Author: Earth Institute11
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Methods Used to Reconstruct Ancient Rain Forests May Need Revision, Says Study
One way in which scientists use carbon isotopes found in fossils to identify the sites of ancient rain forests may not work as expected.
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Our Biggest, Best Event of the Year is Going Virtual
Lamont Open House at Home is four days of exciting and informative virtual earth science activities for children, families, educators, and science enthusiasts of all ages.
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Greenland on Track to Lose Ice Faster Than in Any Century Over the Last 12,000 Years
If human societies don’t sharply curb emissions of greenhouse gases, Greenland’s rate of ice loss this century is likely to greatly outpace that of any century since shortly after the end of the last ice age, a new study concludes.
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Celebrating 150 Years Since the Birth of Thomas W. Lamont
The philanthropic banker donated the estate that now houses the history-making Lamont-Doherty Earth Observatory.
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Project Will Delve Into How Climate and Tectonics Shaped Human Ancestors Over 25 Million Years
A new project will investigate the relationships between tectonics, climate and the evolution of humans’ primate ancestors in Kenya’s Turkana Basin.
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Stability Check on Antarctica Reveals High Risk for Long-Term Sea Level Rise
The warmer it gets, the faster Antarctica will lose ice, and at some point the losses will become irreversible. That is what researchers say in a new cover story in the leading journal Nature, in which they calculate how much warming the Antarctic Ice Sheet can survive.
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Warmer Temperatures Drive Arctic Greening
Using satellite images spanning decades, a new study has found that the northern tundra is becoming greener, as warmer air and soil temperatures lead to increased plant growth.
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Climate Week at the Earth Institute
Next week, September 21-27, is Climate Week in New York City. Join us for a series of online events covering the climate crisis and pointing us towards action.
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Deep Channels Linking Antarctic Glacier’s Underside to Ocean Could Hasten Melting
Newly discovered seabed channels beneath the Thwaites Glacier may be pathways for warm ocean water to melt the ice’s undersides and contribute to sea level rise.