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temperature in the surrounding seawater", "direction": "decrease/increase", "interpDirection": "decrease/increase", "scope": "climate", "seasonality": "subannual", "variable": "temperature", "variableDetail": "sea surface", "variableGroup": "temperature and salinity", "dynamical": null }, { "scope": "climate", "basis": null, "direction": null, "seasonality": null, "variable": null, "variableDetail": null }, { "scope": "climate", "basis": null, "direction": null, "seasonality": null, "variable": null, "variableDetail": null }, { "basis": "The annual variability of the Bunaken coral d18O refects the seasonal cycle of both salinity and temperature in the surrounding seawater. The characteristics and correlations of the Bunaken Island coral d18O record strongly suggestthat it monitors the air-sea interaction associatedwith Southeast Asian summer monsoon.", "coefficient": "NA", "direction": "positive", "fraction": "NA", "inferredMaterial": "seawater", "integrationTime": "1", "integrationTimeBasis": "anchoring seasonal maxima and minima of the d18O depth series to March and October of each year. Crosschecks on the age assignments were available through examination of the annual growth bands and the strong semi-annual carbon isotope signal", "integrationTimeUncertainty": "~1/4", "integrationTimeUncertaintyType": "chronological", "integrationTimeUnits": "month", "mathematicalRelation": "linear", "rank": 1, "scope": "isotope", "seasonality": "subannual", "variable": "seawaterIsotope", "variableGroup": "EffectiveMoisture", "variableGroupDirection": "negative", "variableGroupOriginal": "d18O_seawater" }, { "basis": "The annual variability of the Bunaken coral d18O refects the seasonal cycle of both salinity and temperature in the surrounding seawater: \"in the Indonesian coral records, coral d18O is more heavily infuenced by rainfall variability.\" The characteristics and correlations of the Bunaken Island coral d18O record strongly suggestthat it monitors the air-sea interaction associatedwith Southeast Asian summer monsoon.", "coefficient": "NA", "direction": "negative", "fraction": "NA", "inferredMaterial": "seawater", "integrationTime": "1", "integrationTimeBasis": "anchoring seasonal maxima and minima of the d18O depth series to March and October of each year. 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D., Cobb, K., Moore, M. D. and Fairbanks, R. G.: Monsoon–tropical ocean interaction in a network of coral records spanning the 20th century, Marine Geology, 201(1-3), 207–222, doi:10.1016/s0025-3227(03)00217-2, 2003.", "citeKey": "charles2003monsoon", "dataUrl": "doi.org", "doi": "10.1016/S0025-3227(03)00217-2", "issue": -2, "journal": "Marine Geology", "pages": -15, "publisher": "Elsevier BV", "title": "Monsoon?tropical ocean interaction in a network of coral records spanning the 20th century", "type": "journal-article", "volume": 201, "year": 2003 }, { "author": { "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" }, "citation": "Tierney, J. E., Abram, N. J., Anchukaitis, K. J., Evans, M. N., Giry, C., Kilbourne, K. H., Saenger, C. P., Wu, H. C. and Zinke, J.: Tropical sea surface temperatures for the past four centuries reconstructed from coral archives, Paleoceanography, 30(3), 226–252, doi:10.1002/2014pa002717, 2015.", "citeKey": "tierney2015tropical", "doi": "10.1002/2014PA002717", "institution": "World Data Center for Paleoclimatology", "title": "Ocean2kHR-PacificBunakenCharles2003", "type": "dataCitation", "url": "https://www.ncdc.noaa.gov/paleo/study/1903", "year": 2015 } ], "geo": { "longitude": 124.833, "latitude": -1.5, "elevation": -3, "geometryType": "Point", "ocean": "Pacific", "pages2kRegion": "Ocean", "siteName": "Bunaken Island" }, "@context": "context.jsonld" }