Climate and hydrographic variability in the Indo-Pacific Warm Pool during the last millennium Export

@article{citeulike:5089996, abstract = {Planktonic foraminiferal Mg/Ca and δ 18O 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. }, author = {Newton, Alicia and Thunell, Robert and Stott, Lowell}, citeulike-article-id = {5089996}, citeulike-linkout-0 = {http://www.agu.org/pubs/crossref/2006/2006GL027234.shtml}, citeulike-linkout-1 = {http://dx.doi.org/10.1029/2006GL027234}, day = {12}, doi = {10.1029/2006GL027234}, issn = {0094-8276}, journal = {Geophysical Research Letters}, keywords = {climate, holocene, indian, itcz, millennial, natural, observations, ocean, pacific, plankton, precipitation, proxy, salinity, temperature, variation}, month = {October}, number = {19}, pages = {L19710+}, posted-at = {2009-07-07 21:08:05}, priority = {2}, title = {Climate and hydrographic variability in the Indo-Pacific Warm Pool during the last millennium}, url = {http://dx.doi.org/10.1029/2006GL027234}, volume = {33}, year = {2006} }

TY - JOUR ID - citeulike:5089996 L3 - citeulike-article-id:5089996 N2 - Planktonic foraminiferal Mg/Ca and δ 18O 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. IS - 19 JF - Geophysical Research Letters SN - 0094-8276 TI - Climate and hydrographic variability in the Indo-Pacific Warm Pool during the last millennium VL - 33 SP - L19710 KW - climate KW - holocene KW - indian KW - itcz KW - millennial KW - natural KW - observations KW - ocean KW - pacific KW - plankton KW - precipitation KW - proxy KW - salinity KW - temperature KW - variation AU - Newton, Alicia AU - Thunell, Robert AU - Stott, Lowell PY - 2006/10/12/ UR - http://dx.doi.org/10.1029/2006GL027234 ER -