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L <- lipdR::readLipd("https://lipdverse.org/data/B9haOeIr3qeK8wIiHHfI/1_0_7/TR12SAMU.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: Sano M.
doi: 10.1029/2012JD017749
latitude: 21.67
longitude: 104.1
elevation: 1850
siteName: Mu Cang Chai, Northern Vietnam
TSid: MAT1f7cb77c97
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: TR12SAMU06
variableName: d18O
units: permil
description: cellulose
basis: As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched d18O in tree rings?..moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor...Although the mechanisms underlying variations in tree ring d18O can generally be attributed to d18O of source water and evaporative enrichment of leaf water d18O, in pluvial monsoon regions these effects seem to be well represented by the PDSI,
direction: negative
interpDirection: negative
scope: climate
seasonality: May-Oct
variable: effectivePrecipitation
variableDetail: Seasonal
variableGroup: PDSI
scope: climate
scope: climate
basis: As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.
direction: negative
inferredMaterial: soil water
integrationTime: 1
integrationTimeUnits: years
mathematicalRelation: Linear
rank: 1
scope: isotope
seasonality: May-Oct
seasonalityOriginal: May-October
variable: effectivePrecipitation
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: P_E
basis: calibration with instrumental record
direction: negative
mathematicalRelation: linear
rank: 2
scope: isotope
seasonality: May-Oct
seasonalityOriginal: May-October
variable: precipitation
variableGroup: P
variableOriginal: Precipitation_amount
direction: positive
mathematicalRelation: linear
rank: 3
scope: isotope
seasonality: May-Oct
seasonalityOriginal: May-October
variable: temperature
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T_air
TSid: TR12SAMU01
variableName: d18O
units: permil
description: cellulose
basis: As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched d18O in tree rings?..moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor...Although the mechanisms underlying variations in tree ring d18O can generally be attributed to d18O of source water and evaporative enrichment of leaf water d18O, in pluvial monsoon regions these effects seem to be well represented by the PDSI,
direction: negative
interpDirection: negative
scope: climate
seasonality: May-Oct
variable: effectivePrecipitation
variableDetail: Seasonal
variableGroup: PDSI
scope: climate
scope: climate
basis: As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.
direction: negative
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: May-Oct
seasonalityOriginal: May-October
variable: effectivePrecipitation
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: P_E
scope: isotope
seasonalityOriginal: May-October
variableOriginal: Precipitation_amount
scope: isotope
seasonalityOriginal: May-October
TSid: TR12SAMU02
variableName: d18O
units: permil
description: cellulose
basis: As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched d18O in tree rings?..moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor...Although the mechanisms underlying variations in tree ring d18O can generally be attributed to d18O of source water and evaporative enrichment of leaf water d18O, in pluvial monsoon regions these effects seem to be well represented by the PDSI,
direction: negative
interpDirection: negative
scope: climate
seasonality: May-Oct
variable: effectivePrecipitation
variableDetail: Seasonal
variableGroup: PDSI
scope: climate
scope: climate
basis: As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.
direction: negative
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: May-Oct
seasonalityOriginal: May-October
variable: effectivePrecipitation
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: P_E
scope: isotope
seasonalityOriginal: May-October
variableOriginal: Precipitation_amount
scope: isotope
seasonalityOriginal: May-October
TSid: TR12SAMU03
variableName: d18O
units: permil
description: cellulose
basis: As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched d18O in tree rings?..moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor...Although the mechanisms underlying variations in tree ring d18O can generally be attributed to d18O of source water and evaporative enrichment of leaf water d18O, in pluvial monsoon regions these effects seem to be well represented by the PDSI,
direction: negative
interpDirection: negative
scope: climate
seasonality: May-Oct
variable: effectivePrecipitation
variableDetail: Seasonal
variableGroup: PDSI
scope: climate
scope: climate
basis: As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.
direction: negative
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: May-Oct
seasonalityOriginal: May-October
variable: effectivePrecipitation
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: P_E
scope: isotope
seasonalityOriginal: May-October
variableOriginal: Precipitation_amount
scope: isotope
seasonalityOriginal: May-October
TSid: TR12SAMU04
variableName: d18O
units: permil
description: cellulose
basis: As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched d18O in tree rings?..moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor...Although the mechanisms underlying variations in tree ring d18O can generally be attributed to d18O of source water and evaporative enrichment of leaf water d18O, in pluvial monsoon regions these effects seem to be well represented by the PDSI,
direction: negative
interpDirection: negative
scope: climate
seasonality: May-Oct
variable: effectivePrecipitation
variableDetail: Seasonal
variableGroup: PDSI
scope: climate
scope: climate
basis: As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.
direction: negative
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: May-Oct
seasonalityOriginal: May-October
variable: effectivePrecipitation
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: P_E
scope: isotope
seasonalityOriginal: May-October
variableOriginal: Precipitation_amount
scope: isotope
seasonalityOriginal: May-October
TSid: TR12SAMU05
variableName: d18O
units: permil
description: cellulose
basis: As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched d18O in tree rings?..moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor...Although the mechanisms underlying variations in tree ring d18O can generally be attributed to d18O of source water and evaporative enrichment of leaf water d18O, in pluvial monsoon regions these effects seem to be well represented by the PDSI,
direction: negative
interpDirection: negative
scope: climate
seasonality: May-Oct
variable: effectivePrecipitation
variableDetail: Seasonal
variableGroup: PDSI
scope: climate
scope: climate
basis: As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.
direction: negative
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: May-Oct
seasonalityOriginal: May-October
variable: effectivePrecipitation
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: P_E
scope: isotope
seasonalityOriginal: May-October
variableOriginal: Precipitation_amount
scope: isotope
seasonalityOriginal: May-October
TSid: TR12SAMU00
variableName: d18O
units: z score
description: cellulose
basis: As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched d18O in tree rings?..moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor...Although the mechanisms underlying variations in tree ring d18O can generally be attributed to d18O of source water and evaporative enrichment of leaf water d18O, in pluvial monsoon regions these effects seem to be well represented by the PDSI,
interpDirection: negative
scope: climate
seasonality: May-Oct
variable: effectivePrecipitation
variableDetail: soil moisture
variableGroup: PDSI
rank: NA
scope: climate
rank: NA
scope: climate
basis: As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched d18O in tree rings?..moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor...Although the mechanisms underlying variations in tree ring d18O can generally be attributed to d18O of source water and evaporative enrichment of leaf water d18O, in pluvial monsoon regions these effects seem to be well represented by the PDSI,
direction: negative
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: May-Oct
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
d18O (permil)
interpretation
1
2
3
4
5
6
d18O (permil)
interpretation
1
2
3
4
5
6
d18O (permil)
interpretation
1
2
3
4
5
6
d18O (permil)
interpretation
1
2
3
4
5
6
d18O (permil)
interpretation
1
2
3
4
5
6
d18O (z score)
interpretation
1
2
3
4
5
6