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L <- lipdR::readLipd("https://lipdverse.org/data/zZgsuies0ItMEJZroli1/1_0_7/TR16WEXI.lpd")Report an issue (include datasetId and version)
In compilations: (only most recent versions are shown)
iso2k-1_1_0
archiveType: Wood
originalDataUrl: https://doi.org/10.1594/PANGAEA.869840
lipdVersion: 1.3
journal: Global and Planetary Change
volume: 149
pages: 26-35
title: Multi-century humidity reconstructions from the southeastern Tibetan Plateau inferred from tree-ring δ 18 O
doi: 10.1016/j.gloplacha.2016.12.013
latitude: 30.42
longitude: 95.07
elevation: 3100
siteName: Xinpu, China
TSid: WEB7a8358d2
variableName: year
units: yr AD
description: year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: WEB640da8ea
variableName: d18O
units: permil
description: cellulose
direction: negative
scope: climate
seasonality: Jun-Aug
variable: precipitationIsotope
variableDetail: relative humidity
variableGroup: d18O
scope: climate
scope: climate
basis: Cellulose d18O is strongly influenced by isotopically enriched leaf waters, which is negatively correlated with RH.
direction: positive
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Jun-Aug
seasonalityOriginal: June-August
variable: evaporation
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: ET
scope: isotope
scope: isotope
root
pub
pub1
geo
PaleoData columns
year (yr AD)
interpretation
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d18O (permil)
interpretation
1
2
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