Data in Brief,
Journal Year:
2021,
Volume and Issue:
38, P. 107277 - 107277
Published: Aug. 11, 2021
Global
bottled
water
consumption
has
largely
increased
(14.35
billion
gallons
in
2020)
[1],
[2],
[3],
[4],
[5]
during
the
last
decade
since
consumers
are
demanding
healthier
and
safer
forms
of
rehydration.
Bottled
sources
normally
labeled
as
mountainous
pristine
mineral
springs
(fed
by
rainfall
snow/glacier
melting
processes),
deep
groundwater
wells
or
industrial
purified
water.
The
advent
numerous
international
national-based
brands
simultaneously
raised
a
worldwide
awareness
related
to
source
chemical
content
traceability
[6].
Here,
we
present
first
database
stable
isotope
compositions
reported
concentrations
from
imported
waters
Costa
Rica.
In
total,
45
produced
Rica
31
USA,
Europe,
Oceania,
other
countries
Central
America
were
analyzed
for
δ18O,
δ2H,
d-excess.
Chemical
obtained
available
bottle
labels.
National-based
ranged
-2.47‰
-10.65‰
δ18O
-10.4‰
-78.0‰
while
d-excess
varied
+4.2‰
up
+17.0‰.
International
between
-2.21‰
-11.03‰
-11.3‰
-76.0‰
+5.0‰
+19.1‰.
Rica,
only
19%
parameters
such
Na+,
K+,
Ca+2,
Mg+2,
F−,
Cl−,
NO3−,
SO4−2,
CO3−2,
SiO2,
dry
residue,
pH;
whereas
27%
products
similar
parameters.
absence
specific
geographic
coordinates
origin
limited
spatial
analysis
validate
versus
isoscapes
[7].
This
highlights
potential
relevance
use
improve
urgent
need
more
robust
legislation
order
provide
detailed
information
(i.e.,
source,
composition,
purification
processes)
final
consumers.
Water Resources Research,
Journal Year:
2025,
Volume and Issue:
61(2)
Published: Feb. 1, 2025
Abstract
The
spatial
variation
of
soil
water
isotopes
(SWI)—representing
the
baseline
for
investigating
root
uptake
(RWU)
depths
with
stable
isotope
techniques—has
rarely
been
investigated.
Here,
we
use
SWI
depth
profile
sampling
in
combination
unmanned
aerial
vehicle
(UAV)
based
land
surface
temperature
estimates
and
vegetation
indices
(VI)
order
to
improving
process
understanding
relationships
between
variability
content
patterns
canopy
status,
represented
form
VI.
We
carried
out
a
10
profiles
tropical
dry
forest.
UAV
data
were
collected
analyzed
obtain
detailed
characterization
status.
then
performed
statistical
analysis
VI
temperatures
values
at
different
resolutions
(3
cm–5
m).
Best
used
generating
isoscapes
entire
study
area.
Results
suggest
that
are
strongly
mediated
by
parameters
(VI).
Various
correlate
across
all
depths.
depend
on
(
R
2
0.66
δ
18
O
0.64
H).
Strongest
overall
correlations
found
resolution
0.5
m.
speculate
this
might
be
ideal
spatially
characterizing
investigate
RWU
forest
environments.
Supporting
analyses
UAV‐based
approaches
future
avenue
representation
credibility
such
studies.
Ecohydrology,
Journal Year:
2023,
Volume and Issue:
16(5)
Published: March 7, 2023
Abstract
Tracer‐aided
studies
to
understand
plant
water
uptake
sources
and
dynamics
in
tropical
ecosystems
are
limited.
Here,
we
report
the
analysis
of
dry
season
source
patterns
five
unique
Costa
Rica
across
altitudinal
(<150–3,400
m
asl)
latitudinal
(Caribbean
Pacific
slopes)
gradients:
evergreen
seasonal
rainforests,
cloud
forest,
Páramo
forest.
Soil
samples
were
collected
during
2021.
Plant
soil
extractions
conducted
using
centrifugation.
Stem
extracted
volume
stem
total
content
calculated
via
gravimetric
analysis.
Water
contributions
estimated
a
Bayesian
mixing
model.
Isotope
ratios
stems
exhibited
strong
meteoric
origin.
Enrichment
trends
only
detected
cactus
within
forest
ecosystem.
profiles
revealed
nearly
uniform
isotopic
profiles;
however,
depletion
trend
was
observed
ecosystem
below
25
cm.
More
enriched
compositions
reported
for
volumes
above
~20%
(
adj.
r
2
=
0.34,
p
<
0.01).
The
most
prominent
rainforest
(74.0%),
(86.4%)
(66.0%)
corresponded
well‐mixed
water.
In
ecosystem,
recent
rainfall
produced
by
trade
wind
incursions
resulted
significant
(61.9%),
whereas
mean
annual
precipitation
(38.6%)
baseflow
(33.1%)
dominant
sources.
latter
highlights
prevalence
distinct
between
cold
front
(near‐surface
storage)
more
moisture
season,
revealing
ecohydrological
processing
previously
unknown
this
region.
Hydrological Processes,
Journal Year:
2022,
Volume and Issue:
36(6)
Published: May 14, 2022
Abstract
The
hydroclimatology
of
Northern
South
America
responds
to
the
coupling
between
Pacific
and
Atlantic
oceans,
Amazon–Andes
interactions,
orographic
barrier
regional
Andes.
relative
contributions
oceanic
terrestrial
moisture
sources
have
been
mostly
evaluated
in
modelling
studies,
with
limited
observational
data
for
validation.
We
combine
observations
from
stable
isotopes
precipitation
output
Lagrangian
trajectory
tracking
model
FLEXPART
characterize
contrast
contribution
(from
Pacific)
different
regions
continent)
mean
monthly
Andes
Caribbean
Colombia.
Our
results
indicate
that
most
becoming
rain
region
has
an
atmospheric
residence
time
deviates
commonly
assumed
10
days.
These
times
vary
source
sink
1
day
case
recycling
more
than
days
Andean
originating
Ocean.
Common
integration
both
all
are
order
three
7
Most
comes
including
same
(>30%
months),
Orinoco
River
basin
(up
28%
April),
northern
Amazon
17%
June,
July,
August);
followed
by
individually
considered
Tropical
30%
October,
November
December)
North
January).
fact
a
significant
proportion
rainfall
is
recycled
highlights
water
availability
Colombia
could
potentially
be
altered
current
widespread
pervasive
changes
vegetation
cover.
More
generally,
our
highlight
need
assess
hydrological
consequences
land
cover
change
America,
particularly
country
like
where
water,
food,
energy
security
depend
directly
on
precipitation.
Journal of Hydrometeorology,
Journal Year:
2022,
Volume and Issue:
unknown
Published: April 28, 2022
Abstract
Knowledge
about
precipitation
generation
remains
limited
in
the
tropical
Andes
due
to
lack
of
water
stable
isotope
(WSI)
data.
Therefore,
we
investigated
key
factors
controlling
isotopic
composition
Páramo
highlands
southern
Ecuador
using
event-based
(high
frequency)
WSI
data
collected
between
November
2017
and
October
2018.
Our
results
show
that
air
masses
reach
study
site
preferentially
from
eastern
flank
through
Amazon
basin
(73.2%),
Orinoco
plains
(11.2%),
Mato
Grosso
Massif
(2.7%),
whereas
only
a
small
proportion
stems
Pacific
Ocean
(12.9%).
A
combination
local
regional
influences
δ
18
O
precipitation.
Regional
atmospheric
features
(Atlantic
moisture,
evapotranspiration
over
Forest,
continental
rain-out,
altitudinal
lapse
rates)
are
what
largely
control
meteoric
composition.
Local
precipitation,
temperature,
fraction
corresponding
moderate
heavy
rainfalls
also
influencing
ratios,
highlighting
importance
localized
convective
at
site.
Contrary
O,
d
-excess
values
showed
little
temporal
variation
could
not
be
statistically
linked
or
hydrometeorological
features.
The
latter
reveals
large
amounts
recycled
moisture
contributes
regardless
season
predominant
trajectories
east.
findings
will
help
improve
isotope-based
climatic
models
enhance
paleoclimate
reconstructions
highlands.
Frontiers in Water,
Journal Year:
2022,
Volume and Issue:
3
Published: Jan. 24, 2022
Tropical
peatlands
are
distributed
mainly
in
coastal
lowlands;
however
high
elevation
regions
exhibit
a
large
prevalence
of
small
and
fragmented
that
mostly
understudied.
Artificial
drainage
to
expand
the
area
cattle
farming,
horticulture,
urbanization
is
increasing
carbon
losses
atmosphere
streams
worldwide.
Here,
we
present
an
exploratory
characterization
dissolved
optical
properties
ombrotrophic
peat
bogs
Talamanca
range
Costa
Rica,
across
altitudinal
gradient
(2,400–3,100
m
a.s.l.)
during
rainy
season.
Dissolved
organic
matter
(DOM)
sources
decomposition
processes
were
evaluated
light
inorganic
(DOC
DIC),
properties,
major
water
chemistry.
DOC
concentrations
ranged
from
0.2
up
47.0
mg/L.
DIC
below
2
mg/L
δ
13
C
values
indicated
mixture
between
soil
matter,
CO
water,
lesser
degree
derived
bacterial
.
Absolute
fluorescence
intensity
humic-like
peaks
was
6–7
times
greater
than
fresh-like
all
sites.
Fluorescence
peak
ratios
coupled
with
biological
humification
indexes
point
relative
contribution
recalcitrant
soil-derived
DOM.
Excitation/Emission
matrices
denoted
humic
fulvic
acids
bogs,
moderate
intensities
soluble
microbial
by-products-like
aromatic
protein
at
three
Our
data
provides
baseline
underpin
tropical
dynamics
peatlands.
Hydrological Sciences Journal,
Journal Year:
2024,
Volume and Issue:
69(11), P. 1523 - 1538
Published: Aug. 5, 2024
In
this
study,
we
explore
the
utility
of
stable
isotopes
water
(δ2H
and
δ18O)
as
integrative
proxies
for
evaporative
condition
in
high-mountain
tropical
lakes
using
a
set
small
Ecuadorian
Cajas
National
Park.
Specifically,
(1)
characterize
variability
isotopic
composition
across
several
varying
size
depth
(2)
determine
evaporation
fraction
inflow
these
lakes.
We
have
used
Hydrocalculator
tool
estimation
to
(E/I)
ratio.
Results
indicated
that
larger
lower
seasonal
their
compared
with
smaller
Further,
there
was
clear
variation
monthly
E/I
ratios
estimated
lakes,
indicating
likely
plays
some
(albeit
limited)
role
level
experienced
within
year.
Hydrological Processes,
Journal Year:
2022,
Volume and Issue:
36(2)
Published: Feb. 1, 2022
Abstract
There
is
still
limited
understanding
of
where
stream
water
originates,
their
flow
paths,
how
sources
mix,
and
for
long
transits
montane
tropical
catchments.
Here,
we
used
a
simple
gamma
convolution
integral
model
(GM),
ensemble
hydrograph
separation
(EHS)
tracer‐aided
(TAM)
to
assess
runoff
generation,
mixing
processes
ages
in
the
pristine
rainforest
Quebrada
Grande
catchment
Costa
Rica.
Model
simulations
are
based
on
four‐year
record
(2016–2019)
continuous
hydrometric
stable
isotope
observations.
Comparative
tests
included
multi‐objective
calibration
(2017–2019)
validation
(2016)
using
discharge
data
as
well
an
independent
evaluation
groundwater
soil
data.
GM
TAM
agreed
dominance
young
streamflow
that
was
less
than
95
days
old
75%
study
period.
The
EHS
suggested
fraction
threshold
12
±
2
with
transit
time
distribution
approximates
best‐fit
GM.
These
short
result
high
annual
rainfall
even
during
drier
years
such
2019
4300
mm/a
consistent
quick
near‐surface
generation
mixing.
A
supra‐regional
loss
(~55%)
likely
older
detected.
TAM‐based
(streamflow
KGE
>
0.78,
δ
H
0.90)
average
contribution
more
60%
emphasizing
paths.
This
represents
one
quickest
responses
mostly
catchments
globally.
Journal of Geophysical Research Atmospheres,
Journal Year:
2022,
Volume and Issue:
127(21)
Published: Oct. 18, 2022
Abstract
Every
year,
several
typhoons
originating
from
the
West
Pacific
come
close
to
Taiwan,
modulating
regional
weather
through
intense
rainfall
and
enhanced
humidity.
The
isotopic
ratios
(δ
18
O
δD)
in
typhoon
vapor
evolve
along
its
track
due
rainout,
recycling,
replenishment.
In
2016,
this
signature
was
recorded
Taipei
as
vapors
invaded
local
atmosphere.
After
disintegration,
isotope
of
atmosphere
slowly
return
background
value.
fall
rise
give
a
V‐shaped
variation.
processes
controlling
(like
moisture
turnover,
speed,
wind
direction)
are
fast
(1–2
days).
contrast,
recovery
is
slow
(several
days)
depending
on
replacement
rate
atmospheric
by
incoming
oceanic
vapor.
An
evolution
model
based
Rayleigh
condensation
box
mixing
phase
proposed
employed
explain
V‐shape.
combination
these
two
models
for
four
major
(Nepartak,
Megi,
Meranti,
Malakas)
shows
agreement
with
observations.
suggests
that
precipitation
efficiency,
PE
(rainfall/overhead
moisture),
size
important
parameters
decrease
ratio.
characteristic
turnover
time
(inverse
PE,
obtained
European
Centre
Medium‐Range
Weather
Forecasts
fifth
Re‐Analysis
data)
estimated
be
∼2
days
500
km
radius.
Our
study
provides
constraints
budget
typhoons.
PLOS Water,
Journal Year:
2023,
Volume and Issue:
2(10), P. e0000136 - e0000136
Published: Oct. 11, 2023
Mexico
encompasses
a
large
spectrum
of
landscapes
with
topographic,
geographic,
and
climatic
factors
interacting
in
complex
ecohydrological
setting.
For
decades,
isotope
hydrogeological
tools
have
been
applied
using
short-term
or
seasonal
local
meteoric
water
lines
as
valid
input
functions.
Yet,
systematic
evaluation
characteristics
is
still
lacking.
Here
we
report
on
the
spatial
temporal
variations
21
precipitation
monitoring
stations
across
Mexico.
Our
database
includes
608
monthly
samples
collected
from
2018
to
2021
over
four
regions
(between
5
2,365
m
asl):
Pacific
coast,
Gulf
Mexico/Caribbean
Sea
region,
Central
Northern
plateaus.
Precipitation
δ
18
O
seasonality
dry
(winter)
wet
season
(summer)
was
characterized
by
notable
W-shaped
variability.
Monthly
amounts
compositions
exhibited
poor
strong
linear
regressions
(
Adj
.
r
2
<0.01
0.75),
inverse
(positive)
relationships
northern
monsoon-affected
region.
Low
d
-excess
(5.1
9.7‰)
corresponded
greater
terrestrial
moisture
contributions
(20.5%)
arid
regions.
Moisture
inputs
Ocean
were
associated
near-equilibrium
values
(8.8
14.3‰),
respectively.
The
best-fit
models
for
=
0.85)
H
0.88)
determined
topographic
geographical
predictors,
resulting
an
updated
high-resolution
isoscape
(100
grid)
Orographic
barriers
(-2.10‰
O/km)
coupled
interaction
tropical
cyclones
cold
fronts,
evolution
North
American
Monsoon
system,
passage
easterly
trade
winds
play
remarkable
role
controlling
rainfall
findings
provide
robust
baseline
ecohydrological,
climatic,
forensic,
archeological,
paleoclimate
studies
America.