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L <- lipdR::readLipd("https://lipdverse.org/data/RZkXNWY88wyoRuBTXfa4/1_0_7/IC03HOIL.lpd")
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In compilations: (only most recent versions are shown)
iso2k-1_1_0
archiveType: GlacierIce
originalDataUrl: this compilation
lipdVersion: 1.3
author: Hoffmann
doi: 10.1029/2002GL014870
latitude: -16.62
longitude: -67.77
elevation: 6350
siteName: Illimani
TSid: LPD599a2ac6
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: LPD6a4f2805
variableName: depth
units: cm
description: depth
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: IC03HOIL01A
variableName: d2H
units: permil
description: glacier ice
basis: Comparison with general circulation model results and meteorological data suggest that the Andean high altitude records are primarily controlled by precipitation variability over the Amazon basin.
direction: NaN
interpDirection: NaN
scope: climate
seasonality: Annual
seasonalityOriginal: Annual
variable: precipitationIsotope
variableDetail: of precipitation
variableGroup: source region
scope: climate
scope: climate
basis: Less (more) depletion of the water isotopes correlates well with anomalously dry (wet) conditions over the Amazon in agreement with the isotopic amount effect [Dansgaard, 1964]., Comparison with general circulation model results and meteorological data suggest that the Andean high altitude records are primarily controlled by precipitation variability over the Amazon basin."
direction: positive
inferredMaterial: precipitation
integrationTime: 1
integrationTimeBasis: chronology based on annual layer counting, volcanic and bomb reference horizons
integrationTimeUncertainty: 7-Feb
integrationTimeUncertaintyType: chronology
integrationTimeUnits: years
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Annual
seasonalityOriginal: Annual
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
scope: isotope
scope: isotope
root
pub
pub1
geo
PaleoData columns
year (yr AD)
interpretation
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depth (cm)
interpretation
1
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3
d2H (permil)
interpretation
1
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3
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