Research Square (Research Square),
Journal Year:
2023,
Volume and Issue:
unknown
Published: Nov. 21, 2023
Abstract
In
the
hunt
for
seismic
precursors
with
GNSS
to
detect
earthquake-related
anomalies
in
ionosphere
are
proved
as
an
effective
strategy.
One
method
is
use
TEC
distinguish
between
and
induced
by
geo
magnetic
storm.
this
study,
data
of
four
sites
near
epicenter
November
30,
2018,
Alaska
earthquake
(Mw
7.1)
examined.
We
also
examined
from
Swarm
satellites
during
local
day
nighttime
further
support
EQ-induced
perturbations
ionosphere.
six
days
before
major
EQ,
stations'
displayed
considerable
disturbance
positive
crossing
upper
bound.
The
stations
EQ
detected
1
6
prior
EQ.
swarm
confirmed
these
findings.
On
other
hand,
retrieving
all
preparation
phase
weak
storm
(Kp
4,
Dst
−
50
nT),
we
discover
evidence
low-intensity
25–30
shock.
Further
research
shows
that
UTC
17:30
23:00
storm-induced
anomaly
(caused
=
-50
nT
Kp
4)
predominates
17:00
23:30.
phase,
primary
shock
helpful
separating
geomagnetic
anomalies.
Additionally,
using
monitoring,
work
contributes
growing
lithosphere-ionosphere
connection
concept.
Geocarto International,
Journal Year:
2024,
Volume and Issue:
40(1)
Published: Dec. 23, 2024
Soil
is
a
vital
nonrenewable
resource
characterized
by
rapid
degradation
and
slow
regeneration
processes.
In
this
study,
soil
in
Jaén
San
Ignacio
was
assessed
via
multicriteria
evaluation
approach
combined
with
remote
sensing
(RS)
data.
Nine
factors
were
analyzed
classified
three
categories:
environmental,
topographic,
edaphological
factors.
The
results
revealed
that
the
slope
(59.07%)
main
influencing
factor,
followed
land
use
cover
(LULC)
(56.36%).
map
83.48%
of
area
exhibited
moderate
degradation,
14.49%
low
1.56%
high
degradation.
districts
Pomahuaca
José
de
Lourdes
demonstrated
largest
areas
accounting
for
13.71%
22.54%,
respectively.
Bellavista
Huarango
very
0.27%
0.08%,
(AHP)
method
RS
data
employed
to
assess
highlighting
need
sustainable
restoration
conservation
strategies.
Revista Brasileira de Meteorologia,
Journal Year:
2022,
Volume and Issue:
37(3), P. 313 - 327
Published: Sept. 1, 2022
Resumo
Os
incêndios
ocorrem
devido
às
ações
antrópicas
e
causam
problemas
socioambientais
no
Nordeste
do
Brasil
(NEB).
Portanto,
este
estudo
avaliou
a
variabilidade
espaço-temporal
dos
focos
de
calor
(FC)
nas
três
mesorregiões
climáticas
Alagoas:
Sertão,
Leste
Agreste
Alagoano.
dados
FC
foram
obtidos
Banco
Dados
Queimadas
(BDQueimadas)
entre
1998-2020.
A
série
temporal
foi
submetida
análises
estatísticas
descritiva,
exploratória
multivariada
aplicada
aos
102
municípios
alagoanos.
Com
base
agrupamento
hierárquico
identificaram-se
grupos
homogêneos
(G1,
G2
G3)
Sertão
dois
Alagoano
(G1
G2).
Alguns
não
formaram
(NA),
tais
como:
Belo
Monte
(26,83
±
25,87
focos),
Limoeiro
Anadia
(54,48
38,65
Penedo
(262,83
183,80
focos)
Coruripe
(553
369,40
focos).
interanual
em
Alagoas
está
associada
com
atividades
agrícolas,
desmatamento,
novas
áreas
para
criação
animais
colheita
da
cana-de-açúcar.
Na
avaliação
espacial
via
densidade
por
município
utilizou-se
o
período
total
(1998-2020)
os
anos
destaque
na
(2012
2019).
O
maior
registro
encontra-se
mesorregião
se
descarta
que
sejam
influenciados
pela
ocorrência
seca
períodos
estiagens
Alagoas.
Research Square (Research Square),
Journal Year:
2023,
Volume and Issue:
unknown
Published: Nov. 21, 2023
Abstract
In
the
hunt
for
seismic
precursors
with
GNSS
to
detect
earthquake-related
anomalies
in
ionosphere
are
proved
as
an
effective
strategy.
One
method
is
use
TEC
distinguish
between
and
induced
by
geo
magnetic
storm.
this
study,
data
of
four
sites
near
epicenter
November
30,
2018,
Alaska
earthquake
(Mw
7.1)
examined.
We
also
examined
from
Swarm
satellites
during
local
day
nighttime
further
support
EQ-induced
perturbations
ionosphere.
six
days
before
major
EQ,
stations'
displayed
considerable
disturbance
positive
crossing
upper
bound.
The
stations
EQ
detected
1
6
prior
EQ.
swarm
confirmed
these
findings.
On
other
hand,
retrieving
all
preparation
phase
weak
storm
(Kp
4,
Dst
−
50
nT),
we
discover
evidence
low-intensity
25–30
shock.
Further
research
shows
that
UTC
17:30
23:00
storm-induced
anomaly
(caused
=
-50
nT
Kp
4)
predominates
17:00
23:30.
phase,
primary
shock
helpful
separating
geomagnetic
anomalies.
Additionally,
using
monitoring,
work
contributes
growing
lithosphere-ionosphere
connection
concept.