Late Holocene hydrologic and climatic variability in the Walker Lake basin, Nevada and California
Yuan, Fasong  2003
A Dissertation Submitted to the State University of New York at Albany in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy
College of Arts and Sciences, Department of Earth & Atmospheric Sciences
Advisor: B.K. Linsley

Oxygen and carbon isotopic measurements of the total inorganic carbon (TIC) fraction of sediments from Walker Lake (Nevada, USA) were completed at a decadal-scale resolution spanning the last ~3000 years. On the basis of radiocarbon dating of the total organic fraction of cored sediments, the late Holocene isotope record recorded a relatively dry climate in Period LH-1 (1000 BC to AD 800), a relatively wet climate punctuated by a few severe droughts in Period LH-2 (AD 800 to 1900), and an anthropogenical perturbation era (L14-h: 1900-2000). Relative high accumulation rates in Period LH-2 (AD 800 to 1900) provided detailed information on climatic and hydrologic variability in this region. Coupled with the tree-ring-based Sacramento River flow record, the radiocarbon-based age model was refined for the interval of AD 800 through 1900. A high-resolution (3.5 year per sample) TIC delta18O record spanning the last 1200 years was generated to reflect fluctuations in winter snowfall of the Sierra Nevada. This TIC delta18O record shows two prolonged droughts that occurred during the Medieval Warm Epoch, which are chronologically well consistent with previous findings (STINF, 1994). Time series analyses on the TIC delta18O and the Sacramento River flow records reveal that interdecadal and centennial modes of climate variability persisted over the last millennium. PDO-like interdecadal oscillations that centered in the periods of 50-90 yr were almost in phase with thermal fluctuations in ocean climate of the California Current, suggesting that indedacadal climate oscillations in the Sierra Nevada were intimately linked with the Pacific dynamics. The underlying centennial to multicentennial variability corresponding to the Medieval Warm Epoch and the Little Ice Age comprise the major share of total variance. In addition, the TIC delta18O record of Walker Lake is visually well correlated with the polar ice-core-based cosmogenic nuclide production and the Rice Lake Mg/Ca records. This suggests that at least some centennial oscillations in winter precipitation of the Sierra Nevada were associated with solar activity over the last millennium.

Yuan, F., 2003. Late Holocene hydrologic and climatic variability in the Walker Lake basin, Nevada and California.
 Unpublished PhD dissertation, State University of New York at Albany. 167 pp., +xii;
University at Albany Science Library call number:  SCIENCE MIC Film QC 869 Z899 2003 Y93
Copies of this PhD dissertation can be ordered from Proquest UMI

        Front matter (title, table of contents, abstract, acknowledgements) - 0.5MB pdf file
        Figure pages (greyscale and colour figures) - 2.3MB pdf file
        Appendix 3 - Total inorganic carbon, total carbon, oxygen and carbon isotopic compositions in Walker Lake cores

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