Indo-Pacific Warm Pool (MD98-2160) Last Millennium Mg/Ca, d18O, SST, Salinity Data Newton, A.; Thunell, R.C.; Stott, L.D. Newton, A. Thunell, R.C. Stott, L.D. Other Hydroclimate Reconstruction Sea Surface Temperature Reconstruction earth science/paleoclimate/climate reconstructions|paleoceanography (delta 18O,delta 18O|magnesium/calcium|sea water,null,per mil VSMOW,null,climate reconstructions|paleoceanography,null,null,N,null) earth science/paleoclimate/paleoceanography (magnesium/calcium,Globigerinoides ruber,null,dimensionless,null,paleoceanography,null,null,N,null) earth science/paleoclimate/climate reconstructions|paleoceanography (sea surface temperature,magnesium/calcium,null,degree Celsius,null,climate reconstructions|paleoceanography,null,null,N,null) earth science/paleoclimate/climate reconstructions|paleoceanography (salinity,delta 18O|magnesium/calcium|sea surface,null,practical salinity unit,null,climate reconstructions|paleoceanography,null,null,N,null) earth science/paleoclimate/paleoceanography (age,null,null,calendar year before present,null,paleoceanography,null,null,N,null) earth science/paleoclimate/paleoceanography (depth,null,null,centimeter,null,paleoceanography,null,null,N,null) earth science/paleoclimate/paleoceanography (delta 18O,calcium carbonate,null,per mil PDB,null,paleoceanography,null,null,N,null) earth science/paleoclimate/paleocean earth science/paleoclimate/paleocean earth science/paleoclimate/paleocean earth science/paleoclimate/paleocean (MD98-2160>LATITUDE -5.2>LONGITUDE 117.48) Planktonic foraminiferal Mg/Ca and d18O derived sea surface temperature and salinity records from the Makassar Strait, Indonesia, show a long-term cooling and freshening trend, as well as considerable centennial-scale variability during the last millennium. The warmest temperatures and highest salinities occurred during the Medieval Warm Period (MWP), while the coolest temperatures and lowest salinities occurred during the Little Ice Age (LIA). These changes in the western Pacific, along with observations from other high resolution records indicate a regionally coherent southern displacement of the Inter-tropical Convergence Zone during the LIA, with more arid conditions in the northern tropics and wetter conditions in the southern tropics. NCDC-Paleoclimatology https://www.ncdc.noaa.gov/data-access/paleoclimatology-data - Bauer Bruce Investigator : Newton, A. Investigator : Thunell, R.C. Investigator : Stott, L.D. 2006-07-01 ONLINE Files online, ASCII https://www.ncdc.noaa.gov/paleo/study/5534 https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/newton2006 https://www1.ncdc.noaa.gov/pub/data/paleo/paleocean/sediment_files/complete/m98-2160-tab.txt https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/newton2006 https://www1.ncdc.noaa.gov/pub/data/paleo/paleocean/sediment_files/complete/m98-2160-tab.txt English https://www.ncdc.noaa.gov/paleo/study/5534 https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/newton2006 https://www1.ncdc.noaa.gov/pub/data/paleo/paleocean/sediment_files/complete/m98-2160-tab.txt Newton, A., R. Thunell, and L. Stott. 2006. Climate and hydrographic variability in the Indo-Pacific Warm Pool during the last millennium. Geophys. Res. Lett., 33, L19710. START YEAR: 945 14C yr BP * END YEAR: 109 14C yr BP 117.48 -5.2 117.48 -5.2