undisturbed,
peatland
habitats
are
critical
to
providing
resilient
biodiversity
and
habitat
support,
water
management,
carbon
sequestration.
A
high
stable
table
is
prerequisite
maintain
sink
function;
any
drainage
turns
this
major
terrestrial
store
into
source
that
feeds
back
further
global
climate
change.
Drainage
erosion
features
crucial
indicators
condition
key
for
estimating
national
greenhouse
gas
emissions.
Previous
work
on
mapping
peat
depth
in
Scotland
has
provided
maps
with
reasonable
accuracy
at
100‐m
resolution,
allowing
land
managers
policymakers
both
plan
manage
these
soils
towards
identifying
priority
sites
restoration.
However,
the
spatial
variability
surface
much
finer
than
scale,
limiting
ability
inventory
emissions
or
develop
site‐specific
restoration
management
plans.
This
involves
an
updated
set
using
high‐resolution
(25
cm)
aerial
imagery,
which
provides
identify
segment
individual
channels
features.
Combining
imagery
classical
deep
learning‐based
segmentation
model
enables
scale
be
carried
out
deeper
understanding
resource
will
enable
various
future
analyses
data.
Restoration Ecology,
Journal Year:
2024,
Volume and Issue:
unknown
Published: Nov. 7, 2024
Remote
sensing
(RS)
can
be
an
efficient
monitoring
method
to
assess
the
ecological
impacts
of
restoration.
Yet,
it
has
been
used
relatively
little
monitor
post‐restoration
changes
in
boreal
forestry‐drained
peatlands,
and
particularly
linkages
between
RS
plant
species
remain
vague.
To
understand
this
gap,
we
utilize
data
from
Finnish
peatland
restoration
network
spanning
150
sites
a
10‐year
period.
We
employ
Bayesian
joint
distribution
models
(Hierarchical
Modeling
Species
Communities)
study
(1)
optical
Sentinel‐2
Landsat
satellite
spectral
signatures,
(2)
whether
variables
improve
predictions
vascular
moss
functional
type
occurrence
cover,
(3)
what
kinds
associations
exist
or
types.
Our
results
show
that
increases
reflectance
red
near‐infrared
(NIR)
bands
sparsely
treed
pine
mire
forests
open
mires
but
not
densely
spruce
forests.
Impacts
on
other
tested
consisting
moisture
greenness
indices
are
less
clear.
Additionally,
increase
species‐
type‐specific
predictive
power
only
modestly,
there
few
clear
links
functional‐type
cover.
suggest
NIR
as
satellite‐based
indicators
for
success
further
studies
required
develop
usable
methods
detecting
species‐specific
with
RS.
The Science of The Total Environment,
Journal Year:
2024,
Volume and Issue:
957, P. 177697 - 177697
Published: Nov. 26, 2024
Restoration
can
initiate
a
succession
of
plant
communities
towards
those
pristine
peatlands.
Field
inventory-based
vegetation
monitoring
is
labour-intensive
and
not
feasible
for
every
restored
site.
While
remote
sensing
has
been
used
to
monitor
hydrological
changes
in
peatlands,
it
less
post-restoration
composition.
We
utilised
inventories
from
Finnish
peatland
network
containing
10-year
before-after-control-impact
data
150
sites,
representing
three
types
(spruce
mire
forests,
pine
open
mires),
optical
observations
Landsat
5-9
Sentinel-2
satellites.
employed
non-metric
multidimensional
scaling
(NMDS)
produce
floristic
gradients,
wetness
productivity,
the
data.
constructed
random
forest
regression
models
with
NMDS
dimensions,
i.e.
as
response
variables
satellite
imagery
predictors.
Our
results
show
that
gradients
different
should
be
monitored
variables.
However,
midsummer
NIR
red
band
consistently
explain
variation
all
types.
indicate
them
modelled
reasonable
accuracy
mires
sparsely
treed
forests
but
densely
spruce
forests.
suggest
serve
proxy
assessing
peatlands
little
or
no
trees.