CO08ABSU - v1.0.7

Dataset Id: gWwpc4lJjcaxkSJus9Ge

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R code to load dataset:

L <- lipdR::readLipd("https://lipdverse.org/data/gWwpc4lJjcaxkSJus9Ge/1_0_7/CO08ABSU.lpd")

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Download PaleoData only (csv)

Dataset changelog

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In compilations: (only most recent versions are shown)

iso2k-1_1_2

root

archiveType: Coral

originalDataUrl: https://www.ncdc.noaa.gov/paleo/study/8607

lipdVersion: 1.3

dataContributor: NJA, Polovodova,Irina

pub
pub1

author: list(name = "Abram, N.J., M.K. Gagan, J.E. Cole, W.S. Hantoro, and M. Mudelsee")

citeKey: abram2008recent

journal: Nature Geoscience

volume: 1

pages: -4

title: Recent intensification of tropical climate variability in the Indian Ocean

doi: 10.1038/ngeo357

pub2

author: list(name = "Tierney, Jessica E. , Abram, Nerilie J. , Anchukaitis, Kevin J. , Evans, Michael N. , Giry, Cyril , Kilbourne, K. Halimeda , Saenger, Casey P. , Wu, Henry C. , Zinke, Jens")

citeKey: tierney2015tropical

title: Ocean2kHR-IndianMentawaiAbram2008

doi: 10.1002/2014PA002717

geo

latitude: -0.13

longitude: 98.52

elevation: -6

siteName: Mantawai Islands, West Sumatra, Indonesia

pages2kRegion: Ocean

PaleoData columns
year (yr AD)

TSid: MAT8333f8f3fc

variableName: year

units: yr AD

description: Year AD

interpretation
1

rank: NA

scope: climate

2

rank: NA

scope: climate

3

rank: NA

scope: climate

4

rank: NA

scope: climate

5

rank: NA

scope: climate

d18O (permil)

TSid: Ocean2kHR_010_iso2k

variableName: d18O

units: permil

description: carbonate

useInGlobalTemperatureAnalysis: TRUE

interpretation
1

basis: IOD upwelling cools the ambient SST and decreases rainfall, both of which increase coral d18O.

direction: decrease/increase

interpDirection: decrease/increase

scope: climate

seasonality: subannual

variable: temperature

variableDetail: sea surface

variableGroup: temperature and salinity

2

scope: climate

3

scope: climate

4

basis: IOD upwelling cools the ambient SST and decreases rainfall, both of which increase coral d18O.

coefficient: NA

direction: negative

fraction: NA

inferredMaterial: seawater

integrationTime: 1

integrationTimeBasis: annual cycles of d18O, verified using annual growth bands

integrationTimeUncertainty: 1/12-1/6

integrationTimeUncertaintyType: chronological

integrationTimeUnits: month

mathematicalRelation: linear

rank: 1

scope: isotope

seasonality: subannual

variable: temperature

variableGroup: Temperature

variableGroupDirection: negative

variableGroupOriginal: T_water

5

basis: IOD upwelling cools the ambient SST and decreases rainfall, both of which increase coral d18O.

coefficient: NA

direction: positive

fraction: NA

inferredMaterial: seawater

integrationTime: 1

integrationTimeBasis: annual cycles of d18O, verified using annual growth bands

integrationTimeUncertainty: 1/12-1/6

integrationTimeUncertaintyType: chronological

integrationTimeUnits: month

mathematicalRelation: linear

rank: 2

scope: isotope

variable: seawaterIsotope

variableGroup: EffectiveMoisture

variableGroupDirection: negative

variableGroupOriginal: d18O_seawater

6

coefficient: NA

fraction: NA

rank: NA

scope: isotope