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L <- lipdR::readLipd("https://lipdverse.org/data/raV8oqSVhhL3io2bZaFf/1_0_10/IC00THDS.lpd")Report an issue (include datasetId and version)
In compilations: (only most recent versions are shown)
iso2k-1_1_2
archiveType: GlacierIce
originalDataUrl: https://www.ncdc.noaa.gov/paleo-search/study/11180
lipdVersion: 1.3
author: list(name = "Thompson")
doi: 10.1126/science.289.5486.1916
latitude: 28.38
longitude: 85.72
elevation: 7200
siteName: Dasuopu
TSid: LPD80155fb9
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: LPDe86e42a4
variableName: depth
units: cm
description: depth
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: IC00THDS03B
variableName: d18O
units: permil
description: glacier ice
basis: correlation to meteorological data, ("...these data provide qualitative support for the hypothesis that temperature, not the amount effect, is the dominant process controlling d18O over the Tibetan Plateau.")
direction: positive
interpDirection: positive
scope: climate
seasonality: Jun-Aug
variable: temperature
variableDetail: air@surface
variableDetailOriginal: air
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T
variableOriginal: temperature
scope: climate
scope: climate
basis: Yao, T., Thompson, L. G., Mosley-Thompson, E., Zhihong, Y., Xingping, Z., and Lin, P.-N.: 1996,Climatological Significance of I´18O in North Tibetan Ice Cores, J. Geophys. Res. 101, 29531a€“29537
direction: positive
inferredMaterial: precipitation
integrationTime: 1
integrationTimeBasis: age model based on beta activity and counting of annual layers (seasonal variations of stable isotopes)
integrationTimeUncertainty: 1 after 1440, 5 before 1440
integrationTimeUncertaintyType: chronology
integrationTimeUnits: years
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Jun-Aug
seasonalityOriginal: summer
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
scope: isotope
scope: isotope
TSid: IC00THDS03Ay
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: IC00THDS03A
variableName: d18O
units: permil
description: glacier ice
basis: correlation to meteorological data, ("...these data provide qualitative support for the hypothesis that temperature, not the amount effect, is the dominant process controlling d18O over the Tibetan Plateau.")
direction: positive
interpDirection: positive
scope: climate
seasonality: Jun-Aug
variable: temperature
variableDetail: air@surface
variableDetailOriginal: air
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T
variableOriginal: temperature
scope: climate
scope: climate
basis: Yao, T., Thompson, L. G., Mosley-Thompson, E., Zhihong, Y., Xingping, Z., and Lin, P.-N.: 1996,Climatological Significance of ?18O in North Tibetan Ice Cores, J. Geophys. Res. 101, 29531?29537
direction: positive
inferredMaterial: precipitation
integrationTime: 1
integrationTimeBasis: age model based on beta activity and counting of annual layers (seasonal variations of stable isotopes)
integrationTimeUncertainty: 1 to 15
integrationTimeUncertaintyType: chronology
integrationTimeUnits: years
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Jun-Aug
seasonalityOriginal: summer
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
scope: isotope
scope: isotope
root
pub
pub1
geo
PaleoData columns
year (yr AD) [1-1]
interpretation
1
2
3
depth (cm) [1-1]
interpretation
1
2
3
d18O (permil) [1-1]
interpretation
1
2
3
4
5
6
year (yr AD) [1-2]
interpretation
1
2
3
d18O (permil) [1-2]
interpretation
1
2
3
4
5
6