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L <- lipdR::readLipd("https://lipdverse.org/data/aTIaF2qAj1D9VLqaeVSM/1_0_7/TR08THCO.lpd")
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In compilations: (only most recent versions are shown)
iso2k-1_1_0
archiveType: Wood
originalDataUrl: https://www.ncdc.noaa.gov/paleo/study/17576
lipdVersion: 1.3
author: Edwards T. W. D.
doi: 10.1016/j.yqres.2008.04.013
latitude: 52.5
longitude: -118
elevation: 1700
siteName: Columbia Icefield, British Columbia, Canada
TSid: MAT311be19d10
variableName: year
units: yr AD
description: Year AD_end
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: MAT311be19d102
variableName: year
units: yr AD
description: Year AD_end
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: MAT91b632920d
variableName: year
units: yr AD
description: Year AD_start
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: TR08THCO00
variableName: d18O
units: permil
description: cellulose
basis: Early-millennium climate was marked by relatively warm winters and high growth season relative humidity, especially ~AD 1100a€“1250, followed by the onset of cooler and drier conditions in the early 1500s. Winter temperatures apparently attained 20th century levels by about AD 1800, while relatively low growth season humidity persisted until
about AD 1900.
direction: negative
scope: climate
seasonality: Annual
variable: temperature
variableDetail: Seasonal, annual
variableGroup: T_air, RH, P_amount
scope: climate
scope: climate
basis: precipitation d18O is positively correlated with temperature, and tree source water and tree-ring cellulose record precip d18O
direction: positive
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Dec-Feb
seasonalityOriginal: December, January, February
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
scope: isotope
scope: isotope
root
pub
pub1
geo
PaleoData columns
year (yr AD)
interpretation
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year (yr AD)
interpretation
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year (yr AD)
interpretation
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d18O (permil)
interpretation
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