Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/148881
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dc.contributor.authorRamos, R. D.en_US
dc.contributor.authorGoodkin, Nathalie Fairbanken_US
dc.contributor.authorFan, Tung Yungen_US
dc.date.accessioned2021-06-04T03:13:09Z-
dc.date.available2021-06-04T03:13:09Z-
dc.date.issued2020-
dc.identifier.citationRamos, R. D., Goodkin, N. F. & Fan, T. Y. (2020). Coral records at the northern edge of the Western Pacific warm pool reveal multiple drivers of sea surface temperature, salinity, and rainfall variability since the end of the Little Ice Age. Paleoceanography and Paleoclimatology, 35(5), e2019PA003826-. https://dx.doi.org/10.1029/2019PA003826en_US
dc.identifier.issn2572-4525en_US
dc.identifier.other0000-0003-2584-5336-
dc.identifier.other0000-0001-9697-5520-
dc.identifier.urihttps://hdl.handle.net/10356/148881-
dc.description.abstractReconstructions of key climate parameters prior to anthropogenic influences serve to constrain decadal to multicentury natural climate variability. In the western Pacific region, relatively few reconstructions exist north of the Western Pacific Warm Pool (WPWP), a region critical to global climate. In this study, we collected a coral core from Houbihu, southern Taiwan, and generated a 225-year reconstruction of annual and wintertime sea surface temperature, dry season sea surface salinity, and wet season rainfall records derived from paired Porites Sr/Ca and δ O profiles extending back to the end of the Little Ice Age (1850 CE). Multidecadal sea surface temperature trends generally track regional surface temperature reconstructions, indicating the dominant influence of solar and volcanic radiative forcings. Reconstructed dry season sea surface salinity reflects an advection signal linked to the East Asian Winter Monsoon and the Pacific Decadal Oscillation, both influencing variations in the Kuroshio Intrusion across the Luzon Strait. Reconstructed wet season rainfall, on the other hand, reveals influence of the Pacific Decadal Oscillation on the decadal variability of local and regional rainfall patterns. Relative to the late 1900s, our climate reconstructions document cooler and drier (high salinity and low rainfall) conditions during the end of the Little Ice Age, supporting other lines of evidence of a retracted WPWP region during this period. In the late 20th to early 21st century, our climate reconstructions record warming and freshening (low salinity and high rainfall) trends, highlighting the potential impact of anthropogenic forcing in the extension of the WPWP.en_US
dc.description.sponsorshipMinistry of Education (MOE)en_US
dc.description.sponsorshipNational Research Foundation (NRF)en_US
dc.language.isoenen_US
dc.relationNRF-RF2012-03en_US
dc.relationMOE2016-T2-1-016en_US
dc.relation.ispartofPaleoceanography and Paleoclimatologyen_US
dc.rights©2020 The Author(s). This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.en_US
dc.subjectScience::Geologyen_US
dc.titleCoral records at the northern edge of the Western Pacific warm pool reveal multiple drivers of sea surface temperature, salinity, and rainfall variability since the end of the Little Ice Ageen_US
dc.typeJournal Articleen
dc.contributor.researchEarth Observatory of Singaporeen_US
dc.identifier.doi10.1029/2019PA003826-
dc.description.versionPublished versionen_US
dc.identifier.scopus2-s2.0-85085300475-
dc.identifier.issue5en_US
dc.identifier.volume35en_US
dc.identifier.spagee2019PA003826en_US
dc.subject.keywordsCoralen_US
dc.subject.keywordsWestern Pacic Warm Poolen_US
dc.description.acknowledgementThis research was funded by the National Research Foundation Singapore under its Singapore NRF Fellowship scheme awarded to N. F. Goodkin (National Research Fellow Award NRF-RF2012-03), as administered by the Earth Observatory of Singapore and the Singapore Ministry of Education under the Research Centres of Excellence initiative and by the Ministry of Education, Singapore, through its Academic Research Fund Tier 2 (Project MOE2016-T2-1-016). The coral Sr/Ca and δ18O data generated in this study are available in supporting information Data Set S1 and are archived at the NOAA NCDC World Data Center for Paleoclimatology (https://www.ncdc.noaa.gov/paleo/study/29412).en_US
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