{"NOAAStudyId":"19806","contactInfo":{"address":"325 Broadway, E/NE31","city":"Boulder","constraints":"Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site.","country":"USA","dataCenterUrl":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data","email":"paleo@noaa.gov","fax":"303-497-6513","longName":"National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce ","phone":"303-497-6280","postalCode":"80305-3328","shortName":"DOC/NOAA/NESDIS/NCEI","state":"CO","type":"CONTACT INFORMATION"},"contributionDate":"2016-02-24","dataPublisher":"NOAA","dataType":"SPELEOTHEMS","dataTypeInformation":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets/speleothem","difMetadataLink":"http://www1.ncdc.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-cave-19806.xml","doi":null,"earliestYearBP":161533,"earliestYearCE":-159583,"entryId":"noaa-cave-19806","funding":[{"fundingAgency":"US National Science Foundation","fundingGrant":"645291, 1502830, 903099"}],"investigators":"Carolin, S.A.; Cobb, K.M.; Lynch-Stieglitz, J.; Moerman, J.W.; Partin, J.W.; Lejau, S.; Malang, J.; Clark, B.; Tuen, A.A.; Adkins, J.F.","mostRecentYearBP":-55,"mostRecentYearCE":2005,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/19806","originalSource":null,"publication":[{"abstract":null,"author":{"name":"Stacy A. Carolin, Kim M. Cobb, Jess F. Adkins, Brian Clark, Jessica L. Conroy, Syria Lejau, Jenny Malang, Andrew A. Tuen"},"citation":"Stacy A. Carolin, Kim M. Cobb, Jess F. Adkins, Brian Clark, Jessica L. Conroy, Syria Lejau, Jenny Malang, Andrew A. Tuen. 2013. Varied Response of Western Pacific Hydrology to Climate Forcings over the Last Glacial Period. Science, 340(6140), 1564-1566. doi: 10.1126/science.1233797","edition":null,"identifier":{"id":"10.1126/science.1233797","type":"doi","url":"http://dx.doi.org/10.1126/science.1233797"},"issue":"6140","journal":"Science","pages":"1564-1566","pubRank":"2","pubYear":2013,"reportNumber":null,"title":"Varied Response of Western Pacific Hydrology to Climate Forcings over the Last Glacial Period","type":"publication","volume":"340"},{"abstract":"Over the past decades, tropical stalagmite d18O records have provided valuable insight on glacial and interglacial hydrological variability and its relationship to a variety of natural climate forcings. The transition out of the penultimate glaciation (MIS 6) represents an important target for tropical hydroclimate reconstructions, yet relatively few such reconstructions resolve this transition. Particularly, comparisons between Termination 1 and 2 provide critical insight on the extent and influence of proposed climate mechanisms determined from paleorecords and model experiments spanning the recent deglaciation. Here we present a new compilation of western tropical Pacific hydrology spanning 0-160 kyBP, constructed from eleven different U/Th-dated stalagmite d18O records from Gunung Mulu National Park in northern Borneo. The reconstruction exhibits significant precessional power in phase with boreal fall insolation strength over the 0-160 ky BP period, identifying precessional insolation forcing as the dominant driver of hydroclimate variability in northern Borneo on orbital timescales. A comparison with a network of paleoclimate records from the circum-Pacific suggests the insolation sensitivity may arise from changes in the Walker circulation system. Distinct millennial-scale increases in stalagmite d18O, indicative of reduced regional convection, occur within glacial terminations and may reflect a response to shifts in inter-hemispheric temperature gradients. Our results imply that hydroclimate in this region is sensitive to external forcing, with a response dominated by large-scale temperature gradients.","author":{"name":"Stacy A. Carolin, Kim M. Cobb, Jean Lynch-Stieglitz, Jessica W. Moerman, Judson W. Partin, Syria Lejau, Jenny Malang, Brian Clark, Andrew A. Tuen, Jess F. Adkins"},"citation":"Stacy A. Carolin, Kim M. Cobb, Jean Lynch-Stieglitz, Jessica W. Moerman, Judson W. Partin, Syria Lejau, Jenny Malang, Brian Clark, Andrew A. Tuen, Jess F. Adkins. 2016. Northern Borneo stalagmite records reveal West Pacific hydroclimate across MIS 5 and 6. Earth and Planetary Science Letters, 439, 182-193. doi: 10.1016/j.epsl.2016.01.028","edition":null,"identifier":{"id":"10.1016/j.epsl.2016.01.028","type":"doi","url":"http://dx.doi.org/10.1016/j.epsl.2016.01.028"},"issue":null,"journal":"Earth and Planetary Science Letters","pages":"182-193","pubRank":"1","pubYear":2016,"reportNumber":null,"title":"Northern Borneo stalagmite records reveal West Pacific hydroclimate across MIS 5 and 6","type":"publication","volume":"439"}],"reconstruction":"N","scienceKeywords":null,"site":[{"NOAASiteId":"53294","geo":{"geoType":"Feature","geometry":{"coordinates":["4.15","114.8667"],"type":"POINT"},"properties":{"easternmostLongitude":"114.8667","maxElevationMeters":"250","minElevationMeters":"250","northernmostLatitude":"4.15","southernmostLatitude":"4.15","westernmostLongitude":"114.8667"}},"locationName":"Ocean>Indian Ocean>Malaysia","mappable":"Y","paleoData":[{"NOAADataTableId":"30474","coreLengthMeters":null,"dataFile":[{"NOAAKeywords":["earth 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