Ancient ice reveals sudden climate shift
From deep within Greenland's ice cap, investigators have retrieved signs that the North Atlantic region took fewer than 20 years to shift from glacial conditions to warmer ones at the end of the last ice age. The discovery underscores the possibility that a similarly dramatic climate swing lies just around the greenhouse corner.
Previous studies suggested that the ice age's final cold spell, called the Younger Dryas, ended abruptly around 10,700 years ago. The refined analysis of a deep ice core from south Greenland reveals the extreme speed of the transition to a milder, less stormy climate.
As it emerged from the ice age, the North Atlantic bounced between several warm and cold times. The Younger Dryas period, which started around 11,500 years ago according to ice core dates, marked the last time this region slipped back into glacial conditions. The system of ocean currents that warms Europe ceased operating, and sea ice covered much of the North Atlantic during this period.
Greenland's ice cap, which builds layer by layer each year, provides a climatic record of such events. By comparing deuterium and oxygen isotope levels in the ice cores, researchers can estimate the extent of the ancient sea ice. These data show …