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The Last 2,000 Years
Multi-Millennial
Dendroclimatic Studies from the Western United States
Hughes,
Malcolm K. and Graumlich, Lisa J.
Complete Scientific Reference
Data
from this study archived at the WDC Paleoclimatology include
the raw precipitation reconstruction and filtered precipitation reconstruction plus a description of the reconstruction , as
well as the ringwidth measurements and standardized chronology for the Methuselah Walk tree
ring site.
Summary:
An extensive network of tree ring chronologies of greater than
1000 years in length exists for the western United States. This
multi-millennial-length tree ring chronology network provides
an excellent opportunity to study decadal to century scale variability
in pre-instrumental times. There are now 80 long chronologies
available that are sensitive to a wide variety of environmental
variables, including warm season temperature and winter precipitation.
In
this study, 7979 years of annual (July-June) precipitation were
reconstructed from bristlecone pine in the White Mountains of
eastern California. The graph to the right shows a comparison
between the instrumental (in blue) and reconstructed (in red)
precipitation records. The reconstruction documents the
occurrence of eight multi-decadal droughts, with the two most
recent centered on A.D. 924 and A.D. 1299. The graph below shows
the record since AD 1. The occurrence of these two droughts is
validated by an independent lake-level record from the neighboring
Sierra Nevada Mountains. The timing of coinciding low lake levels
from the Mono Lake record (Stine 1994)
is
shown by the yellow bars. Droughts of this character, were they
to occur today, would clearly have a devastating impact. Future
work will focus on expanding the multi-millennial record of drought
from tree rings and determining forcing mechanisms for these
droughts.
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