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L <- lipdR::readLipd("https://lipdverse.org/data/6nHzeIAXoyT3cj8Ty99A/1_0_7/TR07RECA.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: Reynolds-Henne
doi: 10.1029/2007GB002945
latitude: 46.35
longitude: 8.6
elevation: 900
siteName: Cavergno, Switzerland
TSid: MATad36c816e2
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: TR07RECA01
variableName: d18O
units: permil
description: cellulose
direction: negative (P_amount); positive (temperature)
scope: climate
seasonality: Summer
variable: precipitation
variableDetail: Seasonal
variableGroup: P_amount and temperature
scope: climate
scope: climate
basis: Correlations with 18O of precipitation (GNIP data) showed that source water signals are preserved in d18O tree rings. A possible explanation for the common decadal-to century scale trends, not directly related to mean monthly air temperature or precipitation amount, is variations in moisture source determined by the dominant atmospheric circulation pattern. The NAO index, determinates diminant wind pattern and temperature, and precipitation systems over Europe and influences d18O precipitation in Switzerland.
direction: positive
inferredMaterial: precipitation
integrationTime: 1
integrationTimeUnits: years
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: May-Jun
seasonalityOriginal: P_amount (May, June), T_air (June, July, August,September)
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
scope: isotope
variableGroupOriginal: P_E
scope: isotope
root
pub
pub1
geo
PaleoData columns
year (yr AD)
interpretation
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d18O (permil)
interpretation
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