What is noteworthy about this item is that it picks up independently and strongly the 1150 years long cycle that I had spoken to regarding the
onslaught of cold spells. The cycle may well be real after all.
Something brings it on in a powerful manner and this is likely a
natural balancing mechanism between the Antarctic and the Arctic that
we know nothing about yet.
Recently it has been noted that the cold waters of the antarctic deep
have shrunken an alarming sixty percent. This could be a decadal
cycle that every thousand years goes over the top and chills the Gulf
Stream. Fortunately, it is too soon yet for all alarmists out there.
They have to wait another eight hundred years.
In the meantime we have a pretty sharp confirmation of a climatic
event that lasted centuries and surely reflects global climatic
arrangements.
Sierra Nevada 200
year megadroughts confirmed
by Staff Writers
Reno NV (SPX) Jun 07, 2012
University of Nevada,
Reno, researchers were joined by a Scripps Institution of
Oceanography research team, spending many days on Fallen Leaf Lake to
gather sonar and side-scan radar data to study earthquake faults and
paleoshorelines. The low-tech boat was adorned with high-tech
hardware, such as gyroscopes used on rockets, to gather
high-resolution images of the lake bottom. Using standing trees they
found submerged under 130 feet of water, the team confirmed and
reported in their paper, a culmination of a comprehensive high-tech
assessment of Fallen Leaf Lake - a small moraine-bound lake at the
south end of the Lake Tahoe Basin - that stands of pre-Medieval trees
in the lake suggest the region experienced severe drought at least
every 650 to 1,150 years during the mid- and late-Holocene period.
Credit: Photo by Mike Wolterbeek, University of Nevada, Reno.
The
erratic year-to-year swings in precipitation totals in the Reno-Tahoe
area conjures up the word "drought" every couple of years,
and this year is no exception. The Nevada State Climate Office at the
University of Nevada, Reno, in conjunction with the Nevada Drought
Response Committee, just announced a Stage 1 drought (moderate) for
six counties and a Stage 2 drought (severe) for 11 counties.
Reno,
Lake Tahoe and the Sierra Nevada are no strangers to drought, the
most famous being the Medieval megadrought lasting from 800 to
1250 A.D. when annual precipitation was less than 60 percent of
normal. The Reno-Tahoe region is now about 65 percent of annual
normal precipitation for the year, which doesn't seem like much, but
imagine if this were the "norm" each and every year for the
next 200 years.
Research by scientists
at the University of Nevada, Reno and their partners at Scripps
Institution of Oceanography in San Diego indicates that there are
other instances of such long-lasting, severe droughts in the western
United States throughout history.
Their recent paper, a
culmination of a comprehensive high-tech assessment of Fallen Leaf
Lake - a small moraine-bound lake at the south end of the Lake Tahoe
Basin - reports that stands of pre-Medieval trees in the lake
suggest the region experienced severe drought at least every 650 to
1,150 years during the mid- and late-Holocene period.
"Using an arsenal
of cutting edge sonar tools, remotely operated vehicles (ROVs), and a
manned submersible, we've obtained potentially the most accurate
record thus far on the instances of 200-year-long droughts in the
Sierra," Graham Kent, director of the Nevada Seismological
Laboratory said.
"The record from
Fallen Leaf Lake confirms what was expected and is likely the most
accurate record, in terms of precipitation, than obtained previously
from a variety of methods throughout the Sierra."
Kent is part of the
University of Nevada, Reno and Scripps research team that traced the
megadroughts and dry spells of the region using tree-ring analysis,
shoreline records and sediment deposition in Fallen Leaf Lake.
Using side-scan and
multibeam sonar technology developed to map underwater earthquake
fault lines such as the West Tahoe fault beneath Fallen Leaf Lake,
the team also imaged standing trees up to 130 feet beneath the lake
surface as well as submerged ancient shoreline structure and
development.
The trees matured
while the lake level was 130 to 200 feet below its modern elevation
and were not deposited by a landslide as was suspected.
The team, led by John
Kleppe, University of Nevada, Reno engineering professor emeritus,
published a paper on this research and is presenting its findings in
seminars and workshops.
"The lake is like
a 'canary in a coal mine' for the Sierra, telling the story of
precipitation very clearly," Kent said.
"Fallen Leaf Lake
elevations change rapidly due to its unique ratio between catchment
basin and lake surface of about 8 to 1. With analysis of the standing
trees submerged in the lake, sediment cores and our sonar scanning of
ancient shorelines, we can more accurately and easily trace the
precipitation history of the region."
Water balance
calculations and analysis of tree-ring samples undertaken by Kleppe,
Kent and Scripps scientists Danny Brothers and Neal Driscoll, along
with Professor Franco Biondi of the University's College of Science,
suggest annual precipitation was less than 60 percent of normal from
the late 10th century to the early 13th century.
Their research was
documented in a scientific paper, Duration and severity of Medieval
drought in the Lake Tahoe Basin, published in the Quaternary Science
Reviews in November 2011.
Tree-ring records and
submerged paleoshoreline geomorphology suggest a Medieval low-lake
level of Fallen Leaf Lake lasted more than 220 years. More than 80
trees were found lying on the lake floor at various elevations above
the paleoshoreline.
"Although the
ancient cycle of megadroughts seems to occur every 650 to 1150 years
and the last one was 750 years ago, it is uncertain when the next
megadrought will occur. With climate change upon us, it will be
interesting to see how carbon dioxide loading in the atmosphere will
affect this cycle," Kent said.
Professor Paula Noble,
in the University's College of Science's Department of Geological
Sciences and Engineering, is expanding this research to include the
fine-scale study of climate change through out the Holocene (about
12,000 years) using recently collected 40-foot-long sediment cores in
Fallen Leaf Lake.
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