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L <- lipdR::readLipd("https://lipdverse.org/data/jbrbttBPh0gIiDnpY0Bu/1_0_7/TR13POMA.lpd")Report an issue (include datasetId and version)
In compilations: (only most recent versions are shown)
iso2k-1_1_0
archiveType: Wood
originalDataUrl: https://www.ncdc.noaa.gov/paleo/study/20930
lipdVersion: 1.3
journal: Climate Dynamics
volume: 42
pages: 771-785
title: Spring-summer temperatures since AD 1780 reconstructed from stable oxygen isotope ratios in white spruce tree-rings from the Mackenzie Delta, northwestern Canada
doi: 10.1007/s00382-013-1674-3
journal: Arctic, Antarctic, and Alpine Research
volume: 41
pages: 497-505
title: Climatic Signals in δ13C and δ18O of Tree-rings from White Spruce in the Mackenzie Delta Region, Northern Canada
doi: 10.1657/1938-4246-41.4.497
latitude: 68.4
longitude: -133.8
elevation: 3
siteName: Mackenzie Delta, NWT, Canada
TSid: WEBd905a8ca
variableName: year
units: yr AD
description: year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: WEB4de479a5
variableName: d18O
units: permil
description: cellulose
direction: positive
scope: climate
seasonality: Apr-Jul
variable: precipitationIsotope
variableDetail: minimum temperature
variableGroup: d18O
scope: climate
scope: climate
basis: plant waters are influenced by spring-summer precipitation d18O, which is strongly influenced by minimum spring-summer temperatures
direction: positive
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Apr-Jul
seasonalityOriginal: 4 5 6 7 (spring-summer)
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
variableGroupOriginal: T_air
scope: isotope
scope: isotope
root
pub
pub1
pub2
geo
PaleoData columns
year (yr AD)
interpretation
1
2
3
d18O (permil)
interpretation
1
2
3
4
5
6