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L <- lipdR::readLipd("https://lipdverse.org/data/BJGQj35W3JO10WXQY5CX/1_0_7/TR18XUJA00.lpd")Report an issue (include datasetId and version)
In compilations: (only most recent versions are shown)
iso2k-1_1_0
archiveType: Wood
originalDataUrl: https://www1.ncdc.noaa.gov/pub/data/paleo/treering/isotope/asia/india/jageshwar2018d18o.txt
lipdVersion: 1.3
author: Xu C.
journal: Climate of the Past Discussions
pages: 1-31
title: Decreasing Indian summer monsoon in northern Indian sub-continent during the last 180 years: evidence from five tree cellulose oxygen isotope chronologies
doi: 10.5194/cp-14-653
latitude: 29.633
longitude: 79.85
elevation: 3849
siteName: Jageshwar
country: India
TSid: WEB10836628
variableName: year
units: yr AD
description: calendar year in AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: WEB0738fe31
variableName: d18O
units: permil
description: cellulose
basis: PDSI reflects the soil moisture stress which is an integrated effect of the precipitation and temperature
direction: negative
fraction: 0.25
integrationTime: 1 year
integrationTimeBasis: annual rings
mathematicalRelation: linear
rank: 1
scope: climate
seasonality: Jun-Sep
variable: effectivePrecipitation
variableDetail: Seasonal
variableGroup: PDSI
scope: climate
scope: climate
basis: In the monsoon season, high temperature usually indicates less rainfall and low relative humidity, which can make the tree ring cellulose d18O heavier. Low PDSI indicates a dry condition.
direction: negative
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Jun-Sep
seasonalityOriginal: June-September
variable: effectivePrecipitation
variableDetail: d18O of the leaf water
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