University of Wollongong Research Online Faculty of Science - Honours Theses (Archive) University of Wollongong Thesis Collections 2011 Holocene changes in mean sea-surface temperatures from Central Pacific fossil microatolls Harrison John Schofield University of Wollongong Recommended Citation Schofield, Harrison John, Holocene changes in mean sea-surface temperatures from Central Pacific fossil microatolls, Bachelor of Science (Honours), School of Earth & Environmental Sciences, University of Wollongong, 2011. http://ro.uow.edu.au/thsci/1 Research Online is the open access institutional repository for the University of Wollongong. For further information contact the UOW Library:
[email protected] Holocene changes in mean sea-surface temperatures from Central Pacific fossil microatolls Abstract The quae torial Pacific ase t-west sea surface temperature (SST) gradient (SST gradient) is a dynamic component of the El Niño Southern Oscillation (ENSO) and is a key determinant of global climate patterns. The ST gradient, which is averaged over decades to millennia, is a major component of the Pacific mean state, and changes in its strength are related to ENSO variability. Understanding the interaction between Pacific ST gradient and ENSO is important because changes in mean SSTs are projected to alter the Pacific mean SST gradient, but it is not clear what impact this will have on ENSO. By investigating the historical relationship between these two parameters, a better understanding of the interaction between the SST gradient and ENSO can be gained. Studies of climate of the past 10 thousand years (kyr) have documented changes in ENSO, yet little is known about the major components of the Pacific mean state, including the mean SST gradient.