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L <- lipdR::readLipd("https://lipdverse.org/data/6lYiXCN3Eu7Xu4NkIXFH/1_0_7/IC17KOEL.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: Kozachek
doi: 10.5194/cp-13-473-2017
latitude: 43.3483
longitude: 42.4267
elevation: 5115
siteName: Elbrus
TSid: LPD3f5251cc
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: LPD713c6d2a
variableName: depth
units: cm
description: depth
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: IC17KOEL00B
variableName: d18O
units: permil
description: glacier ice
basis: In the warm season (Maya€“October) the isotopic composition depends on local temperatures, but the correlation is not persistent over time, while in the cold season (Novembera€“April), atmospheric circulation is the predominant driver of the ice corea€™s isotopic composition.
direction: NaN
interpDirection: NaN
scope: climate
seasonality: Nov-Apr
variable: circulationVariable
variableDetail: moisture source
variableGroup: atmospheric circluation
scope: climate
scope: climate
basis: Dansgaard W. 1964. Stable isotopes in precipitation. Tellus 16: 436a€“468.
direction: positive
inferredMaterial: precipitation
integrationTime: 1
integrationTimeBasis: based on counting of annual layers (stable isotopes, major ions)
integrationTimeUncertainty: 1
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: IC17KOEL00D
variableName: deuteriumExcess
units: permil
description: glacier ice
direction: NaN
interpDirection: NaN
scope: climate
seasonality: Nov-Apr
variable: deleteMe
variableDetail: NaN
variableGroup: NaN
scope: climate
scope: climate
basis: Dansgaard W. 1964. Stable isotopes in precipitation. Tellus 16: 436a€“468.
direction: positive
inferredMaterial: precipitation
integrationTime: 1
integrationTimeBasis: based on counting of annual layers (stable isotopes, major ions)
integrationTimeUncertainty: 1
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: IC17KOEL00A
variableName: d18O
units: permil
description: glacier ice
basis: In the summer season the isotopic composition depends on the local temperature, while in winter, the atmospheric circulation is the predominant driver of the ice core isotopic composition.
interpDirection: positive
scope: climate
seasonality: Summer
seasonalityOriginal: summer
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: based on counting of annual layers (stable isotopes, major ions)
integrationTimeUncertainty: 1
integrationTimeUncertaintyType: chronology
integrationTimeUnits: years
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Annual
seasonalityOriginal: Annual
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
variableGroupOriginal: d18O of precipitation
scope: isotope
scope: isotope
TSid: IC17KOEL00C
variableName: deuteriumExcess
units: permil
description: glacier ice
basis: So far, no regional or large-scale climate signal could be identified in Elbrus deuterium excess.
interpDirection: NaN
scope: climate
seasonality: Summer
seasonalityOriginal: summer
variable: deleteMe
variableDetail: NaN
variableGroup: NaN
scope: climate
scope: climate
basis: Dansgaard W. 1964. Stable isotopes in precipitation. Tellus 16: 436a€“468.
direction: positive
inferredMaterial: precipitation
integrationTime: 1
integrationTimeBasis: based on counting of annual layers (stable isotopes, major ions)
integrationTimeUncertainty: 1
integrationTimeUncertaintyType: chronology
integrationTimeUnits: years
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Annual
seasonalityOriginal: Annual
variable: precipitationDeuteriumExcess
variableGroup: dxs of precipitation
scope: isotope
scope: isotope
root
pub
pub1
geo
PaleoData columns
year (yr AD)
interpretation
1
2
3
depth (cm)
interpretation
1
2
3
d18O (permil)
interpretation
1
2
3
4
5
6
deuteriumExcess (permil)
interpretation
1
2
3
4
5
6
d18O (permil)
interpretation
1
2
3
4
5
6
deuteriumExcess (permil)
interpretation
1
2
3
4
5
6