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L <- lipdR::readLipd("https://lipdverse.org/data/K5mWl4guYTrkFTnhTKnV/1_0_7/TR11GRTP.lpd")Report an issue (include datasetId and version)
In compilations: (only most recent versions are shown)
iso2k-1_1_0
archiveType: Wood
originalDataUrl: this compilation
lipdVersion: 1.3
author: list(list(name = "GrieSSinger, Jussi"), list(name = "Braeuning, Achim"), list(name = "Helle, Gerd"), list(name = "Thomas, Axel"), list(name = "Schleser, Gerhard"))
journal: Geophysical Research Letters
volume: 38
pages: n/a-n/a
title: Late Holocene Asian summer monsoon variability reflected by δ18O in tree-rings from Tibetan junipers
doi: 10.1029/2010GL045988
latitude: 30.3083
longitude: 91.5167
elevation: 4150
siteName: Reting site, China
TSid: WEBaa035294
variableName: year
units: yr AD
description: year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: WEB7c902e21
variableName: d18O
units: permil
description: cellulose
direction: negative
scope: climate
seasonality: Summer
seasonalityOriginal: summer
variable: precipitationIsotope
variableDetail: summer monsoon
variableGroup: precipitation d18O
scope: climate
scope: climate
basis: Source water d18O is determined by P_isotopes, which is strongly influenced by precipitation amount (negative relation).
direction: positive
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Aug
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
variableGroupOriginal: precipitation amount
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