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L <- lipdR::readLipd("https://lipdverse.org/data/wCUJ7y0r22MgO1lhpXe0/1_0_7/IC15MANE.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: Masson-Delmotte
doi: 10.5194/tc-9-1481-2015
latitude: 77.45
longitude: -51.06
elevation: 2450
siteName: NEEM
TSid: LPD9472e53c
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: IC15MANE00A
variableName: d18O
units: permil
description: glacier ice
basis: correlation to meteorological data
direction: positive
interpDirection: positive
scope: climate
seasonality: Annual
seasonalityOriginal: Annual
variable: temperature
variableDetail: air@surface
variableDetailOriginal: air
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T
variableOriginal: temperature
scope: climate
scope: climate
basis: Dansgaard W. 1964. Stable isotopes in precipitation. Tellus 16: 436a€“468.
direction: positive
inferredMaterial: precipitation
integrationTime: 1
integrationTimeBasis: age model based on volcanic horizons and counting of annual layers (seasonal variations of stable isotopes)
integrationTimeUncertainty: 1 to 10
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
TSid: IC15MANE01B
variableName: deuteriumExcess
units: permil
description: glacier ice
basis: correlation to meteorological data
direction: positive
interpDirection: positive
scope: climate
seasonality: Annual
seasonalityOriginal: Annual
variable: precipitationDeuteriumExcess
variableDetail: air@surface
variableDetailOriginal: air
variableGroup: Sea surface temperature and humidity at the oceanic source region of the precipitation
scope: climate
scope: climate
basis: Dansgaard W. 1964. Stable isotopes in precipitation. Tellus 16: 436a€“468.
direction: positive
inferredMaterial: precipitation
integrationTime: 1
integrationTimeBasis: age model based on volcanic horizons and counting of annual layers (seasonal variations of stable isotopes)
integrationTimeUncertainty: 1 to 10
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
TSid: LPD007e999e
variableName: uncertainty
units: permil
description: There is no significant relationship between stable isotopes and precipitation (net accumulation) on the Quelccaya ice cap. In other words, the precipitation “amount effect” does not appear to govern the stable isotopic chemistry on this tropical glacier. Because 70 to 80% of the precipitation falling on Quelccaya arrives during the wet season, the δ18O history reflects primarily conditions during austral summer. Decadal averages of precipitation amount and δ18O are not strongly related
rank: NA
scope: climate
rank: NA
scope: climate
scope: climate
scope: isotope
scope: isotope
scope: isotope
TSid: LPD007e999e1
variableName: uncertainty1s
units: permil
description: stdev of stack of d excess of glacier ice
rank: NA
scope: climate
rank: NA
scope: climate
scope: climate
scope: isotope
scope: isotope
scope: isotope
root
pub
pub1
geo
PaleoData columns
year (yr AD)
interpretation
1
2
3
d18O (permil)
interpretation
1
2
3
4
5
6
deuteriumExcess (permil)
interpretation
1
2
3
4
5
6
uncertainty (permil)
interpretation
1
2
3
4
5
6
uncertainty1s (permil)
interpretation
1
2
3
4
5
6