The geolocation of features on information surfaces and the use of the open and FAIR data principles in the mountain landscape domain and geoheritage
Permafrost and Periglacial Processes,
Journal Year:
2024,
Volume and Issue:
35(2), P. 98 - 108
Published: Jan. 25, 2024
Abstract
This
note
suggests
that
decimal
latitude/longitude
[dLL]
locations
should
be
used
to
identify
features
of
interest,
landforms,
sample
and
investigations
sites,
in
an
‘information
landscape’
provided
by
the
geomorphological
literature.
All
information
associated
with
a
labelled,
or
tagged,
geolocation
available
for
examination
as
part
landscapes
can
explored
represented
books,
papers
other
publications.
also
outlines
‘open’
FAIR
data
are
findable,
accessible,
interoperable
reusable
how
principles
better
explain
landscapes,
especially
mountain
landscape
domain.
Tors
rock
glaciers
illustrate
sites
inform
fieldwork
literature
searching.
Any
[dLL]‐specified
location
is
identifying
label,
names
given
landforms
toponyms.
Two
letters
(digraph)
landform
labels:
TO
tors
RG
glaciers.
Citations,
(author–date–title–source)
attributions,
labels.
The
shows
these
attributions
linked
geolocations
specifying
time
space
addition
will
facilitate
future
searches
modelling
explore
‘unknowns’
landscape,
this
paper
ways
which
achieved,
including
geoheritage
geotourism.
Language: Английский
Enhancing the Digital Earth via Digital Decimal Geolocation and the FAIR Data Principles
Earth Science Systems and Society,
Journal Year:
2024,
Volume and Issue:
4
Published: May 2, 2024
The
essential
aspects
of
Gore’s
“Digital
Earth”
concept
include
“georeferenced”
data.
This
paper
is
concerned
with
establishing
the
need
for
a
standardised
and
common
form
to
locate
points
on
earth’s
surface.
Rather
than
degree,
minute,
second
(dms)
system
latitude/longitude
location,
decimal
degree
system,
formatted
as
comma
separated
variable
tuple
in
square
brackets,
[dLL],
advocated.
Values,
an
appropriate
number
places,
can
be
inserted
text
computer
searchable.
[dLL]
also
becomes
metadata
data
set
or
index
databases
identifiers
images.
Various
uses
this
are
illustrated.
allows
become
more
“open”
via
FAIR
principles:
findability,
accessibility,
interoperability,
reusability.
Wider
use
earth
sciences
fundamental
collaboration
other
disciplines,
especially
Critical
Zone
Science.
general
geolocation
exploited
wide
variety
analytical
methodologies,
some
which
outlined,
science
environmental
situations.
Language: Английский
Remote Sensing and Landsystems in the Mountain Domain: FAIR Data Accessibility and Landform Identification in the Digital Earth
Remote Sensing,
Journal Year:
2024,
Volume and Issue:
16(17), P. 3348 - 3348
Published: Sept. 9, 2024
Satellite
imagery
has
become
a
major
source
for
identifying
and
mapping
terrestrial
planetary
landforms.
However,
interpretating
landforms
their
significance,
especially
in
changing
environments,
may
still
be
questionable.
Consequently,
ground
truth
to
check
training
models,
mountainous
areas,
can
problematic.
This
paper
outlines
decimal
format,
[dLL],
latitude
longitude
geolocation
that
used
model
interpretation
validation
data
sets.
As
have
positions
space
time,
[dLL]
defined
points,
as
images,
associated
with
metadata
nodes.
Together
vertices,
nodes
help
build
‘information
surfaces’
part
of
the
Digital
Earth.
examines
aspects
Critical
Zone
integration
via
FAIR
principles,
are;
findable,
accessible,
interoperable
re-usable.
Mapping
making
inventories
rock
glacier
are
examined
context
geomorphic
environmental
significance
need
geolocated
truth.
Terrestrial
examination
glaciers
shows
them
predominantly
glacier-derived
not
indicators
permafrost.
Remote-sensing
technologies
track
developing
surface
features
show
climatically
melting
beneath
debris
covers.
Distinguishing
between
glaciers,
debris-covered
over
time
is
challenge
new
remote
sensing
satellites
necessity
common
format
report
many
Earth
features.
Language: Английский
Glacier–rock glacier interactions in the eastern Hindu Kush, Nuristan, Afghanistan [35.92,71.13] in the period 1976–2019
Geografiska Annaler Series A Physical Geography,
Journal Year:
2023,
Volume and Issue:
105(2-3), P. 91 - 120
Published: July 3, 2023
Landsystem
relationships
between
glaciers
and
rock
debris
supply
in
a
mountain
landscape
domain,
(),
are
described.
Decimal
latitude-longitude
[dLL]
geolocations
used
to
identify
features
transects
an
information
landscape.
Geo-located
coded,
enabling
1976
expedition
2019
Google
Earth
imagery
be
compared.
Rock
is
progressively
added
1-3
km
long
which
become
debris-covered.
Cirque
eventually
assume
glacier
(RG)
forms
when
supraglacial
loads
high.
Some
snouts
reach
main
valley
floors
still
advance
over
meadows.
This
behaviour
attributed
high
geomorphic
activity
producing
detritus
transport
the
early
Little
Ice
Age.
The
advances
of
consequence
thinning;
low-angle
moving
beneath
debris-covered
(GLd)
covers.
Persistent
melt
pools
continue
develop
within
surface
cover
expose
ice.
All
below
regional
snowline
permafrost
can
discounted
for
formation.
Scree
slope
(SS)
development
may
ultimately
sufficient
bare
ice
from
(GL)
(RG).
Reverse
slopes
at
foot
screes
mark
mass
continuum
flow
cover,
not
'rooting
zone'
permafrost-derived
RG.
themselves
show
no
evidence
glacier-like
flow.
A
simple
ice-debris
model
necessary
formation
Language: Английский