L <- lipdR::readLipd("https://lipdverse.org/data/SwJhjCbLxX0uQiNBHJc7/1_0_7/CO97CHSY.lpd")Report an issue (include datasetId and version)
In compilations: (only most recent versions are shown)
iso2k-1_1_2
archiveType: Coral
originalDataUrl: https://www.ncdc.noaa.gov/paleo/study/1857
lipdVersion: 1.3
dataContributor: JZ
author: list(name = "Charles, C.D., D.E.Hunter, and R.G.Fairbanks.")
citeKey: charles1997interaction
journal: Science
volume: 277
pages: -3
title: Interaction Between the ENSO and the Asian Monsoon in a Coral Record of Tropical Climate
doi: 10.1126/science.277.5328.925
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-IndianSeychellesCharles1997
doi: 10.1002/2014PA002717
latitude: -4.6062
longitude: 55.4244
elevation: -7
siteName: Beau Vallon Bay, Mahe Island, Republic of the Seychelles
pages2kRegion: Ocean
TSid: MATb8b3cd2a90
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: Ocean2kHR_011_iso2k
variableName: d18O
units: permil
description: carbonate
useInGlobalTemperatureAnalysis: TRUE
basis: Authors suggest that ENSO dominates d18O variations on interannual timescales, while the Asian monsoon system drives decadal variability in d18O at this site
direction: decrease/increase
interpDirection: decrease/increase
scope: climate
seasonality: subannual
variable: temperature
variableDetail: sea surface
variableGroup: temperature and salinity
scope: climate
scope: climate
basis: At the Seychelles, however, one would expect the seasonal temperature variability (of more than 2i¿½C) to dominate the nearly constant d18O of seawater
coefficient: NA
direction: negative
fraction: NA
inferredMaterial: seawater
integrationTime: 1
integrationTimeBasis: used the d18O cycle to count annual layers; assigned the high d18O extremes to Aug 1 of every year and interpolated linearly between these tie points. The largest d18O anomaly (late 1877) matches the most catastrophic monsoon failure on record
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
basis: Furthermore, correspondence with an independent index of monsoon strength demonstrates that the coral successfully captures the large-scale aspects of Asian monsoon behavior
coefficient: NA
direction: positive
fraction: NA
inferredMaterial: seawater
integrationTime: 1
integrationTimeBasis: used the d18O cycle to count annual layers; assigned the high d18O extremes to Aug 1 of every year and interpolated linearly between these tie points. The largest d18O anomaly (late 1877) matches the most catastrophic monsoon failure on record
integrationTimeUncertainty: 1/12-1/6
integrationTimeUncertaintyType: chronological
integrationTimeUnits: month
mathematicalRelation: linear
rank: 2
scope: isotope
seasonality: Wet Season
variable: seawaterIsotope
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: d18O_seawater
coefficient: NA
fraction: NA
rank: NA
scope: isotope
root
pub
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geo
PaleoData columns
year (yr AD)
interpretation
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2
3
4
5
d18O (permil)
interpretation
1
2
3
4
5
6