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L <- lipdR::readLipd("https://lipdverse.org/data/fSUtNl0uXiQNi6agKRON/1_0_7/IC15GANK.lpd")Report an issue (include datasetId and version)
In compilations: (only most recent versions are shown)
iso2k-1_1_0
archiveType: GlacierIce
originalDataUrl: https://www.ncdc.noaa.gov/paleo-search/study/21171
lipdVersion: 1.3
author: Gao
doi: 10.1007/s00382-015-2584-3
latitude: 29.04
longitude: 90.2
elevation: 5950
siteName: Noijin Kangsang Glacier
TSid: MAT127c9803e9
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: IC15GANK01A
variableName: d18O
units: permil
description: glacier ice
basis: correlation to meteorological data
direction: positive
interpDirection: positive
scope: climate
seasonality: Jun-Sep
variable: temperature
variableDetail: air@surface
variableDetailOriginal: air
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T
variableOriginal: temperature
scope: climate
scope: climate
basis: Tian, L., V. Masson-Delmotte, M. Stievenard, T. Yao and J. Jouzel.2001. Tibetan Plateau summer monsoon northward extent revealed by measurements of water stable isotopes.J. Geophys. Res., 106(D22), 28,081?28,088.
direction: positive
inferredMaterial: precipitation
integrationTime: 1
integrationTimeBasis: based on volcanic horizons, beta activity and counting of annual layers (seasonal variations of stable isotopes)
integrationTimeUncertainty: 1 to 2
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: IC15GANK01B
variableName: d2H
units: permil
description: 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
d2H (permil)
interpretation
1
2
3
4
5
6