(First published on Feb. 14, 2017, on State of the Planet.)
Aaron Putnam sits atop a boulder high in the Sierras of central California, banging away with hammer and chisel to chip out a sample of ice age history. Each hunk of rock is a piece of a vast puzzle: How did our climate system behave the last time it warmed up like it’s doing today?
Filed under Science, Climate
This post was first published on Dec. 6, 2013, on the Earth Institute’s State of the Planet blog. It was updated on Oct. 14, 2014 (see below).
Guleed Ali pauses to study his notebook, standing on a steep slope covered in gray volcanic ash and desert brush, high above the present-day shore of Mono Lake in eastern California. He looks across the slope to where, a few hundred yards away, a gash of lighter gray sediment cuts across the hill, then disappears. The exposed sediment is history: A record of deposits left by Mono Lake when it stood far higher than today.
Ali picks a spot, hefts his shovel and begins clawing into the slope, raising puffs of dust, searching for a missing page in that sediment history: something higher upslope, evidence of the stream that would have fed the prehistoric lake: a layer of gravel. He finds only sand – perhaps an ancient beach. He moves across the slope, lifts and plunges his shovel back into the soft hillside.
By studying stream bed sediments, Guleed Ali tries to build a history of how water levels have changed at Mono Lake. Photo: D. Funkhouser
He is digging for dates, looking back tens of thousands of years into the last ice age: When was the lake higher? When did it shrink, and grow again? How does that chronology correspond with the advance and retreat of the massive ice sheets that covered much of North America? And how did the lake’s levels respond to changing climate?
Understanding that past will help scientists like Ali, a PhD student at Lamont-Doherty Earth Observatory, project what might happen in the future as the world warms up. This is no esoteric question for Los Angeles, whose nearly 4 million people depend in part on Mono Lake’s watershed for drinking water, green lawns, agriculture and industry.
This story was first posted on the Earth Institute’s State of the Planet blog on Feb. 15, 2013.
The drought that afflicts the U.S. Southwest has been going on for more than a decade, but if the distant past is any guide, the region could be in for much worse.
Extreme weather and climate-related events already have cost the United States billions of dollars. Speakers at a symposium Friday focused on the hard facts of what we know and don’t know about the causes, and how changing climate affects agriculture, water supplies, wildlife and our economy. The panel was part of the 2013 annual meeting of the American Association for the Advancement of Science, being held in Boston.
The drought offers an example of how difficult is can be to tease out the impacts of human-induced climate change from those of natural climate variations.
Filed under Climate, Stories