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L <- lipdR::readLipd("https://lipdverse.org/data/SS43syE2Cp0YO04h7qMc/1_0_7/TR13SAWA00.lpd")Report an issue (include datasetId and version)
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iso2k-1_1_0
archiveType: Wood
originalDataUrl: https://www.ncdc.noaa.gov/paleo/study/22548
lipdVersion: 1.3
author: Sano M.
journal: Journal of Geophysical Research: Atmospheres
volume: 118
pages: 8399-8410
title: May-September precipitation in the Bhutan Himalaya since 1743 as reconstructed from tree ring cellulose δ18O
doi: 10.1002/jgrd.50664
latitude: 27.983
longitude: 90
elevation: 3500
siteName: Wache, Bhutan
country: Bhutan
TSid: WEB588fc737
variableName: year
units: yr AD
description: calendar year in AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: WEBa8749551
variableName: d18O
units: permil
description: cellulose
basis: Instrumental calibration. The I´18O value of precipitation is negatively correlated with the amount of precipitation at low latitudes, which is known as the a€œamount effecta€
fraction: 0.36
integrationTime: 1 year
mathematicalRelation: linear
rank: 1
scope: climate
seasonality: May-Sep
variable: precipitation
variableDetail: Seasonal, annual
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: P_amount
scope: climate
scope: climate
basis: plant water is linked to precipitation, and the isotope composition of precipitation is negatively correlated with P amount
direction: positive
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: May-Sep
seasonalityOriginal: May-September
variable: precipitationIsotope
variableDetail: leaf water d18O
variableGroup: P_isotope
variableGroupDirection: positive
variableGroupOriginal: P_E
scope: isotope
variableOriginal: Precipitation_amount
scope: isotope
root
pub
pub1
geo
PaleoData columns
year (yr AD)
interpretation
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d18O (permil)
interpretation
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