A newly developed chronology of annual varve thickness (AD
1117-1992) from Santa Barbara Basin has been decomposed into
orthogonal components using singular spectrum analysis (SSA)
to identify and retrieve inter-decadal oscillations. After
removing all variability with periods greater than 150 years,
leading SSA eigenfunctions (EOFs) identify four oscillatory
pairs with periods of
,
,
, and
years
respectively. Based on 2500 simulated series and on two-sided
confidence intervals, EOFs 1-7 are significant at the 99%
level and EOFs 8-9 are significant at the 90% level.
Oscillatory signals retrieved from the marine varves show
an abrupt change in frequency and amplitude near AD 1600.
The largest contribution to this environmental shift is
given by the interdecadal components, especially the
and the
-year oscillation, suggesting a connection with
global-scale decadal cycles identified in the subtropical
Pacific gyre circulation and, possibly, with solar-driven
phenomena. The near-AD 1600 change identified in the varve
record may be related to multi-annual events reported for the
nearby Santa Monica Basin and for forest ecosystems of the
American Southwest.
AGU Index Terms: 4267 Paleoceanography; 3344 Paleoclimatology; 1620 Climate dynamics; 4221 Dendrochronology
Keywords/Free Terms: Paleoclimatology, climate dynamics, dendrochronology, Santa Barbara Basin.
Geophysical Res. Ltrs. 96GL03813
Vol. 24
, No. 2
, p. 193