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L <- lipdR::readLipd("https://lipdverse.org/data/PUi5qjh8kt5AxhCUS1qN/1_0_7/TR16LAAN.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/20002
lipdVersion: 1.3
author: Labuhn I.
doi: 10.5194/cp-12-1101-2016
latitude: 45.7333
longitude: 0.3
elevation: 124
siteName: Angouleme, France
TSid: MAT81d90f33cf
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: TR16LAAN00
variableName: d18O
units: permil
description: cellulose
basis: The oldest part of the reconstruction is characterized by a prolonged period of relatively wet conditions
(1360a€“1450), followed by a period of drier conditions until 1600. Another wet period until 1760 follows, with
a short increase to relatively drier conditions around 1720. The most marked trend in the reconstruction is the shift to
dry conditions from 1760 to 1850. The late 20th century is characterized by increasingly dry summers, but these SPEI
values are not unprecedented in the record.
direction: T_air (positive), P_amount (negative), SPEI (negative)
scope: climate
seasonality: Jun-Aug
seasonalityOriginal: June, July, August
variable: temperature
variableDetail: Maximum temperature
variableGroup: T_air, P_amount, drought index SPEI
scope: climate
scope: climate
basis: Drought conditions lead to enriched soil water and leaf water.
direction: negative
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Jun-Aug
seasonalityOriginal: June, July, August
variable: effectivePrecipitation
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: P_E
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