Instead, more than a century of Atlantic iceberg counts reveals that 1912 was an average year for dangerous floating ice.
The findings also contradict a popular notion that the Jakobshavn Isbrae glacier on Greenland's west coast gave birth to the Titanic's deadly 'berg. Instead, a computer model suggests that one of the glaciers at Greenland's southern tip released the iceberg that hit the Titanic on April 14, 1912, drowning more than 1,500 people in the frigid ocean.
"I think the question of whether this was an unusual year has been laid to rest," said Grant Bigg, an environmental scientist at the University of Sheffield and lead author of a study published Thursday in the journal Weather. "1912 is not an exceptional year."
After a glancing collision with an estimated 325-foot (100 meters) wide iceberg, the Titanic broke into two pieces and sank. In the decades since, the tragedy has acquired a vast history and mythology as people seek to account for the loss of the "unsinkable" ship on its maiden voyage.
Did a supermoon do it?
For years, Titanic theorists have speculated that the ship faced more icebergs than usual due to a warm winter, or sunspots, or high tides from a "supermoon" that could have dislodged icebergs. [Video: How the Titanic Sank]
The new findings run counter to such speculation. They come from a broader examination of Greenland icebergs by Bigg and study co-author David Wilton, also from the University of Sheffield.
The researchers have been tracking icebergs over time to test Greenland's response to climate change and the contribution to sea level rise from icebergs. They are studying data collected by the U.S. Coast Guard's International Ice Patrol extending back to 1900.
According to Bigg, 1912 was a high ice year, but not exceptional compared with the surrounding decades.
In 1912, data shows that 1,038 icebergs moved south from Arctic waters and crossed the 48th parallel. The Coast Guard records show that a slightly higher number of 1,041 icebergs crossed south of 48 degrees north in 1909. Between 1901 and 1920, there were five years when at least 700 icebergs drifted below 48 degrees north, where they could menace ships.
Bigg said the broader study indicates climate change has increased the risk of icebergs for ships sailing near Greenland in recent decades. Between 1991 and 2000, five years saw more icebergs below the 48th parallel than in 1912. "The values are now twice as high as the largest values from earlier in the century," Bigg said. "Greenland's contribution to sea level rise is increasing."
Birth of a tragedy
Bigg and Wilton also created a computer model to plot the likely path of icebergs discharged from Greenland's glaciers. The model showed that the deadly 1912 iceberg probably originated from southern Greenland in late summer or early autumn of 1911.
This 'berg probably sailed directly southwest toward southern Labrador and Newfoundland, rather than heading north up the Greenland coast into Baffin Bay and circling around via the Labrador Current, as other models have suggested, Bigg said.
The iceberg was originally 1,640 feet (500 meters) wide and 985 feet (300 meters) high, the model indicates. By April, the floating chunk was just 325 feet (100 meters) wide.
"It still looked large to the people on the ship, but it had melted quite a bit," Bigg said.
— Becky Oskin, LiveScience
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