L <- lipdR::readLipd("https://lipdverse.org/data/lpb2vgyekehVCJEwWEQT/1_0_6/IC06THPR.lpd")Report an issue (include datasetId and version)
In compilations: (only most recent versions are shown)
iso2k-1_1_2
archiveType: GlacierIce
lipdVersion: 1.3
author: list(name = "Thompson")
doi: 10.3189/172756406781812357
latitude: 33.9167
longitude: 89.0833
elevation: 6070
siteName: Puruogangri ice cap
TSid: LPDbe7e0702
variableName: year
units: yr AD
description: Year AD
coefficient: NA
fraction: NA
rank: NA
scope: isotope
coefficient: NA
fraction: NA
rank: NA
scope: isotope
coefficient: NA
fraction: NA
rank: NA
scope: isotope
TSid: IC06THPR01A
variableName: d18O
units: permil
description: glacier ice
basis: An abrupt warming (inferred from higher d18O values) occurred between 1910 and 1920 (Fig 6a and b)...
direction: positive
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: 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
coefficient: NA
direction: positive
fraction: NA
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 to 60
integrationTimeUncertaintyType: chronology
integrationTimeUnits: years
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Annual
seasonalityOriginal: Annual
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
coefficient: NA
fraction: NA
rank: NA
scope: isotope
coefficient: NA
fraction: NA
rank: NA
scope: isotope
TSid: IC06THPR02Ays
variableName: year
units: yr AD
description: Year AD
coefficient: NA
fraction: NA
rank: NA
scope: isotope
coefficient: NA
fraction: NA
rank: NA
scope: isotope
coefficient: NA
fraction: NA
rank: NA
scope: isotope
TSid: IC06THPR02A
variableName: d18O
units: permil
description: glacier ice
basis: An abrupt warming (inferred from higher d18O values) occurred between 1910 and 1920 (Fig 6a and b)...
direction: positive
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: 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
coefficient: NA
direction: positive
fraction: NA
inferredMaterial: precipitation
integrationTime: 1
integrationTimeBasis: age model based on counting of annual layers (seasonal variations of dust and stable isotopes), beta activity and ice-flow modelling
integrationTimeUncertainty: 1 after 1963, 15 after 1600, up to 68 before 1600
integrationTimeUncertaintyType: chronology
integrationTimeUnits: years
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Annual
seasonalityOriginal: Annual
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
coefficient: NA
fraction: NA
rank: NA
scope: isotope
coefficient: NA
fraction: NA
rank: NA
scope: isotope
TSid: IC06THPR02Bys
variableName: year
units: yr AD
description: Year AD
coefficient: NA
fraction: NA
rank: NA
scope: isotope
coefficient: NA
fraction: NA
rank: NA
scope: isotope
coefficient: NA
fraction: NA
rank: NA
scope: isotope
TSid: IC06THPR02B
variableName: d18O
units: permil
description: glacier ice
basis: An abrupt warming (inferred from higher d18O values) occurred between 1910 and 1920 (Fig 6a and b)...
direction: positive
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: 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
coefficient: NA
direction: positive
fraction: NA
inferredMaterial: precipitation
integrationTime: 1
integrationTimeBasis: age model based on counting of annual layers (seasonal variations of dust and stable isotopes), beta activity and ice-flow modelling
integrationTimeUncertainty: 1 after 1963, 15 after 1600, up to 68 before 1600
integrationTimeUncertaintyType: chronology
integrationTimeUnits: years
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Annual
seasonalityOriginal: Annual
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
coefficient: NA
fraction: NA
rank: NA
scope: isotope
coefficient: NA
fraction: NA
rank: NA
scope: isotope
root
pub
pub1
geo
PaleoData columns
year (yr AD) [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
year (yr AD) [1-3]
interpretation
1
2
3
d18O (permil) [1-3]
interpretation
1
2
3
4
5
6