Sept.
6 (UPI)
-- Human-caused global warming is happening at an unprecedented rate, but a few
instances of historic climate change provide insights into how rising
temperature might impact Earth's systems.
New analysis of one of those instances,
the so-called Palaeocene-Eocene Thermal Maximum, suggests rapid global
temperature increases can transform hydrologic cycles.
"Our study proves that the risks
associated with global warming may be far greater than we generally
think," Sebastien Castelltort, climate scientist at the University of
Geneva, said in a news release.
Beginning 56 million years ago, during
the Palaeocene-Eocene Thermal Maximum -- a period between the Palaeocene and
Eocene epochs, lasting 10,000 to 20,000 years -- temperatures rose between 5
and 8 degrees Celsius.
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Using the analysis of ancient sediment
cores, scientists analyzed the effects of this dramatic rise in temperature on
hydrologic cycles.
Previous studies have charted the rise
in temperature during Palaeocene-Eocene Thermal Maximum, or PETM. Castelltort
and his colleagues analyzed evidence of shifting river dynamics in the Spanish
Pyrenees during the same time period.
The analysis of pebbles in ancient
sediment cores allowed researchers to estimate the flow velocity and discharge
in the river system. At the beginning the of the PETM, river channels deposited
fertile alluvium in the floodplain at the foothills of the Pyrenees. The
deposits encouraged the growth of rich vegetation.
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As temperature rose during the PETM, the
system's dynamics shifted dramatically. Rising temperatures increased the
severity and frequency of flooding by a factor of 14. The sudden change caused
fertile alluvium to be carried directly to the ocean, bypassing the floodplain.
As a result of the change in sediment
deposition patterns, vegetation disappeared from the Pyrenees foothills. The
region was transformed into an arid expanse of gravel.
Scientists suggest their findings --
published this week in the journal Scientific
Reports -- offer a reminder that researchers still understand very
little about the repercussions and consequences of dramatic changes to
hydrologic cycles.
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