The two Lamont-Doherty Earth Observatory scientists received funding from the Center for Climate and Life to examine the vulnerability of Greenland’s massive ice sheet.
Tag: sea level rise
Geochemist Joerg Schaefer, a Center for Climate and Life Fellow, was interviewed by PRI about his research on the instability of Greenland’s massive ice sheet.
On May 4, members of the business community gathered at a midtown Manhattan investment bank to learn how advances in climate science can be used to reduce investment risk and improve returns.
To help predict the future of sea level rise, scientists from Lamont-Doherty Earth Observatory are studying ancient corals on the island of Barbados.
Climate scientist Radley Horton is bringing the effects of sea level rise to the attention of decision-makers and fostering discussions to help society more effectively confront climate change.
Marco Tedesco and Robin Bell, polar scientists at Columbia’s Lamont-Doherty Earth Observatory polar scientists, provide a primer for non-scientists on the study of climate change as it relates to sea level changes.
The death of coral reefs is a more significant factor in the erosion of tropical coastlines than rising sea levels, says research by Lamont’s Alessio Rovere and an international team of scientists.
On May 4, 2018, the dialogue among climate scientists, engineers, and business and finance leaders will focus on “Ice Sheets and Sea Level Rise: Implications for Coastal Property.”
A new study shows that even minor deterioration of ice shelves can instantaneously hasten the decline of ice hundreds of miles landward.
Storms of intensities seen today, combined with a few meters increase in sea level, were enough to transport massive coastal boulders more than 100,000 years ago.
Volcanic eruptions have been known to cool global climate, but they can also exacerbate the melting of ice sheets, says a new study.
A new study validates that the East Antarctic ice sheet should remain stable even if the western ice sheet melts.
Robin Bell, Radley Horton, and Adam Sobel explain how their research helps make communities more resilient to extreme weather and sea level rise.
A new study found that the northeastern U.S. is at particular risk for physical and economic effects of climate hazards.
Research by geophysicist Christine McCarthy reveals how glaciers move, what makes them speed up, and how they are contributing to sea level rise as the climate warms.
The Center has awarded nearly $1 million to four scientists whose research will improve understanding of how climate change impacts the essentials of human sustainability.
Last winter, reporters from The New York Times joined Lamont scientists as they flew their mission of discovery over Antarctica.
New research offers the first comprehensive model for understanding differences in sea level rise along North America’s East Coast.
The widespread presence of seasonally flowing streams signals that the ice may be more vulnerable to melting than previously thought.
Evidence buried in Greenland’s bedrock shows that the Greenland Ice Sheet nearly disappeared for an extended time in the last million years or so.
Figuring out how far sea level rose during past warm periods in Earth’s history starts with a walk on the beach, a keen eye for evidence of ancient shorelines, and a highly accurate GPS system.
Geologist Alessio Rovere and Trinity Mensah-Senoo walk along a beach in Ghana gathering data that will be used to monitor coastal erosion.
Lamont marine geologist and paleoclimatologist Maureen Raymo studies ancient shorelines to understand how high seas rose in the past, and how high they might climb in the future.
In a new study, Lamont’s Michael Previdi and Lorenzo Polvani found that the effect of rising temperatures on snowfall in Antarctica has so far been overshadowed by the frozen continent’s large natural climate variability.
Humans have been burning fossil fuels for only about 150 years, yet that has started a cascade of changes that will still be felt 10,000 years from now.
A new study uses sediment cores to track the expansion and retreat of glaciers through time and finds they are more sensitive than realized.