Low-Latitude Western North Atlantic Climate Variability During the Past Millennium: Insights from Proxies and Models
WOODS HOLE OCEANOGRAPHIC INSTITUTION MA
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Estimates of natural climate variability during the past millennium provide a frame of reference in which to assess the significance of recent changes. This thesis investigates new methods of reconstructing low-latitude sea surface temperature SST and hydrography, and combines these methods with traditional techniques to improve the present understanding of western North Atlantic climate variability. A new strontiumcalcium SrCa - SST calibration is derived for Atlantic Montastrea corals. This calibration shows that Montastrea SrCa is a promising SST proxy if the effect of coral growth is considered. Further analyses of coral growth using Computed Axial Tomography CAT imaging indicate growth in Siderastrea corals varies inversely with SST on interannual timescales. A 440-year reconstruction of low-latitude western North Atlantic SST based on this relationship suggests the largest cooling of the last few centuries occurred from 1650-1730 A.D., and was 1 deg C cooler than today. Sporadic multidecadal variability in this record is inconsistent with evidence for a persistent 65-80 year North Atlantic SST oscillation. Volcanic and anthropogenic radiative forcing are identified as important sources of externally-forced SST variability, with the latter accounting for most of the 20th century warming trend. An 1800-year reconstruction of SST and hydrography near the Gulf Stream also suggests SSTs remained within about 1 deg C of modern values. This cooling is small relative to other regional proxy records and may reflect the influence of internal oceanic and atmospheric circulation. Simulations with an atmospheric general circulation model AGCM indicate that the magnitude of cooling estimated by proxy records is consistent with tropical hydrologic proxy records.
- Physical and Dynamic Oceanography
- Atmospheric Physics